explanation      blue bibcodes open ADS page with paths to full text
Author name code: usoskin
ADS astronomy entries on 2022-09-14
author:"Usoskin, Ilya G." 

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Title: Extreme solar events
Authors: Cliver, Edward W.; Schrijver, Carolus J.; Shibata, Kazunari;
   Usoskin, Ilya G.
2022LRSP...19....2C    Altcode: 2022arXiv220509265C
  We trace the evolution of research on extreme solar and
  solar-terrestrial events from the 1859 Carrington event to the rapid
  development of the last twenty years. Our focus is on the largest
  observed/inferred/theoretical cases of sunspot groups, flares on the
  Sun and Sun-like stars, coronal mass ejections, solar proton events,
  and geomagnetic storms. The reviewed studies are based on modern
  observations, historical or long-term data including the auroral and
  cosmogenic radionuclide record, and Kepler observations of Sun-like
  stars. We compile a table of 100- and 1000-year events based on
  occurrence frequency distributions for the space weather phenomena
  listed above. Questions considered include the Sun-like nature of
  superflare stars and the existence of impactful but unpredictable solar
  "black swans" and extreme "dragon king" solar phenomena that can involve
  different physics from that operating in events which are merely large.

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Title: Solar Energetic-Particle Ground-Level Enhancements and the
    Solar Cycle
Authors: Owens, Mathew J.; Barnard, Luke A.; Pope, Benjamin J. S.;
   Lockwood, Mike; Usoskin, Ilya; Asvestari, Eleanna
2022SoPh..297..105O    Altcode: 2022arXiv220712787O
  Severe geomagnetic storms appear to be ordered by the solar cycle in
  a number of ways. They occur more frequently close to solar maximum
  and the declining phase, are more common in larger solar cycles,
  and show different patterns of occurrence in odd- and even-numbered
  solar cycles. Our knowledge of the most extreme space-weather events,
  however, comes from spikes in cosmogenic-isotope (<SUP>14</SUP>C,
  <SUP>10</SUP>Be, and <SUP>36</SUP>Cl) records that are attributed
  to significantly larger solar energetic-particle (SEP) events than
  have been observed during the space age. Despite both storms and
  SEPs being driven by solar-eruptive phenomena, the event-by-event
  correspondence between extreme storms and extreme SEPs is low. Thus,
  it should not be assumed a priori that the solar-cycle patterns found
  for storms also hold for SEPs and the cosmogenic-isotope events. In
  this study, we investigate the solar-cycle trends in the timing and
  magnitude of the 67 SEP ground-level enhancements (GLEs) recorded
  by neutron monitors since the mid-1950s. Using a number of models of
  GLE-occurrence probability, we show that GLEs are around a factor of
  four more likely around solar maximum than around solar minimum, and
  that they preferentially occur earlier in even-numbered solar cycles
  than in odd-numbered cycles. There are insufficient data to conclusively
  determine whether larger solar cycles produce more GLEs. Implications
  for putative space-weather events in the cosmogenic-isotope records
  are discussed. We find that GLEs tend to cluster within a few tens
  of days, likely due to particularly productive individual active
  regions, and with approximately 11-year separations, owing to the
  solar-cycle ordering. However, these timescales would not explain any
  cosmogenic-isotope spikes requiring multiple extreme SEP events over
  consecutive years.

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Title: Solar cyclic activity over the last millennium
    reconstructedfrom annual <SUP>14</SUP>C data (Corrigendum)
Authors: Usoskin, I. G.; Solanki, S. K.; Krivova, N.; Hofer, B.;
   Kovaltsov, G. A.; Wacker, L.; Brehm, N.; Kromer, B.
2022A&A...664C...3U    Altcode:
  No abstract at ADS

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Title: Long-term forcing of Sun's coronal field, open flux and
    cosmic ray modulation potential during grand minima, maxima and
    regular activity phases by the solar dynamo mechanism
Authors: Dash, Soumyaranjan; Nandy, Dibyendu; Usoskin, Ilya
2022arXiv220812103D    Altcode:
  Magnetic fields generated in the Sun's interior by the solar dynamo
  mechanism drive solar activity over a range of time-scales. While
  space-based observations of the Sun's corona exist only for few decades,
  direct sunspot observations exist for a few centuries, solar open flux
  and cosmic ray flux variations can be reconstructed through studies of
  cosmogenic isotopes over thousands of years. While such reconstructions
  indicate the presence of extreme solar activity fluctuations in
  the past, causal links between millennia scale dynamo activity,
  consequent coronal field, solar open flux and cosmic ray modulation
  remain elusive. By utilizing a stochastically forced solar dynamo model
  we perform long-term simulations to illuminate how the dynamo generated
  magnetic fields govern the structure of the solar corona and the state
  of the heliosphere -- as indicated by variations in the open flux
  and cosmic ray modulation potential. We establish differences in the
  nature of the large-scale structuring of the solar corona during grand
  maximum, minimum, and regular solar activity phases and simulate how the
  open flux and cosmic ray modulation potential varies over time scales
  encompassing these different phases of solar activity. We demonstrate
  that the power spectrum of simulated and reconstructed solar open flux
  are consistent with each other. Our study provides the theoretical
  basis for interpreting long-term solar cycle variability based on
  reconstructions relying on cosmogenic isotopes and connects solar
  internal variations to the forcing of the state of the heliosphere.

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Title: Rapid Auroral Wandering During the Laschamp Event
Authors: Mukhopadhyay, Agnit; Usoskin, Ilya; Liemohn, Michael;
   Panovska, Sanja; Brenner, Austin; Garcia-Sage, Katherine; Welling,
   Daniel; Ganushkina, Natalia
2022cosp...44.1573M    Altcode:
  41 thousand years ago, the Laschamp geomagnetic excursion caused Earth's
  magnetic field to drastically diminish to $\sim$4% of the modern
  dipole moment and altered its dipole-dominated structure. While the
  impact of this geomagnetic event on environmental factors and human
  lifestyle has been contemplated to be linked with modifications in the
  geospace environment, no concerted investigation has been conducted
  to study this until recently. In particular, the structure of the
  magnetosphere during such an event was unconstrained. We present an
  initial investigation of the global space environment and related
  plasma environments during several phases of the Laschamp event using
  an advanced multi-model approach. We use recent paleomagnetic field
  models of this event to study the paleomagnetosphere going beyond a
  simple dipole approximation but consider a realistic geomagnetic field
  configuration. The field is used within the global magnetohydrodynamic
  model BATS-R-US to simulate the magnetosphere during discrete epochs
  spanning the peak of the event. Since solar conditions have remained
  fairly constant over the last $\sim$100k years, modern estimates of
  the solar wind were used to drive the model. Finally, plasma pressure
  and currents generated by BATS-R-US at their inner boundary are used
  to compute auroral fluxes using a stand-alone version of the MAGNIT
  model, an adiabatic kinetic model of the aurora. Our results show that
  changes in the geomagnetic field, both in strength and direction, have
  profound effects on the space environment and the ensuing auroral
  pattern. Magnetopause distances during the deepest phase of the
  excursion match previous predictions, while high-resolution mapping of
  magnetic fields allow close examination of magnetospheric structure
  for non-dipolar configurations. Temporal progression of the event
  also exhibits rapid locomotion of the auroral region over ~250 years
  along with the movement of the geomagnetic poles. Our estimates suggest
  that the aurora extended to low latitudes, with the center of the oval
  located at near-equatorial latitudes during the peak of the event. While
  the study does not find evidence of any link between geomagnetic
  variability and habitability conditions, geographic locations of the
  auroral oval coincide with early human activity in Eurasia and Oceania.

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Title: Application of a neutron monitor data analysis for
    quantification of cosmic-ray induced terrestrial effects
Authors: Mishev, Alexander; Usoskin, Ilya
2022cosp...44.1061M    Altcode:
  The studies of cosmic rays (CRs) performed with the worldwide NM
  network provide key information about various processes, such as
  production and acceleration of energetic particles at the Sun and the
  interplanetary medium, interactions of galactic cosmic rays (GCRs) with
  magnetic fields in the heliosphere i.e. probing the electromagnetic and
  plasma conditions of the heliosphere. The introduction of an NM as a
  continuous recorder of CR intensity resulted from the design by John
  Simpson. During the International Geophysical Year (IGY) 1957-1958,
  a 12-counter neutron monitor was designed. Lately, the design of NM
  was optimized resulting in an increase of the counting rates, appearing
  the second generation of NMs known as NM64, nowadays used as a standard
  detector. Besides, a specific class of solar energetic particles (SEPs),
  namely those registered at the ground by neutron monitors, that is,
  ground-level enhancements (GLEs), are conveniently studied using NM
  data. GLE events are numbered consecutively, starting from the first
  event that was detected in 1942. The most recent event was No. 73 in
  October 2021. An important topic in the field of space physics is
  related to the quantification of CR effects on atmospheric physics
  and chemistry as well as space weather. For this purpose is necessary
  to possess precise information of SEP spectra. This can be achieved
  based on NM data analysis. Here we demonstrate the capabilities of
  the verified method for the determination of SEP spectra and pitch
  angle distributions in their dynamical development throughout GLE
  events. Subsequently, on the basis of the derived spectra, we assess
  the ion production rate in the atmosphere and exposure to radiation
  at flight altitudes, thus quantifying important cosmic-ray induced
  terrestrial effects.

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Title: Characteristics of the First Ground Level Enhancement (GLE)
    of Solar Cycle 25 on 28 October 2021
Authors: Papaioannou, Athanasios; Usoskin, Ilya; Gieseler, Jan; Herbst,
   Konstantin; Kühl, Patrick; Rouillard, Alexis; Mishev, Alexander;
   Wimmer-Schweingruber, Robert; Vainio, Rami; Anastasiadis, Anastasios;
   Kouloumvakos, Athanasios
2022cosp...44.1064P    Altcode:
  We present an overview of the first ground-level enhancement (GLE)
  event of solar cycle 25, recorded on 28 October 2021 (GLE73), based
  on the available neutron monitor (NM) network observations and on data
  from near-Earth spacecraft (GOES, SOHO, SolO). The maximum increase was
  $\sim$7.3% for DOMC (Dome C NM at Concordia station) and 5.4% for SOPO
  (South Pole) conventional NMs located on the Antarctic plateau. Bare
  (lead-free) NMs at the same sites detected a higher response (14.0%
  for DOMB and 6.6% for SOPB). The Fort Smith (FSMT) NM shows the earliest
  increase among the high-latitude NMs, indicating a moderate anisotropy
  in the first phase of the GLE event. The maximum rigidity of accelerated
  protons did not exceed 2.4 GV. We estimated the solar release time (SRT)
  of $\geq$1 GV protons into open magnetic field lines at $\sim$15:40
  UT. In-situ proton observations from near-Earth spacecraft were
  combined with the detection of a solar flare in soft X-rays (SXRs),
  a coronal mass ejection (CME), radio bursts and extreme ultraviolet
  (EUV) observations to identify the solar origin of the GLE. Around the
  $\geq$1 GV proton SRT the CME-driven shock was located at a height of
  $\sim$2.33 Rs. The timing of the EUV wave evolution towards the field
  lines magnetically connected to Earth seem to be in good agreement
  with the inferred release time of $\geq$1 GV protons.

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Title: Spectral and Anisotropy Characteristics of the Solar Protons
    during Ground Level Enhancement (GLE) # 73 on 28 October 2021 derived
    with Neutron Monitor data
Authors: Mishev, Alexander; Usoskin, Ilya; Koldobskiy, Sergey;
   Kocharov, Leon; Larsen, Nicholas
2022cosp...44.1075M    Altcode:
  The first ground-level enhancement of the current solar cycle 25
  occurred on 28 October 2021. It was observed by several space-borne
  and ground-based instruments, specifically neutron monitors. A moderate
  count-rate increase over the galactic-cosmic ray background was observed
  by high-altitude polar stations on the South Pole and Concordia stations
  at the Antarctic plateau. Most of the neutron monitors registered
  only a marginal increase. Here, using de-trended records, employing
  verified by direct space-borne measurements method we derived the
  rigidity spectra and angular distribution of incoming solar protons
  for the GLE #73. We employed the newly computed and parameterized
  neutron-monitor yield function. The rigidity spectra and anisotropy of
  the solar protons were obtained in their dynamical evolution throughout
  the event. Quantification of acceleration mechanism is discussed.

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Title: Reconstructions of solar activity and variability from
    cosmogenic isotope data
Authors: Krivova, Natalie; Usoskin, Ilya
2022cosp...44.1046K    Altcode:
  Our knowledge about the activity and variability of the Sun on the
  millennial time scale relies on cosmogenic isotope data. Modulated by
  the solar open magnetic field, the fluctuating flux of the energetic
  cosmic ray particles in the vicinity of Earth leads to the formation
  of varying amounts of the radionuclides in the atmosphere. These
  radionuclides are naturally stored in terrestrial archives for millennia
  and can be measured in laboratories nowadays. In combination with
  appropriate models, such data then allow us to go back in time and
  understand how the Sun behaved in the past. We will review the latest
  progress in understanding and reconstruction of the solar activity
  over the last millennia.

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Title: Analysis of diurnal cosmic-ray variations as observed by
    polar NMs
Authors: Gil, Agnieszka; Usoskin, Ilya; Poluianov, Stepan; Mishev,
   Alexander
2022cosp...44.1067G    Altcode:
  Galactic cosmic rays (GCRs) show a low local anisotropy perceived as
  a diurnal variability of neutron-monitor (NM) count rates. The NMs
  have different abilities of observations of the GCR diurnal variation,
  because their asymptotic directions are spatially diverse at a large
  extent. We demonstrate that there is one NM at Dome C (DOMC) which
  does not observe diurnal variability. Compared to other polar NMs,
  for which the diurnal variation amplitudes span between 0.16 to 0.4%,
  it is very small (0.03%) for DOMC. It is due to the narrow asymptotic
  cone of the DOMC NM, directed practically in the polar direction
  with geographic latitude over 75 degrees south. Hence, DOMC NM is the
  uniquely located NM, which accepts cosmic rays from the off-equatorial
  and off-ecliptic plane. This is of special interest for comprehensive
  studies of cosmic-ray transport in the Earth vicinity, particularly
  for anisotropic solar energetic particle events.

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Title: Long-Term Solar Variability and Solar Cycle Predictions:
    Current State of Understanding
Authors: Nandi, Dibyendu; Usoskin, Ilya; Pevtsov, Alexei
2022cosp...44.3520N    Altcode:
  The Sun's activity varies over timescales ranging from the very short
  to the very long. Long-term solar activity variations impact the
  Earth's atmosphere and climate and have implications for space mission
  planning and life-time estimates. This variability across different
  scales is driven by solar magnetic fields which originate in the deep
  convection zone, emerge through the surface and evolve. Understanding
  the physical basis for long-term variability over decadal scales and
  longer is important for developing predictive models for sunspot cycle
  which is an outstanding challenge. Concurrently, exploring the basis
  of fluctuations that lead to extreme episodes such as grand maxima in
  solar activity remains an important exercise with no clear indication
  that such episodes are predictable. We shall review here the current
  state of our understanding of long-term solar variability, and identify
  challenges that are expected to spur future developments in this field.

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Title: High-Resolution Spectral and Anisotropy Characteristics of
    Solar Protons During the GLE N<SUP>∘</SUP>73 on 28 October 2021
    Derived with Neutron-Monitor Data Analysis
Authors: Mishev, Alexander L.; Kocharov, Leon G.; Koldobskiy, Sergey
   A.; Larsen, Nicholas; Riihonen, Esa; Vainio, Rami; Usoskin, Ilya G.
2022SoPh..297...88M    Altcode:
  The first ground-level enhancement of the current Solar Cycle 25
  occurred on 28 October 2021. It was observed by several space-borne
  and ground-based instruments, specifically neutron monitors. A
  moderate count-rate increase over the background was observed by
  high-altitude polar stations on the South Pole and Dome C stations at
  the Antarctic plateau. Most of the neutron monitors registered only
  marginal count-rate increases. Using detrended records and employing
  a method verified by direct space-borne measurements, we derive the
  rigidity spectra and angular distributions of the incoming solar
  protons in the vicinity of Earth. For the analysis, we employed a
  newly computed and parameterized neutron-monitor yield function. The
  rigidity spectra and anisotropy of solar protons were obtained in their
  time evolution throughout the event. A comparison with the Solar and
  Heliospheric Observatory/Energetic and Relativistic Nuclei and Electron
  (SOHO/ENRE) experiment data is also performed. We briefly discuss the
  results derived from our analysis.

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Title: Properties of Daily Helium Fluxes
Authors: Aguilar, M.; Cavasonza, L. Ali; Ambrosi, G.; Arruda, L.;
   Attig, N.; Barao, F.; Barrin, L.; Bartoloni, A.; Başeǧmez-du Pree,
   S.; Battiston, R.; Behlmann, M.; Berdugo, J.; Bertucci, B.; Bindi,
   V.; Bollweg, K.; Borgia, B.; Boschini, M. J.; Bourquin, M.; Bueno,
   E. F.; Burger, J.; Burger, W. J.; Burmeister, S.; Cai, X. D.; Capell,
   M.; Casaus, J.; Castellini, G.; Cervelli, F.; Chang, Y. H.; Chen,
   G. M.; Chen, G. R.; Chen, H. S.; Chen, Y.; Cheng, L.; Chou, H. Y.;
   Chouridou, S.; Choutko, V.; Chung, C. H.; Clark, C.; Coignet, G.;
   Consolandi, C.; Contin, A.; Corti, C.; Cui, Z.; Dadzie, K.; Dass,
   A.; Delgado, C.; Della Torre, S.; Demirköz, M. B.; Derome, L.; Di
   Falco, S.; Di Felice, V.; Díaz, C.; Dimiccoli, F.; von Doetinchem,
   P.; Dong, F.; Donnini, F.; Duranti, M.; Egorov, A.; Eline, A.; Feng,
   J.; Fiandrini, E.; Fisher, P.; Formato, V.; Freeman, C.; Gámez,
   C.; García-López, R. J.; Gargiulo, C.; Gast, H.; Gervasi, M.;
   Giovacchini, F.; Gómez-Coral, D. M.; Gong, J.; Goy, C.; Grabski, V.;
   Grandi, D.; Graziani, M.; Haino, S.; Han, K. C.; Hashmani, R. K.;
   He, Z. H.; Heber, B.; Hsieh, T. H.; Hu, J. Y.; Incagli, M.; Jang,
   W. Y.; Jia, Yi; Jinchi, H.; Karagöz, G.; Khiali, B.; Kim, G. N.;
   Kirn, Th.; Konyushikhin, M.; Kounina, O.; Kounine, A.; Koutsenko, V.;
   Krasnopevtsev, D.; Kuhlman, A.; Kulemzin, A.; La Vacca, G.; Laudi, E.;
   Laurenti, G.; Lazzizzera, I.; Lee, H. T.; Lee, S. C.; Li, H. L.; Li,
   J. Q.; Li, M.; Li, Q.; Li, Q. Y.; Li, S.; Li, S. L.; Li, J. H.; Li,
   Z. H.; Liang, J.; Liang, M. J.; Light, C.; Lin, C. H.; Lippert, T.;
   Liu, J. H.; Lu, S. Q.; Lu, Y. S.; Luebelsmeyer, K.; Luo, J. Z.; Luo,
   Xi; Machate, F.; Mañá, C.; Marín, J.; Marquardt, J.; Martin, T.;
   Martínez, G.; Masi, N.; Maurin, D.; Medvedeva, T.; Menchaca-Rocha,
   A.; Meng, Q.; Mikhailov, V. V.; Molero, M.; Mott, P.; Mussolin, L.;
   Negrete, J.; Nikonov, N.; Nozzoli, F.; Ocampo-Peleteiro, J.; Oliva,
   A.; Orcinha, M.; Palermo, M.; Palmonari, F.; Paniccia, M.; Pashnin,
   A.; Pauluzzi, M.; Pensotti, S.; Plyaskin, V.; Pohl, M.; Poluianov, S.;
   Qin, X.; Qu, Z. Y.; Quadrani, L.; Rancoita, P. G.; Rapin, D.; Conde,
   A. Reina; Robyn, E.; Rosier-Lees, S.; Rozhkov, A.; Rozza, D.; Sagdeev,
   R.; Schael, S.; von Dratzig, A. Schultz; Schwering, G.; Seo, E. S.;
   Shan, B. S.; Siedenburg, T.; Song, J. W.; Song, X. J.; Sonnabend, R.;
   Strigari, L.; Su, T.; Sun, Q.; Sun, Z. T.; Tacconi, M.; Tang, X. W.;
   Tang, Z. C.; Tian, J.; Ting, Samuel C. C.; Ting, S. M.; Tomassetti,
   N.; Torsti, J.; Urban, T.; Usoskin, I.; Vagelli, V.; Vainio, R.;
   Valencia-Otero, M.; Valente, E.; Valtonen, E.; Vázquez Acosta, M.;
   Vecchi, M.; Velasco, M.; Vialle, J. P.; Wang, C. X.; Wang, L.; Wang,
   L. Q.; Wang, N. H.; Wang, Q. L.; Wang, S.; Wang, X.; Wang, Yu; Wang,
   Z. M.; Wei, J.; Weng, Z. L.; Wu, H.; Xiong, R. Q.; Xu, W.; Yan, Q.;
   Yang, Y.; Yashin, I. I.; Yi, H.; Yu, Y. M.; Yu, Z. Q.; Zannoni, M.;
   Zhang, C.; Zhang, F.; Zhang, F. Z.; Zhang, J. H.; Zhang, Z.; Zhao,
   F.; Zheng, C.; Zheng, Z. M.; Zhuang, H. L.; Zhukov, V.; Zichichi,
   A.; Zuccon, P.; AMS Collaboration
2022PhRvL.128w1102A    Altcode:
  We present the precision measurement of 2824 daily helium fluxes in
  cosmic rays from May 20, 2011 to October 29, 2019 in the rigidity
  interval from 1.71 to 100 GV based on 7.6 ×10<SUP>8</SUP> helium
  nuclei collected with the Alpha Magnetic Spectrometer (AMS) aboard
  the International Space Station. The helium flux and the helium to
  proton flux ratio exhibit variations on multiple timescales. In nearly
  all the time intervals from 2014 to 2018, we observed recurrent helium
  flux variations with a period of 27 days. Shorter periods of 9 days and
  13.5 days are observed in 2016. The strength of all three periodicities
  changes with time and rigidity. In the entire time period, we found that
  below ∼7 GV the helium flux exhibits larger time variations than the
  proton flux, and above ∼7 GV the helium to proton flux ratio is time
  independent. Remarkably, below 2.4 GV a hysteresis between the helium
  to proton flux ratio and the helium flux was observed at greater than
  the 7 σ level. This shows that at low rigidity the modulation of the
  helium to proton flux ratio is different before and after the solar
  maximum in 2014.

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Title: The first ground-level enhancement of solar cycle 25 on 28
    October 2021
Authors: Papaioannou, A.; Kouloumvakos, A.; Mishev, A.; Vainio, R.;
   Usoskin, I.; Herbst, K.; Rouillard, A. P.; Anastasiadis, A.; Gieseler,
   J.; Wimmer-Schweingruber, R.; Kühl, P.
2022A&A...660L...5P    Altcode: 2022arXiv220207927P
  <BR /> Aims: The first relativistic solar proton event of solar
  cycle 25 was detected on 28 October 2021 by neutron monitors (NMs)
  on the ground and particle detectors on board spacecraft in near-Earth
  space. This is the first ground-level enhancement (GLE) of the current
  cycle. A detailed reconstruction of the NM response together with the
  identification of the solar eruption that generated these particles is
  investigated based on in situ and remote-sensing measurements. <BR />
  Methods: In situ proton observations from a few MeV to ∼500 MeV
  were combined with the detection of a solar flare in soft X-rays,
  a coronal mass ejection, radio bursts, and extreme ultraviolet (EUV)
  observations to identify the solar origin of the GLE. Timing analysis
  was performed, and a relation to the solar sources was outlined. <BR
  /> Results: GLE73 reached a maximum particle rigidity of ∼2.4 GV
  and is associated with type III, type II, and type IV radio bursts
  and an EUV wave. A diversity of time profiles recorded by NMs was
  observed. This points to the event having an anisotropic nature. The
  peak flux at E &gt; 10 MeV was only ∼30 pfu and remained at this level
  for several days. The release time of ≥1 GV particles was found to
  be ∼15:40 UT. GLE73 had a moderately hard rigidity spectrum at very
  high energies (γ ∼ 5.5). Comparison of GLE73 to previous GLEs with
  similar solar drivers is performed. <P />Movies are available at <A
  href="https://www.aanda.org/10.1051/0004-6361/202142855/olm">https://www.aanda.org</A>

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Title: Performance of the current and extended global NM network
    for solar particle registration and analysis
Authors: Mishev, A.; Usoskin, I.
2022icrc.confE1315M    Altcode: 2022PoS...395E1315M
  No abstract at ADS

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Title: New reconstruction of the event-integrated spectra for
    GLE events
Authors: Koldobskiy, S.; Raukunen, O.; Vainio, R.; Kovaltsov, G.;
   Usoskin, I.
2022icrc.confE1273K    Altcode: 2022PoS...395E1273K
  No abstract at ADS

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Title: High-multiplicity neutron events registered by NEMESIS
    experiment
Authors: Kasztelan, M.; Enqvist, T.; Jędrzejczak, K.; Joutsenvaara,
   J.; Kotavaara, O.; Kuusiniemi, P.; Loo, K. K.; Orzechowski, J.;
   Puputti, J.; Sobkow, A.; Słupecki, M.; Szabelski, J.; Usoskin, I.;
   Trzaska, W. H.; Ward, T. E.
2022icrc.confE.497K    Altcode: 2022PoS...395E.497K
  No abstract at ADS

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Title: Strongest directly observed Solar Proton Event of 23-Feb-1956:
    Revised reference for the cosmogenic-isotope method
Authors: Usoskin, I.; Koldobskiy, S.; Kovaltsov, G.; Sukhodolov, T.;
   Mishev, A.; Mironova, I.
2022icrc.confE1319U    Altcode: 2022PoS...395E1319U
  No abstract at ADS

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Title: Pulse height-length analysis of data from neutron monitors
    DOMC/DOMB with a new data acquisition system
Authors: Similä, M.; Poluianov, S.; Usoskin, I.; Mishev, A.;
   Kovaltsov, G.; Strauss, D. T.
2022icrc.confE1237S    Altcode: 2022PoS...395E1237S
  No abstract at ADS

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Title: Application of the verified neutron monitor yield function
    for GLE analysis
Authors: Mishev, A.; Usoskin, I.; Koldobskiy, S.; Kovaltsov, G.;
   Kocharov, L.
2022icrc.confE1236M    Altcode: 2022PoS...395E1236M
  No abstract at ADS

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Title: New NEMESIS Results
Authors: Trzaska, W. H.; Enqvist, T.; Jędrzejczak, K.; Joutsenvaara,
   J.; Kasztelan, M.; Kotavaara, O.; Kuusiniemi, P.; Loo, K.; Orzechowski,
   J.; Puputti, J.; Sobkow, A.; Słupecki, M.; Szabelski, J.; Usoskin,
   I.; Ward, T.
2022icrc.confE.514T    Altcode: 2022PoS...395E.514T
  No abstract at ADS

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Title: A major update of the International GLE Database: Correction
    for the variable GCR background
Authors: Usoskin, I.; Koldobskiy, S.; Gil, A.; Kovaltsov, G.; Usoskina,
   I.; Willamo, T.; Ibragimov, A.
2022icrc.confE1241U    Altcode: 2022PoS...395E1241U
  No abstract at ADS

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Title: Role of heavier-than-proton nuclei in neutron monitor response
Authors: Koldobskiy, S.; Kovaltsov, G.; Usoskin, I.
2022icrc.confE1284K    Altcode: 2022PoS...395E1284K
  No abstract at ADS

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Title: New neutron monitor altitude-dependent yield function and
    its application to an analysis of neutron-monitor data
Authors: Mishev, A.; Koldobskiy, S.; Kovaltsov, G.; Gil, A.;
   Usoskin, I.
2022icrc.confE1247M    Altcode: 2022PoS...395E1247M
  No abstract at ADS

---------------------------------------------------------
Title: Quality survey of Neutron Monitor data sources for 1951-2019
Authors: Väisänen, P.; Usoskin, I.; Mursula, K.
2022icrc.confE1244V    Altcode: 2022PoS...395E1244V
  No abstract at ADS

---------------------------------------------------------
Title: Halloween GLEs on October-November 2003, spectra and angular
distribution: Revised results
Authors: Mishev, A.; Usoskin, I.; Kocharov, L.
2022icrc.confE1261M    Altcode: 2022PoS...395E1261M
  No abstract at ADS

---------------------------------------------------------
Title: Tree-rings reveal two strong solar proton events in 7176 and
    5259 BCE
Authors: Brehm, Nicolas; Christl, Marcus; Knowles, Timothy D. J.;
   Casanova, Emmanuelle; Evershed, Richard P.; Adolphi, Florian;
   Muscheler, Raimund; Synal, Hans-Arno; Mekhaldi, Florian; Paleari,
   Chiara I.; Leuschner, Hanns-Hubert; Bayliss, Alex; Nicolussi, Kurt;
   Pichler, Thomas; Schlüchter, Christian; Pearson, Charlotte L.;
   Salzer, Matthew W.; Fonti, Patrick; Nievergelt, Daniel; Hantemirov,
   Rashit; Brown, David M.; Usoskin, Ilya; Wacker, Lukas
2022NatCo..13.1196B    Altcode:
  The Sun sporadically produces eruptive events leading to intense
  fluxes of solar energetic particles (SEPs) that dramatically disrupt
  the near-Earth radiation environment. Such events have been directly
  studied for the last decades but little is known about the occurrence
  and magnitude of rare, extreme SEP events. Presently, a few events
  that produced measurable signals in cosmogenic radionuclides such
  as <SUP>14</SUP>C, <SUP>10</SUP>Be and <SUP>36</SUP>Cl have been
  found. Analyzing annual <SUP>14</SUP>C concentrations in tree-rings
  from Switzerland, Germany, Ireland, Russia, and the USA we discovered
  two spikes in atmospheric <SUP>14</SUP>C occurring in 7176 and 5259
  BCE. The ~2% increases of atmospheric <SUP>14</SUP>C recorded for
  both events exceed all previously known <SUP>14</SUP>C peaks but after
  correction for the geomagnetic field, they are comparable to the largest
  event of this type discovered so far at 775 CE. These strong events
  serve as accurate time markers for the synchronization with floating
  tree-ring and ice core records and provide critical information on
  the previous occurrence of extreme solar events which may threaten
  modern infrastructure.

---------------------------------------------------------
Title: Time Lag Between Cosmic-Ray and Solar Variability: Sunspot
    Numbers and Open Solar Magnetic Flux
Authors: Koldobskiy, Sergey A.; Kähkönen, Riikka; Hofer, Bernhard;
   Krivova, Natalie A.; Kovaltsov, Gennady A.; Usoskin, Ilya G.
2022SoPh..297...38K    Altcode:
  Solar magnetic activity drives the dominant 11-year cyclic variability
  of different space environmental indices, but they can be delayed
  with respect to the original variations due to the different physical
  processes involved. Here, we analyzed the pairwise time lags between
  three global solar and heliospheric indices: sunspot numbers (SSN),
  representing the solar surface magnetic activity, the open solar flux
  (OSF), representing the heliospheric magnetic variability, and the
  galactic cosmic-ray (GCR) intensity near Earth, using the standard
  cross-correlation and the more detailed wavelet-coherence methods. All
  the three indices appear highly coherent at a timescale longer than
  a few years with persistent high coherence at the timescale of the
  11-year solar cycle. The GCR variability is delayed with respect to
  the inverted SSN by about eight 27-day Bartels rotations on average,
  but the delay varies greatly with the 22-year cycle, being shorter or
  longer around positive A + or negative A − solar polarity epochs,
  respectively. The 22-year cyclicity of the time lag is determined by
  the global heliospheric drift effects, in agreement with theoretical
  models. The OSF lags by about one year behind SSN, and is likely
  determined by a combination of the short lifetime of active regions and
  a longer (≈3 years) transport time of the surface magnetic field to
  the poles. GCRs covary nearly in antiphase with the OSF, also depicting
  a strong 22-year cycle in the delay, confirming that the OSF is a
  good index of the heliospheric modulation of GCRs. This provides an
  important observational constraint for solar and heliospheric physics.

---------------------------------------------------------
Title: Effective Energy of Cosmogenic Isotope (<SUP>10</SUP>Be,
    <SUP>14</SUP>C and <SUP>36</SUP>Cl) Production by Solar Energetic
    Particles and Galactic Cosmic Rays
Authors: Koldobskiy, Sergey; Usoskin, Ilya; Kovaltsov, Gennady A.
2022JGRA..12729919K    Altcode:
  Cosmogenic isotopes <SUP>14</SUP>C, <SUP>10</SUP>Be and <SUP>36</SUP>Cl
  measured in datable natural archives provide the only known quantitative
  proxy for cosmic-ray (CR) and solar-activity variability before the
  era of direct measurements. Studies of relations between the measured
  isotope concentrations and CR variability require complicated modeling
  including the isotope production and transport in the terrestrial
  system. Here we propose a rough "effective energy" method to make
  quick estimates of the CR variability directly from the cosmogenic
  data using an approximate linear scaling between the measured isotope
  concentrations and the energy-integrated flux of CR above the effective
  energy. The method is based on the thoroughly computed effective yield
  function presented here. A simple way to account for the variable
  geomagnetic field is also provided. The method was developed for
  both solar energetic particles (SEPs) and galactic cosmic ray (GCR)
  variability and is shown to provide a robust result within 20% and 1%
  accuracy, respectively, without an assumption of the specific spectral
  shape. Applications of the effective-energy method to the known extreme
  SEP events and the secular GCR variability are discussed. The new
  method provides a simple and quick tool to assess the CR variability
  in the past. On the other hand, it does not supersede the full detailed
  modeling required for precise results.

---------------------------------------------------------
Title: Application of CCM SOCOL-AERv2-BE to cosmogenic beryllium
isotopes: description and validation for polar regions
Authors: Golubenko, Kseniia; Rozanov, Eugene; Kovaltsov, Gennady;
   Leppänen, Ari-Pekka; Sukhodolov, Timofei; Usoskin, Ilya
2021GMD....14.7605G    Altcode:
  The short-living cosmogenic isotope <SUP>7</SUP>Be, which is produced
  by cosmic rays in the atmosphere, is often used as a tracer for
  atmospheric dynamics, with precise and high-resolution measurements
  covering the recent decades. The long-living isotope <SUP>10</SUP>Be,
  as measured in polar ice cores with an annual resolution, is a proxy
  for long-term cosmic-ray variability, whose signal can, however,
  be distorted by atmospheric transport and deposition that need to be
  properly modeled to be accounted for. While transport of <SUP>7</SUP>Be
  can be modeled with high accuracy using the known meteorological
  fields, atmospheric transport of <SUP>10</SUP>Be was typically modeled
  using case-study-specific simulations or simplified box models based
  on parameterizations. Thus, there is a need for a realistic model
  able to simulate atmospheric transport and deposition of beryllium
  with a focus on polar regions and (inter)annual timescales that is
  potentially able to operate in a self-consistent mode without the
  prescribed meteorology. Since measurements of <SUP>10</SUP>Be are
  extremely laborious and hence scarce, it is difficult to compare
  model results directly with measurement data. On the other hand,
  the two beryllium isotopes are believed to have similar transport
  and deposition properties, being different only in production and
  lifetime, and thus the results of <SUP>7</SUP>Be transport can be
  generally applied to <SUP>10</SUP>Be. Here we present a new model,
  called CCM SOCOL-AERv2-BE, to trace isotopes of <SUP>7</SUP>Be and
  <SUP>10</SUP>Be in the atmosphere based on the chemistry-climate model
  (CCM) SOCOL (SOlar Climate Ozone Links), which has been improved by
  including modules for the production, deposition, and transport of
  <SUP>7</SUP>Be and <SUP>10</SUP>Be. Production of the isotopes was
  modeled for both galactic and solar cosmic rays by applying the CRAC
  (Cosmic Ray Atmospheric Cascade) model. Transport of <SUP>7</SUP>Be was
  modeled without additional gravitational settling due to the submicron
  size of the background aerosol particles. An interactive deposition
  scheme was applied including both wet and dry deposition. Modeling was
  performed using a full nudging to the meteorological fields for the
  period of 2002-2008 with a spin-up period of 1996-2001. The modeled
  concentrations of <SUP>7</SUP>Be in near-ground air were compared with
  the measured ones at a weekly time resolution in four nearly antipodal
  high-latitude locations: two in the Northern (Finland and Canada) and
  two in the Southern (Chile and the Kerguelen Islands) Hemisphere. The
  model results agree with the measurements in the absolute level within
  error bars, implying that the production, decay, and lateral deposition
  are correctly reproduced. The model also correctly reproduces the
  temporal variability of <SUP>7</SUP>Be concentrations on annual and
  sub-annual scales, including the presence and absence of the annual
  cycle in the Northern and Southern Hemisphere, respectively. We
  also modeled the production and transport of <SUP>7</SUP>Be for a
  major solar energetic particle event (SPE) on 20 January 2005, which
  appears insufficient to produce a measurable signal but may serve as
  a reference event for historically known extreme SPEs. Thus, a new
  full 3D time-dependent model, based on CCM SOCOL, of <SUP>7</SUP>Be
  and <SUP>10</SUP>Be atmospheric production, transport, and deposition
  has been developed. Comparison with real data on the <SUP>7</SUP>Be
  concentration in the near-ground air validates the model and its
  accuracy.

---------------------------------------------------------
Title: Ground Level Enhancement Events: Interplanetary Protons versus
    Protons Interacting at the Sun.
Authors: Kocharov, Leon; Usoskin, Ilya; Mishev, Alexander
2021AGUFMSH51B..03K    Altcode:
  We compare results of the solar high-energy proton detection with
  the neutron monitor network in Ground Level Enhancement (GLE) events
  and the data of pion-decay gamma-ray emission produced by high-energy
  protons interacting at the Sun. Observational data support the idea of a
  common origin of the GLE-producing protons and the protons interacting
  at the Sun to produce sustained gamma-ray emission. Then we discuss
  capabilities of the CME bow-shock acceleration models to explain the
  observational data and argue for the flare and CME synergy in production
  of high-energy protons in the long duration events.

---------------------------------------------------------
Title: Periodicities in the Daily Proton Fluxes from 2011 to 2019
    Measured by the Alpha Magnetic Spectrometer on the International
    Space Station from 1 to 100 GV
Authors: Aguilar, M.; Cavasonza, L. Ali; Ambrosi, G.; Arruda, L.;
   Attig, N.; Barao, F.; Barrin, L.; Bartoloni, A.; Başeǧmez-du Pree,
   S.; Battiston, R.; Behlmann, M.; Beranek, B.; Berdugo, J.; Bertucci,
   B.; Bindi, V.; Bollweg, K.; Borgia, B.; Boschini, M. J.; Bourquin, M.;
   Bueno, E. F.; Burger, J.; Burger, W. J.; Burmeister, S.; Cai, X. D.;
   Capell, M.; Casaus, J.; Castellini, G.; Cervelli, F.; Chang, Y. H.;
   Chen, G. M.; Chen, G. R.; Chen, H. S.; Chen, Y.; Cheng, L.; Chou,
   H. Y.; Chouridou, S.; Choutko, V.; Chung, C. H.; Clark, C.; Coignet,
   G.; Consolandi, C.; Contin, A.; Corti, C.; Cui, Z.; Dadzie, K.; Dass,
   A.; Delgado, C.; Della Torre, S.; Demirköz, M. B.; Derome, L.; Di
   Falco, S.; Di Felice, V.; Díaz, C.; Dimiccoli, F.; von Doetinchem,
   P.; Dong, F.; Donnini, F.; Duranti, M.; Egorov, A.; Eline, A.; Feng,
   J.; Fiandrini, E.; Fisher, P.; Formato, V.; Freeman, C.; Gámez,
   C.; García-López, R. J.; Gargiulo, C.; Gast, H.; Gervasi, M.;
   Giovacchini, F.; Gómez-Coral, D. M.; Gong, J.; Goy, C.; Grabski, V.;
   Grandi, D.; Graziani, M.; Haino, S.; Han, K. C.; Hashmani, R. K.;
   He, Z. H.; Heber, B.; Hsieh, T. H.; Hu, J. Y.; Incagli, M.; Jang,
   W. Y.; Jia, Yi; Jinchi, H.; Karagöz, G.; Khiali, B.; Kim, G. N.;
   Kirn, Th.; Konyushikhin, M.; Kounina, O.; Kounine, A.; Koutsenko, V.;
   Krasnopevtsev, D.; Kuhlman, A.; Kulemzin, A.; La Vacca, G.; Laudi, E.;
   Laurenti, G.; Lazzizzera, I.; Lebedev, A.; Lee, H. T.; Lee, S. C.;
   Li, J. Q.; Li, M.; Li, Q.; Li, S.; Li, J. H.; Li, Z. H.; Liang, J.;
   Light, C.; Lin, C. H.; Lippert, T.; Liu, J. H.; Liu, Z.; Lu, S. Q.;
   Lu, Y. S.; Luebelsmeyer, K.; Luo, J. Z.; Luo, Xi; Machate, F.; Mañá,
   C.; Marín, J.; Marquardt, J.; Martin, T.; Martínez, G.; Masi, N.;
   Maurin, D.; Medvedeva, T.; Menchaca-Rocha, A.; Meng, Q.; Mikhailov,
   V. V.; Molero, M.; Mott, P.; Mussolin, L.; Negrete, J.; Nikonov,
   N.; Nozzoli, F.; Oliva, A.; Orcinha, M.; Palermo, M.; Palmonari,
   F.; Paniccia, M.; Pashnin, A.; Pauluzzi, M.; Pensotti, S.; Phan,
   H. D.; Plyaskin, V.; Pohl, M.; Poluianov, S.; Qin, X.; Qu, Z. Y.;
   Quadrani, L.; Rancoita, P. G.; Rapin, D.; Conde, A. Reina; Robyn,
   E.; Rosier-Lees, S.; Rozhkov, A.; Rozza, D.; Sagdeev, R.; Schael,
   S.; von Dratzig, A. Schultz; Schwering, G.; Seo, E. S.; Shakfa, Z.;
   Shan, B. S.; Siedenburg, T.; Solano, C.; Song, J. W.; Song, X. J.;
   Sonnabend, R.; Strigari, L.; Su, T.; Sun, Q.; Sun, Z. T.; Tacconi,
   M.; Tang, X. W.; Tang, Z. C.; Tian, J.; Ting, Samuel C. C.; Ting,
   S. M.; Tomassetti, N.; Torsti, J.; Urban, T.; Usoskin, I.; Vagelli,
   V.; Vainio, R.; Valencia-Otero, M.; Valente, E.; Valtonen, E.;
   Vázquez Acosta, M.; Vecchi, M.; Velasco, M.; Vialle, J. P.; Wang,
   C. X.; Wang, L.; Wang, L. Q.; Wang, N. H.; Wang, Q. L.; Wang, S.;
   Wang, X.; Wang, Yu; Wang, Z. M.; Wei, J.; Weng, Z. L.; Wu, H.; Xiong,
   R. Q.; Xu, W.; Yan, Q.; Yang, Y.; Yashin, I. I.; Yi, H.; Yu, Y. M.;
   Yu, Z. Q.; Zannoni, M.; Zhang, C.; Zhang, F.; Zhang, F. Z.; Zhang,
   J. H.; Zhang, Z.; Zhao, F.; Zheng, C.; Zheng, Z. M.; Zhuang, H. L.;
   Zhukov, V.; Zichichi, A.; Zuccon, P.; AMS Collaboration
2021PhRvL.127A1102A    Altcode:
  We present the precision measurement of the daily proton fluxes in
  cosmic rays from May 20, 2011 to October 29, 2019 (a total of 2824
  days or 114 Bartels rotations) in the rigidity interval from 1 to
  100 GV based on 5.5 ×10<SUP>9</SUP> protons collected with the Alpha
  Magnetic Spectrometer aboard the International Space Station. The proton
  fluxes exhibit variations on multiple timescales. From 2014 to 2018,
  we observed recurrent flux variations with a period of 27 days. Shorter
  periods of 9 days and 13.5 days are observed in 2016. The strength of
  all three periodicities changes with time and rigidity. The rigidity
  dependence of the 27-day periodicity is different from the rigidity
  dependences of 9-day and 13.5-day periods. Unexpectedly, the strength of
  9-day and 13.5-day periodicities increases with increasing rigidities
  up to ∼10 GV and ∼20 GV , respectively. Then the strength of the
  periodicities decreases with increasing rigidity up to 100 GV.

---------------------------------------------------------
Title: Mind the Gap: New Precise <SUP>14</SUP>C Data Indicate the
    Nature of Extreme Solar Particle Events
Authors: Usoskin, Ilya G.; Kovaltsov, Gennady A.
2021GeoRL..4894848U    Altcode:
  Extreme solar particle events of 775 CE, 994 CE, and 660
  BCE are nearly two orders of magnitude stronger than those
  observed instrumentally. Because of the large observational gap
  between directly measured and historical events, it was unclear
  whether they can be produced by the Sun "normally" or from an
  unknown phenomenon. Recent works by Miyake et al. (2021, doi: <A
  href="https://doi.org/10.1029/2021GL093419">https://doi.org/10.1029/2021GL093419</A>)
  and Brehm et al. (2021, <A
  href="https://doi.org/10.1038/s41561-020-00674-0">https://doi.org/10.1038/s41561-020-00674-0</A>)
  start filling the gap with weaker yet extreme events approaching the
  detectability threshold. More such events are expected to be found in
  the future but the present result, if confirmed, would imply that the
  extreme solar events likely represent the high-energy/low-probability
  tail of the continuous distribution of solar eruptive events rather
  than a new unknown type of events. However, more statistic is needed
  for a solid conclusion. This would lead to better understanding of
  the processes producing such events that is important for their risk
  assessments for the modern technology.

---------------------------------------------------------
Title: Multiple Sources of Solar High-energy Protons
Authors: Kocharov, Leon; Omodei, Nicola; Mishev, Alexander;
   Pesce-Rollins, Melissa; Longo, Francesco; Yu, Sijie; Gary, Dale E.;
   Vainio, Rami; Usoskin, Ilya
2021ApJ...915...12K    Altcode:
  During the 24th solar cycle, the Fermi Large Area Telescope (LAT)
  has observed a total of 27 solar flares possessing delayed γ-ray
  emission, including the exceptionally well-observed flare and coronal
  mass ejection (CME) on 2017 September 10. Based on the Fermi/LAT data,
  we plot, for the first time, maps of possible sources of the delayed
  &gt;100 MeV γ-ray emission of the 2017 September 10 event. The
  long-lasting γ-ray emission is localized under the CME core. The
  γ-ray spectrum exhibits intermittent changes in time, implying that
  more than one source of high-energy protons was formed during the
  flare-CME eruption. We find a good statistical correlation between
  the γ-ray fluences of the Fermi/LAT-observed delayed events and
  the products of corresponding CME speed and the square root of the
  soft X-ray flare magnitude. Data support the idea that both flares
  and CMEs jointly contribute to the production of subrelativistic and
  relativistic protons near the Sun.

---------------------------------------------------------
Title: Properties of a New Group of Cosmic Nuclei: Results from the
    Alpha Magnetic Spectrometer on Sodium, Aluminum, and Nitrogen
Authors: Aguilar, M.; Cavasonza, L. Ali; Alpat, B.; Ambrosi,
   G.; Arruda, L.; Attig, N.; Barao, F.; Barrin, L.; Bartoloni, A.;
   Başeǧmez-du Pree, S.; Battiston, R.; Behlmann, M.; Beranek, B.;
   Berdugo, J.; Bertucci, B.; Bindi, V.; Bollweg, K.; Borgia, B.;
   Boschini, M. J.; Bourquin, M.; Bueno, E. F.; Burger, J.; Burger,
   W. J.; Burmeister, S.; Cai, X. D.; Capell, M.; Casaus, J.; Castellini,
   G.; Cervelli, F.; Chang, Y. H.; Chen, G. M.; Chen, G. R.; Chen,
   H. S.; Chen, Y.; Cheng, L.; Chou, H. Y.; Chouridou, S.; Choutko,
   V.; Chung, C. H.; Clark, C.; Coignet, G.; Consolandi, C.; Contin,
   A.; Corti, C.; Cui, Z.; Dadzie, K.; Delgado, C.; Della Torre, S.;
   Demirköz, M. B.; Derome, L.; Di Falco, S.; Di Felice, V.; Díaz, C.;
   Dimiccoli, F.; von Doetinchem, P.; Dong, F.; Donnini, F.; Duranti, M.;
   Egorov, A.; Eline, A.; Feng, J.; Fiandrini, E.; Fisher, P.; Formato,
   V.; Freeman, C.; Gámez, C.; García-López, R. J.; Gargiulo, C.;
   Gast, H.; Gervasi, M.; Giovacchini, F.; Gómez-Coral, D. M.; Gong,
   J.; Goy, C.; Grabski, V.; Grandi, D.; Graziani, M.; Haino, S.; Han,
   K. C.; Hashmani, R. K.; He, Z. H.; Heber, B.; Hsieh, T. H.; Hu, J. Y.;
   Incagli, M.; Jang, W. Y.; Jia, Yi; Jinchi, H.; Khiali, B.; Kim, G. N.;
   Kirn, Th.; Konyushikhin, M.; Kounina, O.; Kounine, A.; Koutsenko, V.;
   Krasnopevtsev, D.; Kuhlman, A.; Kulemzin, A.; La Vacca, G.; Laudi, E.;
   Laurenti, G.; Lazzizzera, I.; Lebedev, A.; Lee, H. T.; Lee, S. C.;
   Li, J. Q.; Li, M.; Li, Q.; Li, S.; Li, J. H.; Li, Z. H.; Liang, J.;
   Light, C.; Lin, C. H.; Lippert, T.; Liu, J. H.; Liu, Z.; Lu, S. Q.;
   Lu, Y. S.; Luebelsmeyer, K.; Luo, J. Z.; Luo, Xi; Machate, F.; Mañá,
   C.; Marín, J.; Marquardt, J.; Martin, T.; Martínez, G.; Masi, N.;
   Maurin, D.; Medvedeva, T.; Menchaca-Rocha, A.; Meng, Q.; Mikhailov,
   V. V.; Molero, M.; Mott, P.; Mussolin, L.; Negrete, J.; Nikonov,
   N.; Nozzoli, F.; Oliva, A.; Orcinha, M.; Palermo, M.; Palmonari,
   F.; Paniccia, M.; Pashnin, A.; Pauluzzi, M.; Pensotti, S.; Phan,
   H. D.; Plyaskin, V.; Pohl, M.; Poluianov, S.; Qin, X.; Qu, Z. Y.;
   Quadrani, L.; Rancoita, P. G.; Rapin, D.; Conde, A. Reina; Robyn,
   E.; Rosier-Lees, S.; Rozhkov, A.; Rozza, D.; Sagdeev, R.; Schael,
   S.; von Dratzig, A. Schulz; Schwering, G.; Seo, E. S.; Shakfa, Z.;
   Shan, B. S.; Siedenburg, T.; Solano, C.; Song, J. W.; Song, X. J.;
   Sonnabend, R.; Strigari, L.; Su, T.; Sun, Q.; Sun, Z. T.; Tacconi, M.;
   Tang, X. W.; Tang, Z. C.; Tian, J.; Ting, Samuel C. C.; Ting, S. M.;
   Tomassetti, N.; Torsti, J.; Tüysüz, C.; Urban, T.; Usoskin, I.;
   Vagelli, V.; Vainio, R.; Valencia-Otero, M.; Valente, E.; Valtonen,
   E.; Vázquez Acosta, M.; Vecchi, M.; Velasco, M.; Vialle, J. P.;
   Wang, C. X.; Wang, L.; Wang, L. Q.; Wang, N. H.; Wang, Q. L.; Wang,
   S.; Wang, X.; Wang, Yu; Wang, Z. M.; Wei, J.; Weng, Z. L.; Wu, H.;
   Xiong, R. Q.; Xu, W.; Yan, Q.; Yang, Y.; Yashin, I. I.; Yi, H.; Yu,
   Y. M.; Yu, Z. Q.; Zannoni, M.; Zhang, C.; Zhang, F.; Zhang, F. Z.;
   Zhang, J. H.; Zhang, Z.; Zhao, F.; Zheng, C.; Zheng, Z. M.; Zhuang,
   H. L.; Zhukov, V.; Zichichi, A.; Zuccon, P.; AMS Collaboration
2021PhRvL.127b1101A    Altcode:
  We report the properties of sodium (Na) and aluminum (Al) cosmic rays
  in the rigidity range 2.15 GV to 3.0 TV based on 0.46 million sodium
  and 0.51 million aluminum nuclei collected by the Alpha Magnetic
  Spectrometer experiment on the International Space Station. We found
  that Na and Al, together with nitrogen (N), belong to a distinct
  cosmic ray group. In this group, we observe that, similar to the N
  flux, both the Na flux and Al flux are well described by the sums of a
  primary cosmic ray component (proportional to the silicon flux) and a
  secondary cosmic ray component (proportional to the fluorine flux). The
  fraction of the primary component increases with rigidity for the N,
  Na, and Al fluxes and becomes dominant at the highest rigidities. The
  Na /Si and Al /Si abundance ratios at the source, 0.036 ±0.003 for
  Na /Si and 0.103 ±0.004 for Al /Si , are determined independent of
  cosmic ray propagation.

---------------------------------------------------------
Title: Modelling the evolution of the Sun's open and total magnetic
    flux
Authors: Krivova, N. A.; Solanki, S. K.; Hofer, B.; Wu, C. -J.;
   Usoskin, I. G.; Cameron, R.
2021A&A...650A..70K    Altcode: 2021arXiv210315603K
  Solar activity in all its varied manifestations is driven by the
  magnetic field. Two global quantities are particularly important for
  many purposes, the Sun's total and open magnetic flux, which can be
  computed from sunspot number records using models. Such sunspot-driven
  models, however, do not take into account the presence of magnetic
  flux during grand minima, such as the Maunder minimum. Here we
  present a major update of a widely used simple model, which now takes
  into account the observation that the distribution of all magnetic
  features on the Sun follows a single power law. The exponent of the
  power law changes over the solar cycle. This allows for the emergence
  of small-scale magnetic flux even when no sunspots have been present
  for multiple decades and leads to non-zero total and open magnetic
  flux also in the deepest grand minima, such as the Maunder minimum,
  thus overcoming a major shortcoming of the earlier models. The results
  of the updated model compare well with the available observations and
  reconstructions of the solar total and open magnetic flux. This opens
  up the possibility of improved reconstructions of the sunspot number
  from time series of the cosmogenic isotope production rate.

---------------------------------------------------------
Title: GLE # 67 Event on 2 November 2003: An Analysis of the Spectral
    and Anisotropy Characteristics Using Verified Yield Function and
    Detrended Neutron Monitor Data
Authors: Mishev, Alexander L.; Koldobskiy, Sergey A.; Kocharov,
   Leon G.; Usoskin, Ilya G.
2021SoPh..296...79M    Altcode:
  During Solar Cycle 23 16 ground-level enhancement events were registered
  by the global neutron monitor network. In this work we focus on the
  period with increased solar activity during late October - early
  November 2003 producing a sequence of three events, specifically on
  ground-level enhancement GLE 67 on 2 November 2003. On the basis of an
  analysis of neutron monitor and space-borne data we derived the spectra
  and pitch-angle distribution of high-energy solar particles with their
  dynamical evolution throughout the event. According to our analysis,
  the best fit of the spectral and angular properties of solar particles
  was obtained by a modified power-law rigidity spectrum and a double
  Gaussian, respectively. The derived angular distribution is consistent
  with the observations where an early count rate increase at Oulu neutron
  monitor with asymptotic viewing direction in the anti-Sun direction was
  registered. The quality of the fit and model constraints were assessed
  by a forward modeling. The event integrated particle fluence was derived
  using two different methods. The derived results are briefly discussed.

---------------------------------------------------------
Title: Seven Decades of Neutron Monitors (1951-2019): Overview and
    Evaluation of Data Sources
Authors: Väisänen, Pauli; Usoskin, Ilya; Mursula, Kalevi
2021JGRA..12628941V    Altcode:
  The worldwide network of neutron monitors (NMs) is the primary
  instrument to study cosmic ray variability on time scales of up to 70
  yr. Since the 1950s, 147 NMs with publicly available data have been in
  operation, and their records are archived in and distributed through
  different repositories and data sources. A comprehensive analysis of all
  available NM data sets (300 data sets from 147 NMs) is performed here to
  check the quality and consistency of the data. The data sources include
  World Data Center for Cosmic Rays, the Neutron Monitor Database, the
  Pushkov Institute of Terrestrial Magnetism, Ionosphere, and Radiowave
  Propagation (IZMIRAN) and individual station/institution databases. It
  was found that The data from the same NM can be nonidentical and of
  different quality in different sources. We give and tabulate here a
  recommendation for the optimal data source of each NM. We also present
  here a list of 29 "prime" stations with the longest and most reliable
  data. Verified data sets for these prime stations are provided as
  supplementary information.

---------------------------------------------------------
Title: Solar cyclic activity over the last millennium reconstructed
    from annual <SUP>14</SUP>C data
Authors: Usoskin, I. G.; Solanki, S. K.; Krivova, N. A.; Hofer, B.;
   Kovaltsov, G. A.; Wacker, L.; Brehm, N.; Kromer, B.
2021A&A...649A.141U    Altcode: 2021arXiv210315112U
  <BR /> Aims: The 11-year solar cycle (Schwabe cycle) is the dominant
  pattern of solar magnetic activity reflecting the oscillatory dynamo
  mechanism in the Sun's convection zone. Solar cycles have been
  directly observed since 1700, while indirect proxy data suggest their
  existence over a much longer period of time, but generally without
  resolving individual cycles and their continuity. Here we reconstruct
  individual solar cycles for the last millennium using recently
  obtained <SUP>14</SUP>C data and state-of-the-art models. <BR />
  Methods: Starting with the <SUP>14</SUP>C production rate determined
  from the so far most precise measurements of radiocarbon content in
  tree rings, solar activity was reconstructed in the following three
  physics-based steps: (1) correction of the <SUP>14</SUP>C production
  rate for the changing geomagnetic field; (2) computation of the
  open solar magnetic flux; and (3) conversion into sunspot numbers
  outside of grand minima. All known uncertainties, including both
  measurement and model uncertainties, were straightforwardly accounted
  for by a Monte-Carlo method. <BR /> Results: Cyclic solar activity is
  reconstructed for the period 971-1900 (85 individual cycles) along with
  its uncertainties. This more than doubles the number of solar cycles
  known from direct solar observations. We found that the lengths and
  strengths of well-defined cycles outside grand minima are consistent
  with those obtained from the direct sunspot observations after 1750. The
  validity of the Waldmeier rule (cycles with fast-rising phase tend to
  be stronger) is confirmed at a highly significant level. Solar activity
  is found to be in a deep grand minimum when the activity is mostly
  below the sunspot formation threshold for about 250 years. Therefore,
  although considerable cyclic variability in <SUP>14</SUP>C is seen even
  during grand minima, individual solar cycles can hardly be reliably
  resolved therein. Three potential solar particle events, ca. 994,
  1052, and 1279 AD, are shown to occur around the maximum phases of
  solar cycles. <BR /> Conclusions: A new approximately 1000-year-long
  solar activity reconstruction, in the form of annual (pseudo) sunspot
  numbers with the full assessment of all known uncertainties, is
  presented based on new high-precision Δ<SUP>14</SUP>C measurements and
  state-of-the-art models, more than doubling the number of individually
  resolved solar cycles. This forms a solid basis for new, more detailed
  studies of solar variability. <P />Tabular data of the reconstructed
  activity are only available at the CDS via anonymous ftp to <A
  href="http://cdsarc.u-strasbg.fr/">cdsarc.u-strasbg.fr</A>
  (ftp://130.79.128.5) or via <A
  href="http://cdsarc.u-strasbg.fr/viz-bin/cat/J/A+A/649/A141">http://cdsarc.u-strasbg.fr/viz-bin/cat/J/A+A/649/A141</A>

---------------------------------------------------------
Title: High Altitude Polar NM With the New DAQ System as a Tool to
    Study Details of the Cosmic Ray Induced Nucleonic Cascade
Authors: Similä, Markus; Usoskin, Ilya; Poluianov, Stepan; Mishev,
   Alexander; Kovaltsov, Gennady A.; Strauss, Du Toit
2021JGRA..12628959S    Altcode: 2021arXiv210404727S
  A neutron monitor (NM) is, since the 1950s, a standard ground based
  detector whose count rate reflects cosmic ray variability. The worldwide
  network of NMs forms a rough spectrometer for cosmic rays. Recently, a
  brand new data acquisition (DAQ) system has been installed on the DOMC
  and DOMB NMs, located at the Concordia research station on the Central
  Antarctic plateau. The new DAQ system digitizes, at a 2 MHz sampling
  rate, and records all individual pulses corresponding to secondary
  particles in the detector. An analysis of the pulse characteristics
  (viz. shape, magnitude, duration, waiting time) has been performed,
  and several clearly distinguishable branches were identified: (A)
  corresponding to signal from individual secondary neutrons; (B)
  representing the detector's noise; (C) double pulses corresponding
  to the shortly separated nucleons of the same atmospheric cascades;
  (D) very high multiple pulses which are likely caused by atmospheric
  muons; and (E) double pulses potentially caused by contamination of the
  neighboring detector. An analysis of the waiting time distributions has
  revealed two clearly distinguishable peaks: peak (I) at about 1 ms being
  related to the intracascade diffusion and thermalization of secondary
  atmospheric neutrons; and peak (II) at 30-1,000 ms corresponding to
  individual atmospheric cascades. This opens a new possibility to study
  spectra of cosmic ray particles in a single location as well as details
  of the cosmic ray induced atmospheric cascades, using the same data set.

---------------------------------------------------------
Title: Atmospheric production and transport of 7Be activity by
cosmic rays: Modelling with the chemistry-climate model SOCOLv3.0
    and comparison with direct measurements
Authors: Golubenko, Kseniia; Rozanov, Eugene; Kovaltsov, Genady;
   Leppänen, Ari-Pekka; Usoskin, Ilya
2021EGUGA..23.2287G    Altcode:
  We present the first results of modelling of the short-living
  cosmogenic isotope 7Be production, deposition, and transport using the
  chemistry-climate model SOCOLv3.0 aimed to study solar-terrestrial
  interactions and climate changes. We implemented an interactive
  deposition scheme, based on gas tracers with and without nudging to
  the known meteorological fields. Production of 7Be was modelled using
  the 3D time-dependent Cosmic Ray induced Atmospheric Cascade (CRAC)
  model. The simulations were compared with the real concentrations
  (activity) and depositions measurements of 7Be in the air and water at
  Finnish stations. We have successfully reproduced and estimated the
  variability of the cosmogenic isotope 7Be produced by the galactic
  cosmic rays (GCR) on time scales longer than about a month, for the
  period of 2002-2008. The agreement between the modelled and measured
  data is very good (within 12%) providing a solid validation for the
  ability of the SOCOL CCM to reliably model production, transport,
  and deposition of cosmogenic isotopes, which is needed for precise
  studies of cosmic-ray variability in the past.

---------------------------------------------------------
Title: New reconstruction of event-integrated spectra (spectral
    fluences) for major solar energetic particle events
Authors: Koldobskiy, S.; Raukunen, O.; Vainio, R.; Kovaltsov, G. A.;
   Usoskin, I.
2021A&A...647A.132K    Altcode: 2021arXiv210110234K
  <BR /> Aims: Fluences of solar energetic particles (SEPs) are not
  easy to evaluate, especially for high-energy events (i.e. ground-level
  enhancements, GLEs). Earlier estimates of event-integrated SEP fluences
  for GLEs were based on partly outdated assumptions and data, and they
  required revisions. Here, we present the results of a full revision
  of the spectral fluences for most major SEP events (GLEs) for the
  period from 1956 to 2017 using updated low-energy flux estimates along
  with greatly revisited high-energy flux data and applying the newly
  invented reconstruction method including an improved neutron-monitor
  yield function. <BR /> Methods: Low- and high-energy parts of the
  SEP fluence were estimated using a revised space-borne/ionospheric
  data and ground-based neutron monitors, respectively. The measured
  data were fitted by the modified Band function spectral shape. The
  best-fit parameters and their uncertainties were assessed using a
  direct Monte Carlo method. <BR /> Results: A full reconstruction of
  the event-integrated spectral fluences was performed in the energy
  range above 30 MeV, parametrised and tabulated for easy use along
  with estimates of the 68% confidence intervals. <BR /> Conclusions:
  This forms a solid basis for more precise studies of the physics of
  solar eruptive events and the transport of energetic particles in the
  interplanetary medium, as well as the related applications. <P />The
  reconstructed fluences in tabulated form and the corresponding best-fit
  parameters are only available at the CDS via anonymous ftp to <A
  href="http://cdsarc.u-strasbg.fr/">cdsarc.u-strasbg.fr</A>
  (ftp://130.79.128.5) or via <A
  href="http://cdsarc.u-strasbg.fr/viz-bin/cat/J/A+A/647/A132">http://cdsarc.u-strasbg.fr/viz-bin/cat/J/A+A/647/A132</A>

---------------------------------------------------------
Title: VizieR Online Data Catalog: 1000-year sunspot series (Usoskin+,
    2021)
Authors: Usoskin, I. G.; Solanki, S. K.; Krivova, N.; Hofer, B.;
   Kovaltsov, G. A.; Wacker, L.; Brehm, N.; Kromer, B.
2021yCat..36490141U    Altcode:
  A new quantitative reconstruction of annually resolved solar activity,
  in the form of SNs (at least outside grand minima) with a full
  uncertainty assessment, is presented for the period 971-1900. For the
  first time, individual solar cycles are presented for the whole of the
  last millennium, more than doubling the existing statistics of solar
  cycles. <P />Three tabular files are presented. <P />File 'osf.dat'
  contains annual reconstructions of the opens solar flux (OSF) [Fo]
  along with its 1-sigma uncertainties [sF] and the smoothed (22-yr SSA --
  see text) values [&lt;Fo&gt;]. This table corresponds to Figure 8 in
  the text. <P />File 'osn.dat' contains annual reconstructions of the
  sunspot number (SN) [SN] along with its 1-sigma uncertainties [sSN]
  and the smoothed (22-yr SSA -- see text) values [&lt;SN&gt;]. This
  table corresponds to Figure 11 in the text. <P />File 'table1.dat'
  presents a textual tabular version of Table 1 in the text and contains
  the internal cycle number [n], years of minimum [Ymin] and maximum
  [Ymax] of each cycle, cycle-averaged sunspot number [&lt;SN&gt;], its
  1-sigma uncertainty [sS], cycle length (min-to-min) [T], and quality
  flag [q]. <P />(3 data files).

---------------------------------------------------------
Title: The Alpha Magnetic Spectrometer (AMS) on the international
space station: Part II - Results from the first seven years
Authors: Aguilar, M.; Ali Cavasonza, L.; Ambrosi, G.; Arruda, L.;
   Attig, N.; Barao, F.; Barrin, L.; Bartoloni, A.; Başeğmez-du Pree,
   S.; Bates, J.; Battiston, R.; Behlmann, M.; Beischer, B.; Berdugo,
   J.; Bertucci, B.; Bindi, V.; de Boer, W.; Bollweg, K.; Borgia, B.;
   Boschini, M. J.; Bourquin, M.; Bueno, E. F.; Burger, J.; Burger,
   W. J.; Burmeister, S.; Cai, X. D.; Capell, M.; Casaus, J.; Castellini,
   G.; Cervelli, F.; Chang, Y. H.; Chen, G. M.; Chen, H. S.; Chen, Y.;
   Cheng, L.; Chou, H. Y.; Chouridou, S.; Choutko, V.; Chung, C. H.;
   Clark, C.; Coignet, G.; Consolandi, C.; Contin, A.; Corti, C.; Cui,
   Z.; Dadzie, K.; Dai, Y. M.; Delgado, C.; Della Torre, S.; Demirköz,
   M. B.; Derome, L.; Di Falco, S.; Di Felice, V.; Díaz, C.; Dimiccoli,
   F.; von Doetinchem, P.; Dong, F.; Donnini, F.; Duranti, M.; Egorov, A.;
   Eline, A.; Feng, J.; Fiandrini, E.; Fisher, P.; Formato, V.; Freeman,
   C.; Galaktionov, Y.; Gámez, C.; García-López, R. J.; Gargiulo, C.;
   Gast, H.; Gebauer, I.; Gervasi, M.; Giovacchini, F.; Gómez-Coral,
   D. M.; Gong, J.; Goy, C.; Grabski, V.; Grandi, D.; Graziani, M.;
   Guo, K. H.; Haino, S.; Han, K. C.; Hashmani, R. K.; He, Z. H.; Heber,
   B.; Hsieh, T. H.; Hu, J. Y.; Huang, Z. C.; Hungerford, W.; Incagli,
   M.; Jang, W. Y.; Jia, Yi; Jinchi, H.; Kanishev, K.; Khiali, B.;
   Kim, G. N.; Kirn, Th.; Konyushikhin, M.; Kounina, O.; Kounine, A.;
   Koutsenko, V.; Kuhlman, A.; Kulemzin, A.; La Vacca, G.; Laudi, E.;
   Laurenti, G.; Lazzizzera, I.; Lebedev, A.; Lee, H. T.; Lee, S. C.;
   Leluc, C.; Li, J. Q.; Li, M.; Li, Q.; Li, S.; Li, T. X.; Li, Z. H.;
   Light, C.; Lin, C. H.; Lippert, T.; Liu, Z.; Lu, S. Q.; Lu, Y. S.;
   Luebelsmeyer, K.; Luo, J. Z.; Lyu, S. S.; Machate, F.; Mañá, C.;
   Marín, J.; Marquardt, J.; Martin, T.; Martínez, G.; Masi, N.; Maurin,
   D.; Menchaca-Rocha, A.; Meng, Q.; Mo, D. C.; Molero, M.; Mott, P.;
   Mussolin, L.; Ni, J. Q.; Nikonov, N.; Nozzoli, F.; Oliva, A.; Orcinha,
   M.; Palermo, M.; Palmonari, F.; Paniccia, M.; Pashnin, A.; Pauluzzi,
   M.; Pensotti, S.; Phan, H. D.; Plyaskin, V.; Pohl, M.; Porter, S.; Qi,
   X. M.; Qin, X.; Qu, Z. Y.; Quadrani, L.; Rancoita, P. G.; Rapin, D.;
   Reina Conde, A.; Rosier-Lees, S.; Rozhkov, A.; Rozza, D.; Sagdeev,
   R.; Schael, S.; Schmidt, S. M.; Schulz von Dratzig, A.; Schwering,
   G.; Seo, E. S.; Shan, B. S.; Shi, J. Y.; Siedenburg, T.; Solano,
   C.; Song, J. W.; Sonnabend, R.; Sun, Q.; Sun, Z. T.; Tacconi, M.;
   Tang, X. W.; Tang, Z. C.; Tian, J.; Ting, Samuel C. C.; Ting, S. M.;
   Tomassetti, N.; Torsti, J.; Tüysüz, C.; Urban, T.; Usoskin, I.;
   Vagelli, V.; Vainio, R.; Valente, E.; Valtonen, E.; Vázquez Acosta,
   M.; Vecchi, M.; Velasco, M.; Vialle, J. P.; Wang, L. Q.; Wang, N. H.;
   Wang, Q. L.; Wang, S.; Wang, X.; Wang, Z. X.; Wei, J.; Weng, Z. L.;
   Wu, H.; Xiong, R. Q.; Xu, W.; Yan, Q.; Yang, Y.; Yi, H.; Yu, Y. J.;
   Yu, Z. Q.; Zannoni, M.; Zhang, C.; Zhang, F.; Zhang, F. Z.; Zhang,
   J. H.; Zhang, Z.; Zhao, F.; Zheng, Z. M.; Zhuang, H. L.; Zhukov, V.;
   Zichichi, A.; Zimmermann, N.; Zuccon, P.; AMS Collaboration
2021PhR...894....1A    Altcode:
  The Alpha Magnetic Spectrometer (AMS) is a precision particle physics
  detector on the International Space Station (ISS) conducting a unique,
  long-duration mission of fundamental physics research in space. The
  physics objectives include the precise studies of the origin of dark
  matter, antimatter, and cosmic rays as well as the exploration of new
  phenomena. Following a 16-year period of construction and testing, and
  a precursor flight on the Space Shuttle, AMS was installed on the ISS
  on May 19, 2011. In this report we present results based on 120 billion
  charged cosmic ray events up to multi-TeV energies. This includes the
  fluxes of positrons, electrons, antiprotons, protons, and nuclei. These
  results provide unexpected information, which cannot be explained by
  the current theoretical models. The accuracy and characteristics of
  the data, simultaneously from many different types of cosmic rays,
  provide unique input to the understanding of origins, acceleration,
  and propagation of cosmic rays.

---------------------------------------------------------
Title: Application of the Verified Neutron Monitor Yield Function
    for an Extended Analysis of the GLE # 71 on 17 May 2012
Authors: Mishev, A. L.; Koldobskiy, S. A.; Usoskin, I. G.; Kocharov,
   L. G.; Kovaltsov, G. A.
2021SpWea..1902626M    Altcode:
  Intense solar activity was observed in May 2012. A notable ground
  level enhancement (GLE) was registered on 17 May 2012 by several
  space borne instruments as well as on ground by neutron monitors
  (NMs). This event is known as GLE # 71. Here, we derived the spectral
  and angular characteristics, and apparent source position of the solar
  protons during the GLE # 71, employing verified newly computed NM
  yield function and sophisticated unfolding procedure. We considerably
  improved the previously derived information about the spectra and
  angular distribution, namely, the precision, time span, and time
  resolution of the derived characteristics, specifically during the
  event onset and late phase. A comparison with direct measurements,
  with the Payload for Antimatter Matter Exploration and Light nuclei
  Astrophysics (PAMELA) experiment, of the particle fluence was performed,
  and good agreement between NM and direct space borne data analysis was
  achieved. Subsequently, we computed the effective dose rates in the
  polar region at several altitudes during the event using the derived
  rigidity spectra of the solar protons as a reliable input for the
  corresponding radiation model. The contribution of the galactic cosmic
  rays and solar protons to the exposure is explicitly considered. We
  computed the integrated exposure during the event and discussed the
  exposure of crew members/passengers to radiation at several altitudes.

---------------------------------------------------------
Title: Properties of Heavy Secondary Fluorine Cosmic Rays: Results
    from the Alpha Magnetic Spectrometer
Authors: Aguilar, M.; Cavasonza, L. Ali; Allen, M. S.; Alpat, B.;
   Ambrosi, G.; Arruda, L.; Attig, N.; Barao, F.; Barrin, L.; Bartoloni,
   A.; Başeǧmez-du Pree, S.; Battiston, R.; Behlmann, M.; Beranek,
   B.; Berdugo, J.; Bertucci, B.; Bindi, V.; Bollweg, K.; Borgia, B.;
   Boschini, M. J.; Bourquin, M.; Bueno, E. F.; Burger, J.; Burger, W. J.;
   Burmeister, S.; Cai, X. D.; Capell, M.; Casaus, J.; Castellini, G.;
   Cervelli, F.; Chang, Y. H.; Chen, G. M.; Chen, G. R.; Chen, H. S.;
   Chen, Y.; Cheng, L.; Chou, H. Y.; Chouridou, S.; Choutko, V.; Chung,
   C. H.; Clark, C.; Coignet, G.; Consolandi, C.; Contin, A.; Corti, C.;
   Cui, Z.; Dadzie, K.; Delgado, C.; Della Torre, S.; Demirköz, M. B.;
   Derome, L.; Di Falco, S.; Di Felice, V.; Díaz, C.; Dimiccoli, F.;
   von Doetinchem, P.; Dong, F.; Donnini, F.; Duranti, M.; Egorov, A.;
   Eline, A.; Feng, J.; Fiandrini, E.; Fisher, P.; Formato, V.; Freeman,
   C.; Galaktionov, Y.; Gámez, C.; García-López, R. J.; Gargiulo,
   C.; Gast, H.; Gervasi, M.; Giovacchini, F.; Gómez-Coral, D. M.;
   Gong, J.; Goy, C.; Grabski, V.; Grandi, D.; Graziani, M.; Haino, S.;
   Han, K. C.; Hashmani, R. K.; He, Z. H.; Heber, B.; Hsieh, T. H.; Hu,
   J. Y.; Incagli, M.; Jang, W. Y.; Jia, Yi; Jinchi, H.; Kanishev, K.;
   Khiali, B.; Kim, G. N.; Kirn, Th.; Konyushikhin, M.; Kounina, O.;
   Kounine, A.; Koutsenko, V.; Kuhlman, A.; Kulemzin, A.; La Vacca, G.;
   Laudi, E.; Laurenti, G.; Lazzizzera, I.; Lebedev, A.; Lee, H. T.;
   Lee, S. C.; Li, J. Q.; Li, M.; Li, Q.; Li, S.; Li, J. H.; Li, Z. H.;
   Liang, J.; Light, C.; Lin, C. H.; Lippert, T.; Liu, J. H.; Liu, Z.;
   Lu, S. Q.; Lu, Y. S.; Luebelsmeyer, K.; Luo, J. Z.; Luo, Xi; Lyu,
   S. S.; Machate, F.; Mañá, C.; Marín, J.; Marquardt, J.; Martin,
   T.; Martínez, G.; Masi, N.; Maurin, D.; Menchaca-Rocha, A.; Meng,
   Q.; Mikhailov, V. V.; Mo, D. C.; Molero, M.; Mott, P.; Mussolin,
   L.; Negrete, J.; Nikonov, N.; Nozzoli, F.; Oliva, A.; Orcinha, M.;
   Palermo, M.; Palmonari, F.; Paniccia, M.; Pashnin, A.; Pauluzzi, M.;
   Pensotti, S.; Phan, H. D.; Piandani, R.; Plyaskin, V.; Poluianov,
   S.; Qin, X.; Qu, Z. Y.; Quadrani, L.; Rancoita, P. G.; Rapin, D.;
   Conde, A. Reina; Robyn, E.; Rosier-Lees, S.; Rozhkov, A.; Rozza, D.;
   Sagdeev, R.; Schael, S.; Schulz von Dratzig, A.; Schwering, G.; Seo,
   E. S.; Shakfa, Z.; Shan, B. S.; Siedenburg, T.; Solano, C.; Song,
   J. W.; Song, X. J.; Sonnabend, R.; Strigari, L.; Su, T.; Sun, Q.;
   Sun, Z. T.; Tacconi, M.; Tang, X. W.; Tang, Z. C.; Tian, J.; Ting,
   Samuel C. C.; Ting, S. M.; Tomassetti, N.; Torsti, J.; Tüysüz, C.;
   Urban, T.; Usoskin, I.; Vagelli, V.; Vainio, R.; Valencia-Otero, M.;
   Valente, E.; Valtonen, E.; Vázquez Acosta, M.; Vecchi, M.; Velasco,
   M.; Vialle, J. P.; Wang, C. X.; Wang, L.; Wang, L. Q.; Wang, N. H.;
   Wang, Q. L.; Wang, S.; Wang, X.; Wang, Yu; Wang, Z. M.; Wei, J.; Weng,
   Z. L.; Wu, H.; Xiong, R. Q.; Xu, W.; Yan, Q.; Yang, Y.; Yashin, I. I.;
   Yi, H.; Yu, Y. M.; Yu, Z. Q.; Zannoni, M.; Zhang, C.; Zhang, F.; Zhang,
   F. Z.; Zhang, J. H.; Zhang, Z.; Zhao, F.; Zheng, C.; Zheng, Z. M.;
   Zhuang, H. L.; Zhukov, V.; Zichichi, A.; Zuccon, P.; AMS Collaboration
2021PhRvL.126h1102A    Altcode:
  Precise knowledge of the charge and rigidity dependence of the
  secondary cosmic ray fluxes and the secondary-to-primary flux ratios is
  essential in the understanding of cosmic ray propagation. We report the
  properties of heavy secondary cosmic ray fluorine F in the rigidity
  R range 2.15 GV to 2.9 TV based on 0.29 million events collected
  by the Alpha Magnetic Spectrometer experiment on the International
  Space Station. The fluorine spectrum deviates from a single power
  law above 200 GV. The heavier secondary-to-primary F/Si flux ratio
  rigidity dependence is distinctly different from the lighter B/O (or
  B/C) rigidity dependence. In particular, above 10 GV, the F//Si B /O
  ratio can be described by a power law R<SUP>δ</SUP> with δ =0.052
  ±0.007 . This shows that the propagation properties of heavy cosmic
  rays, from F to Si, are different from those of light cosmic rays,
  from He to O, and that the secondary cosmic rays have two classes.

---------------------------------------------------------
Title: Robustness of Solar-Cycle Empirical Rules Across Different
    Series Including an Updated Active-Day Fraction (ADF) Sunspot
    Group Series
Authors: Usoskin, Ilya; Kovaltsov, Gennady; Kiviaho, Wilma
2021SoPh..296...13U    Altcode: 2020arXiv201208415U
  Empirical rules of solar-cycle evolution form important observational
  constraints for the solar-dynamo theory. This includes the Waldmeier
  rule relating the magnitude of a solar cycle to the length of its
  ascending phase, and the Gnevyshev-Ohl rule clustering cycles to
  pairs of an even-numbered cycle followed by a stronger odd-numbered
  cycle. These rules were established as based on the "classical" Wolf
  sunspot number series, which has been essentially revisited recently,
  with several revised sets released by the research community. Here we
  test the robustness of these empirical rules for different sunspot
  (group) series for the period 1749 - 1996, using four classical
  and revised international sunspot-number and group sunspot-number
  series. We also provide an update of the sunspot-group series based
  on the active-day fraction (ADF) method, using the new database of
  solar observations. We show that the Waldmeier rule is robust and
  independent of the exact sunspot (group) series: its classical and n +1
  (relating the length of n th cycle to the magnitude of (n +1 )th cycle)
  formulations are significant or highly significant for all series,
  while its simplified formulation (relating the magnitude of a cycle to
  its full length) is insignificant for all series. The Gnevyshev-Ohl
  rule was found robust for all analyzed series for Solar Cycles 8 -
  21, but unstable across the Dalton minimum and before it.

---------------------------------------------------------
Title: Properties of Iron Primary Cosmic Rays: Results from the
    Alpha Magnetic Spectrometer
Authors: Aguilar, M.; Cavasonza, L. Ali; Allen, M. S.; Alpat, B.;
   Ambrosi, G.; Arruda, L.; Attig, N.; Barao, F.; Barrin, L.; Bartoloni,
   A.; Başeǧmez-du Pree, S.; Battiston, R.; Behlmann, M.; Beischer,
   B.; Berdugo, J.; Bertucci, B.; Bindi, V.; de Boer, W.; Bollweg, K.;
   Borgia, B.; Boschini, M. J.; Bourquin, M.; Bueno, E. F.; Burger, J.;
   Burger, W. J.; Burmeister, S.; Cai, X. D.; Capell, M.; Casaus, J.;
   Castellini, G.; Cervelli, F.; Chang, Y. H.; Chen, G. M.; Chen, G. R.;
   Chen, H. S.; Chen, Y.; Cheng, L.; Chou, H. Y.; Chouridou, S.; Choutko,
   V.; Chung, C. H.; Clark, C.; Coignet, G.; Consolandi, C.; Contin,
   A.; Corti, C.; Cui, Z.; Dadzie, K.; Delgado, C.; Della Torre, S.;
   Demirköz, M. B.; Derome, L.; Di Falco, S.; Di Felice, V.; Díaz, C.;
   Dimiccoli, F.; von Doetinchem, P.; Dong, F.; Donnini, F.; Duranti, M.;
   Egorov, A.; Eline, A.; Feng, J.; Fiandrini, E.; Fisher, P.; Formato,
   V.; Freeman, C.; Galaktionov, Y.; Gámez, C.; García-López, R. J.;
   Gargiulo, C.; Gast, H.; Gervasi, M.; Giovacchini, F.; Gómez-Coral,
   D. M.; Gong, J.; Goy, C.; Grabski, V.; Grandi, D.; Graziani, M.; Haino,
   S.; Han, K. C.; Hashmani, R. K.; He, Z. H.; Heber, B.; Hsieh, T. H.;
   Hu, J. Y.; Incagli, M.; Jang, W. Y.; Jia, Yi; Jinchi, H.; Kanishev,
   K.; Khiali, B.; Kim, G. N.; Kirn, Th.; Konyushikhin, M.; Kounina,
   O.; Kounine, A.; Koutsenko, V.; Kuhlman, A.; Kulemzin, A.; La Vacca,
   G.; Laudi, E.; Laurenti, G.; Lazzizzera, I.; Lebedev, A.; Lee, H. T.;
   Lee, S. C.; Li, J. Q.; Li, M.; Li, Q.; Li, S.; Li, J. H.; Li, Z. H.;
   Liang, J.; Light, C.; Lin, C. H.; Lippert, T.; Liu, J. H.; Liu, Z.;
   Lu, S. Q.; Lu, Y. S.; Luebelsmeyer, K.; Luo, J. Z.; Luo, Xi; Lyu,
   S. S.; Machate, F.; Mañá, C.; Marín, J.; Marquardt, J.; Martin,
   T.; Martínez, G.; Masi, N.; Maurin, D.; Menchaca-Rocha, A.; Meng,
   Q.; Mikhailov, V. V.; Mo, D. C.; Molero, M.; Mott, P.; Mussolin,
   L.; Negrete, J.; Nikonov, N.; Nozzoli, F.; Oliva, A.; Orcinha, M.;
   Palermo, M.; Palmonari, F.; Paniccia, M.; Pashnin, A.; Pauluzzi, M.;
   Pensotti, S.; Phan, H. D.; Piandani, R.; Plyaskin, V.; Poluianov,
   S.; Qin, X.; Qu, Z. Y.; Quadrani, L.; Rancoita, P. G.; Rapin, D.;
   Conde, A. Reina; Robyn, E.; Rosier-Lees, S.; Rozhkov, A.; Rozza, D.;
   Sagdeev, R.; Schael, S.; von Dratzig, A. Schulz; Schwering, G.; Seo,
   E. S.; Shakfa, Z.; Shan, B. S.; Siedenburg, T.; Solano, C.; Song,
   J. W.; Song, X. J.; Sonnabend, R.; Strigari, L.; Su, T.; Sun, Q.;
   Sun, Z. T.; Tacconi, M.; Tang, X. W.; Tang, Z. C.; Tian, J.; Ting,
   Samuel C. C.; Ting, S. M.; Tomassetti, N.; Torsti, J.; Tüysüz, C.;
   Urban, T.; Usoskin, I.; Vagelli, V.; Vainio, R.; Valencia-Otero, M.;
   Valente, E.; Valtonen, E.; Vázquez Acosta, M.; Vecchi, M.; Velasco,
   M.; Vialle, J. P.; Wang, C. X.; Wang, L.; Wang, L. Q.; Wang, N. H.;
   Wang, Q. L.; Wang, S.; Wang, X.; Wang, Yu; Wang, Z. M.; Wei, J.;
   Weng, Z. L.; Wu, H.; Xiong, R. Q.; Xu, W.; Yan, Q.; Yang, Y.; Yashin,
   I. I.; Yi, H.; Yu, Y. M.; Yu, Z. Q.; Zannoni, M.; Zhang, C.; Zhang,
   F.; Zhang, F. Z.; Zhang, J. H.; Zhang, Z.; Zhao, F.; Zheng, C.;
   Zheng, Z. M.; Zhuang, H. L.; Zhukov, V.; Zichichi, A.; Zimmermann,
   N.; Zuccon, P.; AMS Collaboration
2021PhRvL.126d1104A    Altcode:
  We report the observation of new properties of primary iron (Fe) cosmic
  rays in the rigidity range 2.65 GV to 3.0 TV with 0.62 ×10<SUP>6</SUP>
  iron nuclei collected by the Alpha Magnetic Spectrometer experiment on
  the International Space Station. Above 80.5 GV the rigidity dependence
  of the cosmic ray Fe flux is identical to the rigidity dependence of
  the primary cosmic ray He, C, and O fluxes, with the Fe /O flux ratio
  being constant at 0.155 ±0.006 . This shows that unexpectedly Fe and
  He, C, and O belong to the same class of primary cosmic rays which is
  different from the primary cosmic rays Ne, Mg, and Si class.

---------------------------------------------------------
Title: VizieR Online Data Catalog: GLE integral intensities
    (Koldobskiy+, 2021)
Authors: Koldobskiy, S.; Raukunen, O.; Vainio, R.; Kovaltsov, G. A.;
   Usoskin, I.
2021yCat..36470132K    Altcode:
  File params.dat contains parameters of the modified Band-function
  fit of the integral flux (fluence) for SEP registered by satellite/
  ionospheric experiments and neutron monitor network (58 most powerful
  GLE events). Each string corresponds to the separate GLE event <P
  />File fluences.dat contains ready-to-use fluences (in units of
  cm<SUP>-2</SUP>) of solar energetic particles for 58 considered GLE
  events (GLE # and date are given for event identification). Fluences
  are obtained using best MBF fit and are given in log-space scale from
  0.239GV to 20GV. Fluences corresponding to energies &gt;100, &gt;430
  and &gt;1000MeV are also given. <P />(2 data files).

---------------------------------------------------------
Title: International Space Weather Action Team (ISWAT) S1: Long-term
    Solar Variability
Authors: Nandi, Dibyendu; Usoskin, Ilya; Pevtsov, Alexei
2021cosp...43E2412N    Altcode:
  The COSPAR International Space Weather Action Team (ISWAT) is a global
  hub for space weather community efforts toward the realization
  of the International Living With a Star-COSPAR Space Weather
  Roadmap goals. The community provides an inclusive environment for
  collaborative research efforts, information sharing and capacity
  building in the space weather sciences with a specific focus on
  enabling prediction and applications. Action teams within ISWAT
  address a specific focussed topic around which the team expertise
  is built. In this poster presentation we highlight the ISWAT Action
  Team S1 (Long term solar variability). The team is motivated towards
  understanding solar drivers of long term variability in the heliospheric
  space environment, its impact on geospace and other planets. This
  ISWAT Team is moderated by Dibyendu Nandi, Ilya Usoskin and Alexei
  Pevtsov. Interested scientists can join the team through the ISWAT
  website at: https://iswat-cospar.org/.

---------------------------------------------------------
Title: Validation of the updated neutron monitor yield function via
    data from AMS-02
Authors: Gil, Agnieszka; Usoskin, Ilya; Koldobskiy, Sergey; Kovaltsov,
   Gennady A.; Mishev, Alexander
2021cosp...43E.861G    Altcode:
  We present an updated yield function (YF), along with the corresponding
  parametrization, for the standard neutron monitor (NM), 6NM64, for both
  primary protons and ????-particles (the latter effectively includes
  heavier species). The updated YF was computed using the Mishev et
  al. (2013) approach, based on a full Monte Carlo simulations of the
  cosmic-ray induced atmospheric cascade, for different altitudes,
  covering the entire range of locations, from sea level to 500 g/cm$
  ^{2}$ (∼5.7 km). The validation of the updated YF was done by
  applying the cosmic-ray spectra directly measured in situ by the
  AMS-02 experiment for 79 Bartels rotations, from May 2011 through May
  2017. We confronted the modeled results with the measured count rates
  of all NM64 neutron monitors operating during the studied period. We
  also obtained the scaling factors $\kappa$, being the ratio of the
  computed to the measured NM count rates, assessing the stability of
  all the selected NMs. A list of stable NMs is provided.

---------------------------------------------------------
Title: COSPAR International Space Weather Action Teams: Addressing
    Challenges Across the Field of Space Weather.
Authors: Kuznetsova, M. M.; Belehaki, A.; Bisi, M. M.; Bruinsma, S.;
   Fung, S. F.; Glover, A.; Grande, M.; Guo, J.; Jun, I.; Linker, J.;
   Mann, I. R.; Masson, A.; Mendoza, A. M. M.; Murray, S. A.; Nandy, D.;
   Opgenoorth, H. J.; Pevtsov, A. A.; Plainaki, C.; Reiss, M.; Sutton,
   E. K.; Temmer, M.; Usoskin, I. G.; Yao, Z.; Yardley, S.; Zheng, Y.
2020AGUFMSH0030022K    Altcode:
  Advanced predictions of space weather impacts require improved
  understanding and modeling capabilities of coupled chains of space
  environment processes. It is necessary to assemble parts of the
  source-to-impact puzzle by identifying, addressing and solving
  problems focused on specific physical domains, and then to connect
  all validated solutions from space weather origins on the sun to
  impacts on coupled geospace system, humans and technologies. To
  address the need for multi-disciplinary international space weather
  research community connecting experts in space weather phenomena
  across all domains and experts in space environment impact,
  the COSPAR Panel on Space Weather facilitated establishment of
  a network of International Space Weather Action Teams (ISWAT, <A
  href="https://www.iswat-cospar.org">https://www.iswat-cospar.org</A>,
  @IswatCosparOrg). ISWAT serves as a global hub for community coordinated
  topical collaborations focused on different aspects of space weather
  including advancing understanding, assessment and improvement of
  modeling capabilities, transitioning advances in research to operations,
  optimized utilization of available observations, and generating inputs
  to future instrumentation deployment. Action teams are building
  blocks of ISWAT initiative. ISWAT action teams are organized into
  domain-based ISWAT clusters. Action teams are working in coordinated
  effort across physical domain and across borders. The primary ISWAT
  goal is to advance space weather predictive capabilities based on best
  science available. The ISWAT currently includes more than 250 active
  participants and more than 50 action teams. The presentation will
  overview the outcome from the COSPAR ISWAT Inaugural Working Meeting
  in February 2020, highlight recent progress in advancing physics-based
  predictive capabilities and discuss plans for transforming COSPAR space
  weather Roadmap into a living document maintained by the community.

---------------------------------------------------------
Title: A New Full 3-D Model of Cosmogenic Tritium <SUP>3</SUP>H
Production in the Atmosphere (CRAC:3H)
Authors: Poluianov, S. V.; Kovaltsov, G. A.; Usoskin, I. G.
2020JGRD..12533147P    Altcode: 2020arXiv200907700P
  A new model of cosmogenic tritium (<SUP>3</SUP>H) production in the
  atmosphere is presented. The model belongs to the CRAC (Cosmic Ray
  Atmospheric Cascade) family and is named as CRAC:3H. It is based on
  a full Monte Carlo simulation of the cosmic ray induced atmospheric
  cascade using the Geant4 toolkit. The CRAC:3H model is able, for the
  first time, to compute tritium production at any location and time, for
  any given energy spectrum of the primary incident cosmic ray particles,
  explicitly treating, also for the first time, particles heavier than
  protons. This model provides a useful tool for the use of <SUP>3</SUP>H
  as a tracer of atmospheric and hydrological circulation. A numerical
  recipe for practical use of the model is appended.

---------------------------------------------------------
Title: Revised GLE database: Fluences of solar energetic particles
    as measured by the neutron-monitor network since 1956
Authors: Usoskin, I.; Koldobskiy, S.; Kovaltsov, G. A.; Gil, A.;
   Usoskina, I.; Willamo, T.; Ibragimov, A.
2020A&A...640A..17U    Altcode:
  <BR /> Aims: Continuous measurements of ground-based neutron
  monitors (NMs) form the main data source for studying high-energy
  high-intensity solar energetic particle (SEP) events that are called
  ground-level enhancements (GLEs). All available data are collected
  in the International GLE Database (IGLED), which provides formal NM
  count-rate increases above the constant pre-increase level which is due
  to galactic cosmic rays (GCR). This data set is used to reconstruct the
  energy spectra of GLE events. However, the assumption of a constant
  GCR background level throughout GLE events is often invalid. Here we
  thoroughly revise the IGLED and provide a data set of detrended NM
  count-rate increases that accounts for the variable GCR background. <BR
  /> Methods: The formal GLE count-rate increases were corrected for
  the variable GCR background, which may vary significantly during GLE
  events. The corresponding integral omnidirectional fluences of SEPs
  were reconstructed for all GLEs with sufficient strength from the
  detrended data using the effective rigidity method. <BR /> Results:
  The database of the detrended NM count rate is revised for GLE events
  since 1956. Integral omnidirectional fluences were estimated for 58
  GLE events and parametrised for 52 sufficiently strong events using
  the modified Ellison-Ramaty spectral shape. <BR /> Conclusions: The
  IGLED was revised to account for the variable GCR background. Integral
  omnidirectional fluences reconstructed for most of GLE events were
  added to IGLED. This forms the basis for more precise studies of
  parameters of SEP events and thus for solar and space physics. <P />The
  revised fluences are only available at the CDS via anonymous ftp to <A
  href="http://cdsarc.u-strasbg.fr/">http://cdsarc.u-strasbg.fr</A>
  (ftp://130.79.128.5) or via <A
  href="http://cdsarc.u-strasbg.fr/viz-bin/cat/J/A+A/640/A17">http://cdsarc.u-strasbg.fr/viz-bin/cat/J/A+A/640/A17</A>

---------------------------------------------------------
Title: The mini-neutron monitor: a new approach in neutron monitor
    design
Authors: Strauss, Du Toit; Poluianov, Stepan; van der Merwe, Cobus;
   Krüger, Hendrik; Diedericks, Corrie; Krüger, Helena; Usoskin,
   Ilya; Heber, Bernd; Nndanganeni, Rendani; Blanco-Ávalos, Juanjo;
   García-Tejedor, Ignacio; Herbst, Konstantin; Caballero-Lopez,
   Rogelio; Moloto, Katlego; Lara, Alejandro; Walter, Michael; Giday,
   Nigussie Mezgebe; Traversi, Rita
2020JSWSC..10...39S    Altcode:
  The near-Earth cosmic ray flux has been monitored for more than 70
  years by a network of ground-based neutron monitors (NMs). With
  the ever-increasing importance of quantifying the radiation risk
  and effects of cosmic rays for, e.g., air and space-travel, it is
  essential to continue operating the existing NM stations, while
  expanding this crucial network. In this paper, we discuss a smaller
  and cost-effective version of the traditional NM, the mini-NM. These
  monitors can be deployed with ease, even to extremely remote locations,
  where they operate in a semi-autonomous fashion. We believe that the
  mini-NM, therefore, offers the opportunity to increase the sensitivity
  and expand the coverage of the existing NM network, making this
  network more suitable to near-real-time monitoring for space weather
  applications. In this paper, we present the technical details of the
  mini-NM's design and operation, and present a summary of the initial
  tests and science results.

---------------------------------------------------------
Title: Natural Sources of Ionization and Their Impact on Atmospheric
    Electricity
Authors: Golubenko, K.; Rozanov, E.; Mironova, I.; Karagodin, A.;
   Usoskin, I.
2020GeoRL..4788619G    Altcode:
  We present a study of atmospheric electricity using the
  chemistry-climate model SOCOL considering ionization by solar energetic
  particles during an extreme solar proton event (SPE), galactic cosmic
  rays (GCR), and terrestrial radon (Rn-222). We calculate the global
  distribution of the atmospheric conductivity and fair-weather downward
  current density (J<SUB>z</SUB>) using atmospheric ionization rates
  from all sources. We found that J<SUB>z</SUB> is enhanced (by more than
  3.5 pA/m<SUP>2</SUP>) in radon source and polar regions. Contribution
  of Rn-222 is essential at middle and low latitudes/altitudes where
  GCR-induced air conductivity is reduced. The model results are in
  good agreement with the available observations. We also studied the
  effects of an extreme SPE, corresponding to the 774 AD event, on
  the atmospheric electricity and found that it would lead to a large
  increase of J<SUB>z</SUB> on a global scale. The magnitude of the
  effects depends on location and can exceed background value more than
  30 times over the high latitudes (a conservative upper bound). Such
  an assessment has been performed for the first time.

---------------------------------------------------------
Title: VizieR Online Data Catalog: CR Ground Level Enhancements
    spectra (IGLED) (Usoskin+, 2020)
Authors: Usoskin, I. G.; Koldobskiy, S.; Kovaltsov, G. A.; Gil, A.;
   Usoskina, I.; Willamo, T.; Ibragimov, A.
2020yCat..36400017U    Altcode:
  Files (names as 'GLEXX_spec.dat') contain, for each GLE event numbered
  as XX, name [Name], vertical geomagnetic cutoff rigidity [Pc], nominal
  atmospheric depth [h], the integral GLE intensity [X], reconstructed
  effective rigidity [Re] along with its full-range lower [e_Re] and upper
  [E_Re] uncertainties, omni-directional integral fluence F(&gt;Re)
  [F] along with its full-range lower [e<SUB>F] and upper [E</SUB>F]
  uncertainties, for all NMs with available data. F=0 implies that only
  the upper limit on F(&gt;Re) can be provided. <P />(2 data files).

---------------------------------------------------------
Title: Revisited Reference Solar Proton Event of 23 February 1956:
    Assessment of the Cosmogenic-Isotope Method Sensitivity to Extreme
    Solar Events
Authors: Usoskin, Ilya G.; Koldobskiy, Sergey A.; Kovaltsov, Gennady
   A.; Rozanov, Eugene V.; Sukhodolov, Timofei V.; Mishev, Alexander L.;
   Mironova, Irina A.
2020JGRA..12527921U    Altcode: 2020arXiv200510597U
  Our direct knowledge of solar eruptive events is limited to several
  decades and does not include extreme events, which can only be studied
  by the indirect proxy method over millennia, or by a large number
  of Sun-like stars. There is a gap, spanning 1-2 orders of magnitude,
  in the strength of events between directly observed and reconstructed
  ones. Here, we study the proxy method sensitivity to identify extreme
  solar particle events (SPEs). First, the strongest directly observed SPE
  (23 February 1956), used as a reference for proxy-based reconstructions,
  was revisited using the newly developed method. Next, sensitivity of
  the cosmogenic-isotope method to detect a reference SPE was assessed
  against the precision and number of individual isotopic records, showing
  that it is too weak by a factor ≈30 to be reliably identified in a
  single record. Uncertainties of <SUP>10</SUP>Be and <SUP>14</SUP>C data
  are shown to be dominated by local/regional patterns and measurement
  errors, respectively. By combining several proxy records, a SPE 4-5
  times stronger than the reference one can be potentially detected,
  increasing the present-day sensitivity by an order of magnitude. This
  will allow filling the observational gap in SPE strength distribution,
  thus enriching statistics of extreme events from 3-4 presently known
  ones to several tens. This will provide a solid basis for research
  in the field of extreme events, both for fundamental science, namely
  solar and stellar physics, and practical applications, such as the
  risk assessments of severe space-based hazards for modern technological
  society.

---------------------------------------------------------
Title: Current status and possible extension of the global neutron
    monitor network
Authors: Mishev, Alexander; Usoskin, Ilya
2020JSWSC..10...17M    Altcode: 2020arXiv200512621M
  The global neutron monitor network has been successfully used over
  several decades to study cosmic ray variations and fluxes of energetic
  solar particles. Nowadays, it is used also for space weather purposes,
  e.g. alerts and assessment of the exposure to radiation. Here, we
  present the current status of the global neutron monitor network. We
  discuss the ability of the global neutron monitor network to study
  solar energetic particles, specifically during large ground level
  enhancements. We demonstrate as an example, the derived solar proton
  characteristics during ground level enhancements GLE #5 and the
  resulting effective dose over the globe at a typical commercial jet
  flight altitude of 40 kft (≈12,200 m) above sea level. We present
  a plan for improvement of space weather services and applications of
  the global neutron monitor network, specifically for studies related to
  solar energetic particles, namely an extension of the existing network
  with several new monitors. We discuss the ability of the optimized
  global neutron monitor network to study various populations of solar
  energetic particles and to provide reliable space weather services.

---------------------------------------------------------
Title: Properties of Neon, Magnesium, and Silicon Primary Cosmic
    Rays Results from the Alpha Magnetic Spectrometer
Authors: Aguilar, M.; Ali Cavasonza, L.; Ambrosi, G.; Arruda, L.;
   Attig, N.; Barao, F.; Barrin, L.; Bartoloni, A.; Başeǧmez-du Pree,
   S.; Battiston, R.; Becker, U.; Behlmann, M.; Beischer, B.; Berdugo,
   J.; Bertucci, B.; Bindi, V.; de Boer, W.; Bollweg, K.; Borgia, B.;
   Boschini, M. J.; Bourquin, M.; Bueno, E. F.; Burger, J.; Burger,
   W. J.; Burmeister, S.; Cai, X. D.; Capell, M.; Casaus, J.; Castellini,
   G.; Cervelli, F.; Chang, Y. H.; Chen, G. M.; Chen, H. S.; Chen, Y.;
   Cheng, L.; Chou, H. Y.; Chouridou, S.; Choutko, V.; Chung, C. H.;
   Clark, C.; Coignet, G.; Consolandi, C.; Contin, A.; Corti, C.; Cui,
   Z.; Dadzie, K.; Dai, Y. M.; Delgado, C.; Della Torre, S.; Demirköz,
   M. B.; Derome, L.; Di Falco, S.; Di Felice, V.; Díaz, C.; Dimiccoli,
   F.; von Doetinchem, P.; Dong, F.; Donnini, F.; Duranti, M.; Egorov, A.;
   Eline, A.; Feng, J.; Fiandrini, E.; Fisher, P.; Formato, V.; Freeman,
   C.; Galaktionov, Y.; Gámez, C.; García-López, R. J.; Gargiulo, C.;
   Gast, H.; Gebauer, I.; Gervasi, M.; Giovacchini, F.; Gómez-Coral,
   D. M.; Gong, J.; Goy, C.; Grabski, V.; Grandi, D.; Graziani, M.;
   Guo, K. H.; Haino, S.; Han, K. C.; Hashmani, R. K.; He, Z. H.; Heber,
   B.; Hsieh, T. H.; Hu, J. Y.; Huang, Z. C.; Incagli, M.; Jang, W. Y.;
   Jia, Yi; Jinchi, H.; Kanishev, K.; Khiali, B.; Kim, G. N.; Kirn, Th.;
   Konyushikhin, M.; Kounina, O.; Kounine, A.; Koutsenko, V.; Kuhlman,
   A.; Kulemzin, A.; La Vacca, G.; Laudi, E.; Laurenti, G.; Lazzizzera,
   I.; Lebedev, A.; Lee, H. T.; Lee, S. C.; Li, J. Q.; Li, M.; Li, Q.;
   Li, S.; Li, T. X.; Li, Z. H.; Light, C.; Lin, C. H.; Lippert, T.;
   Liu, Z.; Lu, S. Q.; Lu, Y. S.; Luebelsmeyer, K.; Luo, J. Z.; Lyu,
   S. S.; Machate, F.; Mañá, C.; Marín, J.; Marquardt, J.; Martin,
   T.; Martínez, G.; Masi, N.; Maurin, D.; Menchaca-Rocha, A.; Meng,
   Q.; Mo, D. C.; Molero, M.; Mott, P.; Mussolin, L.; Ni, J. Q.; Nikonov,
   N.; Nozzoli, F.; Oliva, A.; Orcinha, M.; Palermo, M.; Palmonari, F.;
   Paniccia, M.; Pashnin, A.; Pauluzzi, M.; Pensotti, S.; Phan, H. D.;
   Piandani, R.; Plyaskin, V.; Poluianov, S.; Qi, X. M.; Qin, X.; Qu,
   Z. Y.; Quadrani, L.; Rancoita, P. G.; Rapin, D.; Reina Conde, A.;
   Rosier-Lees, S.; Rozhkov, A.; Rozza, D.; Sagdeev, R.; Schael, S.;
   Schmidt, S. M.; Schulz von Dratzig, A.; Schwering, G.; Seo, E. S.;
   Shan, B. S.; Shi, J. Y.; Siedenburg, T.; Solano, C.; Sonnabend,
   R.; Song, J. W.; Sun, Q.; Sun, Z. T.; Tacconi, M.; Tang, X. W.;
   Tang, Z. C.; Tian, J.; Ting, Samuel C. C.; Ting, S. M.; Tomassetti,
   N.; Torsti, J.; Tüysüz, C.; Urban, T.; Usoskin, I.; Vagelli, V.;
   Vainio, R.; Valente, E.; Valtonen, E.; Vázquez Acosta, M.; Vecchi, M.;
   Velasco, M.; Vialle, J. P.; Wallmann, C.; Wang, L. Q.; Wang, N. H.;
   Wang, Q. L.; Wang, S.; Wang, X.; Wang, Z. X.; Wei, J.; Weng, Z. L.;
   Wu, H.; Xiong, R. Q.; Xu, W.; Yan, Q.; Yang, Y.; Yi, H.; Yu, Y. J.;
   Yu, Z. Q.; Zannoni, M.; Zhang, C.; Zhang, F.; Zhang, F. Z.; Zhang,
   J. H.; Zhang, Z.; Zhao, F.; Zheng, Z. M.; Zhuang, H. L.; Zhukov, V.;
   Zichichi, A.; Zimmermann, N.; Zuccon, P.; AMS Collaboration
2020PhRvL.124u1102A    Altcode:
  We report the observation of new properties of primary cosmic rays, neon
  (Ne), magnesium (Mg), and silicon (Si), measured in the rigidity range
  2.15 GV to 3.0 TV with 1.8 ×10<SUP>6</SUP> Ne , 2.2 ×10<SUP>6</SUP>
  Mg , and 1.6 ×10<SUP>6</SUP> Si nuclei collected by the Alpha Magnetic
  Spectrometer experiment on the International Space Station. The Ne and
  Mg spectra have identical rigidity dependence above 3.65 GV. The three
  spectra have identical rigidity dependence above 86.5 GV, deviate
  from a single power law above 200 GV, and harden in an identical
  way. Unexpectedly, above 86.5 GV the rigidity dependence of primary
  cosmic rays Ne, Mg, and Si spectra is different from the rigidity
  dependence of primary cosmic rays He, C, and O. This shows that the
  Ne, Mg, and Si and He, C, and O are two different classes of primary
  cosmic rays.

---------------------------------------------------------
Title: Big Data Processing and Modeling in Solar Physics
Authors: Huang, X.; Usoskin, I.; Zhang, L. Y.; Wang, H. N.
2020AdAst2020E...2H    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: Updated Neutron-Monitor Yield Function: Bridging Between In
    Situ and Ground-Based Cosmic Ray Measurements
Authors: Mishev, Alexander L.; Koldobskiy, Sergey A.; Kovaltsov,
   Gennady A.; Gil, Agnieszka; Usoskin, Ilya G.
2020JGRA..12527433M    Altcode:
  An updated yield function for a standard NM64 neutron monitor (NM)
  is computed and extended to different atmospheric depths from sea
  level to 500 g/cm<SUP>2</SUP> (∼5.7 km altitude) and is presented
  as lookup tables and a full parametrization. The yield function was
  validated using the cosmic ray spectra directly measured in space by
  the AMS-02 experiment during the period May 2011 through May 2017 and
  confronted with count rates of all NM64-type NMs being in operation
  during this period. Using this approach, stability of all the selected
  NMs was analyzed for the period 2011-2017. Most of NMs appear very
  stable and suitable for studies of long-term solar modulation of
  cosmic rays. However, some NMs suffer from instabilities like trends,
  apparent jumps, or strong seasonal waves in the count rates.

---------------------------------------------------------
Title: Interplanetary Protons versus Interacting Protons in the 2017
    September 10 Solar Eruptive Event
Authors: Kocharov, Leon; Pesce-Rollins, Melissa; Laitinen, Timo;
   Mishev, Alexander; Kühl, Patrick; Klassen, Andreas; Jin, Meng;
   Omodei, Nicola; Longo, Francesco; Webb, David F.; Cane, Hilary V.;
   Heber, Bernd; Vainio, Rami; Usoskin, Ilya
2020ApJ...890...13K    Altcode:
  We analyze the relativistic proton emission from the Sun during the
  eruptive event on 2017 September 10, which caused a ground-level
  enhancement (GLE 72) registered by the worldwide network of
  neutron monitors. Using the neutron monitor data and interplanetary
  transport modeling both along and across interplanetary magnetic
  field (IMF) lines, we deduce parameters of the proton injection into
  the interplanetary medium. The inferred injection profile of the
  interplanetary protons is compared with the profile of the &gt;100 MeV
  γ-ray emission observed by the Fermi Large Area Telescope, attributed
  to pion production from the interaction of &gt;300 MeV protons at
  the Sun. GLE 72 started with a prompt component that arrived along
  the IMF lines. This was followed by a more prolonged enhancement
  caused by protons arriving at the Earth across the IMF lines from
  the southwest. The interplanetary proton event is modeled using two
  sources—one source at the root of the Earth-connected IMF line and
  another source situated near the solar western limb. The maximum
  phase of the second injection of interplanetary protons coincides
  with the maximum phase of the prolonged &gt;100 MeV γ-ray emission
  that originated from a small area at the solar western limb, below the
  current sheet trailing the associated coronal mass ejection (CME). A
  possible common source of interacting protons and interplanetary
  protons is discussed in terms of proton acceleration at the CME bow
  shock versus coronal (re-)acceleration in the wake of the CME.

---------------------------------------------------------
Title: Spectral characteristic of mid-term quasi-periodicities in
    sunspot data
Authors: Frick, P.; Sokoloff, D.; Stepanov, R.; Pipin, V.; Usoskin, I.
2020MNRAS.491.5572F    Altcode: 2019arXiv191106881F
  Numerous analyses suggest the existence of various quasi-periodicities
  in solar activity. The power spectrum of solar activity recorded
  in sunspot data is dominated by the ∼11-yr quasi-periodicity,
  known as the Schwabe cycle. In the mid-term range (1 month-11 yr)
  a pronounced variability known as a quasi-biennial oscillation
  is widely discussed. In the shorter time-scale a pronounced peak,
  corresponding to the synodic solar rotation period (∼27 d), is
  observed. Here we revisit the mid-term solar variability in terms of
  statistical dynamics of fully turbulent systems, where solid arguments
  are required to accept an isolated dominant frequency in a continuous
  (smooth) spectrum. For this, we first undertook an unbiased analysis
  of the standard solar data, sunspot numbers and the F10.7 solar radio
  flux index, by applying a wavelet tool, which allows one to perform
  a frequency-time analysis of the signal. Considering the spectral
  dynamics of solar activity cycle by cycle, we showed that no single
  periodicity can be separated, in a statistically significant manner,
  in the specified range of periods. We examine whether a model of the
  solar dynamo can reproduce the mid-term oscillation pattern observed
  in solar data. We found that a realistically observed spectrum can be
  explained if small spatial (but not temporal) scales are effectively
  smoothed. This result is important because solar activity is a global
  feature, although monitored via small-scale tracers like sunspots.

---------------------------------------------------------
Title: What Can Be Learned from Modern Data?
Authors: Kusano, K.; Cliver, E.; Hayakawa, H.; Kovaltsov, G. A.;
   Usoskin, I. G.
2019esps.book....2K    Altcode:
  Our detailed knowledge about the Sun comes from instrumental
  observations, the precision and sophistication of which have rapidly
  increased over the last decades. The primary focus of this book lies in
  solar eruptive events. This chapter provides a review of what we know
  about solar eruptive events, especially about the strongest observed
  ones, from precise modern data.

---------------------------------------------------------
Title: Cosmogenic Isotopes as Proxies for Solar Energetic Particles
Authors: Jull, T.; Baroni, M.; Feinberg, A.; Kovaltsov, G.; Mekhaldi,
   F.; Muscheler, R.; Poluianov, S.; Rozanov, E.; Sukhodolov, T.; Usoskin,
   I. G.
2019esps.book....4J    Altcode:
  Since the statistic of solar events based on direct observational data
  is not sufficient to assess extreme events (see Chapter 2), indirect
  proxy data needs to be used. The principles and details of the use
  of cosmogenic isotopes as a proxy for solar energetic particles are
  presented in this chapter.

---------------------------------------------------------
Title: Extreme Solar Particle Storms; The hostile Sun
Authors: Miyake, Fusa; Usoskin, Ilya; Poluianov, Stepan
2019esps.book.....M    Altcode:
  It is becoming increasingly clear that our modern technological
  society is vulnerable to the impacts of severe solar storms, radiation,
  particle and geomagnetic disturbances. However, the potential severity
  of these extreme solar events and their probability of occurring are
  unknown. What can we expect from the Sun? What could the most severe
  solar particle storms look like? Does the Sun have an unlimited ability
  to produce severe storms? Can a destructive “black swan” event
  occur? Direct solar data covers only several decades, a period too
  short to answer these questions. Fortunately, other indirect ways to
  study these possibly rare extreme solar storms have been discovered,
  paving the way for analysis of these events on the multi-millennial
  time scale. At present, studies of extreme solar events are growing,
  forming a new research discipline. This book, written by leaders in
  the corresponding aspects of the field, presents a first systematic
  review of the current state of the art.

---------------------------------------------------------
Title: Further Search for Extreme Events
Authors: Miyake, F.; Ebihara, Y.; Hayakawa, H.; Maehara, H.; Mitsuma,
   Y.; Usoskin, I.; Wang, F.; Willis, D. M.
2019esps.book....7M    Altcode:
  Not all possible datasets about extreme solar events in the past
  are explored currently; we are still at the beginning of a long
  path. It is likely that more events can be identified in the past,
  and the parameters of the found ones will be defined with higher
  accuracy. Prospects for the further searches for extreme solar events
  are summarized in this chapter.

---------------------------------------------------------
Title: Introduction
Authors: Usoskin, I.; Miyake, F.
2019esps.book....1U    Altcode:
  This chapter introduces the concept of extreme solar events.

---------------------------------------------------------
Title: Properties of Cosmic Helium Isotopes Measured by the Alpha
    Magnetic Spectrometer
Authors: Aguilar, M.; Ali Cavasonza, L.; Ambrosi, G.; Arruda, L.;
   Attig, N.; Bachlechner, A.; Barao, F.; Barrau, A.; Barrin, L.;
   Bartoloni, A.; Başeǧmez-du Pree, S.; Battiston, R.; Becker, U.;
   Behlmann, M.; Beischer, B.; Berdugo, J.; Bertucci, B.; Bindi, V.;
   de Boer, W.; Bollweg, K.; Borgia, B.; Boschini, M. J.; Bourquin,
   M.; Bueno, E. F.; Burger, J.; Burger, W. J.; Cai, X. D.; Capell,
   M.; Caroff, S.; Casaus, J.; Castellini, G.; Cervelli, F.; Chang,
   Y. H.; Chen, G. M.; Chen, H. S.; Chen, Y.; Cheng, L.; Chou, H. Y.;
   Choutko, V.; Chung, C. H.; Clark, C.; Coignet, G.; Consolandi, C.;
   Contin, A.; Corti, C.; Cui, Z.; Dadzie, K.; Dai, Y. M.; Datta, A.;
   Delgado, C.; Della Torre, S.; Demirköz, M. B.; Derome, L.; Di Falco,
   S.; Di Felice, V.; Díaz, C.; Dimiccoli, F.; von Doetinchem, P.;
   Dong, F.; Donnini, F.; Duranti, M.; Egorov, A.; Eline, A.; Feng, J.;
   Fiandrini, E.; Fisher, P.; Formato, V.; Galaktionov, Y.; Gámez, C.;
   García-López, R. J.; Gargiulo, C.; Gast, H.; Gebauer, I.; Gervasi,
   M.; Giovacchini, F.; Gómez-Coral, D. M.; Gong, J.; Goy, C.; Grabski,
   V.; Grandi, D.; Graziani, M.; Guo, K. H.; Haino, S.; Han, K. C.; He,
   Z. H.; Hsieh, T. H.; Huang, H.; Huang, Z. C.; Incagli, M.; Jang,
   W. Y.; Jia, Yi; Jinchi, H.; Kanishev, K.; Khiali, B.; Kim, G. N.;
   Kirn, Th.; Konyushikhin, M.; Kounina, O.; Kounine, A.; Koutsenko, V.;
   Kulemzin, A.; La Vacca, G.; Laudi, E.; Laurenti, G.; Lazzizzera, I.;
   Lebedev, A.; Lee, H. T.; Lee, S. C.; Li, J. Q.; Li, Q.; Li, T. X.;
   Li, Z. H.; Light, C.; Lin, C. H.; Lippert, T.; Liu, Z.; Lu, S. Q.;
   Lu, Y. S.; Luebelsmeyer, K.; Luo, F.; Luo, J. Z.; Luo, Xi; Lyu, S. S.;
   Machate, F.; Mañá, C.; Marín, J.; Martin, T.; Martínez, G.; Masi,
   N.; Maurin, D.; Menchaca-Rocha, A.; Meng, Q.; Mo, D. C.; Molero, M.;
   Mott, P.; Mussolin, L.; Nelson, T.; Ni, J. Q.; Nikonov, N.; Nozzoli,
   F.; Oliva, A.; Orcinha, M.; Palermo, M.; Palmonari, F.; Paniccia,
   M.; Pashnin, A.; Pauluzzi, M.; Pensotti, S.; Phan, H. D.; Plyaskin,
   V.; Poireau, V.; Poluianov, S.; Popkow, A.; Qi, X. M.; Qin, X.; Qu,
   Z. Y.; Quadrani, L.; Rancoita, P. G.; Rapin, D.; Reina Conde, A.;
   Rosier-Lees, S.; Rozhkov, A.; Rozza, D.; Sagdeev, R.; Schael, S.;
   Schmidt, S. M.; Schulz von Dratzig, A.; Schwering, G.; Seo, E. S.;
   Shan, B. S.; Shi, J. Y.; Siedenburg, T.; Solano, C.; Song, J. W.;
   Sun, Z. T.; Tacconi, M.; Tang, X. W.; Tang, Z. C.; Tian, J.; Ting,
   Samuel C. C.; Ting, S. M.; Tomassetti, N.; Torsti, J.; Tüysüz,
   C.; Urban, T.; Usoskin, I.; Vagelli, V.; Vainio, R.; Valente, E.;
   Valtonen, E.; Vázquez Acosta, M.; Vecchi, M.; Velasco, M.; Vialle,
   J. P.; Wang, L. Q.; Wang, N. H.; Wang, Q. L.; Wang, X.; Wang, X. Q.;
   Wang, Z. X.; Wei, J.; Weng, Z. L.; Wu, H.; Xiong, R. Q.; Xu, W.; Yan,
   Q.; Yang, Y.; Yi, H.; Yu, Y. J.; Yu, Z. Q.; Zannoni, M.; Zeissler, S.;
   Zhang, C.; Zhang, F.; Zhang, J. H.; Zhang, Z.; Zhao, F.; Zheng, Z. M.;
   Zhuang, H. L.; Zhukov, V.; Zichichi, A.; Zimmermann, N.; Zuccon, P.;
   AMS Collaboration
2019PhRvL.123r1102A    Altcode:
  Precision measurements by the Alpha Magnetic Spectrometer (AMS) on the
  International Space Station of <SUP>3</SUP>He <SUP>4</SUP>4 fluxes are
  presented. The measurements are based on 100 million <SUP>4</SUP>He
  nuclei in the rigidity range from 2.1 to 21 GV and 18 million
  <SUP>3</SUP>He from 1.9 to 15 GV collected from May 2011 to November
  2017. We observed that the <SUP>3</SUP>He and <SUP>4</SUP>He fluxes
  exhibit nearly identical variations with time. The relative magnitude
  of the variations decreases with increasing rigidity. The rigidity
  dependence of the <SUP>3</SUP>He/<SUP>4</SUP>He flux ratio is measured
  for the first time. Below 4 GV, the <SUP>3</SUP>He/<SUP>4</SUP>He flux
  ratio was found to have a significant long-term time dependence. Above
  4 GV, the <SUP>3</SUP>He/<SUP>4</SUP>He flux ratio was found to be time
  independent, and its rigidity dependence is well described by a single
  power law ∝R<SUP>Δ</SUP> with Δ =-0.294 ±0.004 . Unexpectedly,
  this value is in agreement with the B/O and B/C spectral indices at
  high energies.

---------------------------------------------------------
Title: New Method of Assessment of the Integral Fluence of Solar
    Energetic (&gt; 1 GV Rigidity) Particles from Neutron Monitor Data
Authors: Koldobskiy, Sergey A.; Kovaltsov, Gennady A.; Mishev,
   Alexander L.; Usoskin, Ilya G.
2019SoPh..294...94K    Altcode:
  A new method to reconstruct the high-rigidity part (≥ 1 GV)
  of the spectral fluence of solar energetic particles (SEP) for
  GLE events, based on the world-wide neutron monitor (NM) network
  data, is presented. The method is based on the effective rigidity
  R<SUB>eff</SUB> and scaling factor K<SUB>eff</SUB>. In contrast to
  many other methods based on derivation of the best-fit parameters
  of a prescribed spectral shape, it provides a true non-parametric
  (viz. free of a priori assumptions on the exact spectrum) estimate
  of fluence. We reconstructed the SEP fluences for two recent GLE
  events, #69 (20 Jan. 2005) and #71 (17 May 2012), using four NM yield
  functions: (CD00 - Clem and Dorman in Space Sci. Rev.93, 335, 2000),
  (CM12 - Caballero-Lopez and Moraal in J. Geophys. Res.117, A12103,
  2012), (Mi13 - Mishev, Usoskin, and Kovaltsov in J. Geophys. Res.118,
  2783, 2013), and (Ma16 - Mangeard et al. in J. Geophys. Res.121, 7435,
  2016b). The results were compared with full reconstructions and direct
  measurements by the PAMELA instrument. While reconstructions based on
  Mi13 and CM12 yield functions are consistent with the measurements,
  those based on CD00 and Ma16 ones underestimate the fluence by a factor
  of 2 - 3. It is also shown that the often used power-law approximation
  of the high-energy tail of SEP spectrum does not properly describe the
  GLE spectrum in the NM-energy range. Therefore, the earlier estimates
  of GLE integral fluences need to be revised.

---------------------------------------------------------
Title: A neutron monitor as an integral spectrometer for GLE analysis:
    Effective rigidity and reassessment of integral fluxes
Authors: Koldobskiy, S.; Mishev, A.; Kovaltsov, G.; Usoskin, I.
2019ICRC...36.1093K    Altcode: 2019PoS...358.1093K
  No abstract at ADS

---------------------------------------------------------
Title: Usage of the global NM network for assessment of the radiation
    exposure at flight altitudes
Authors: Mishev, A.; Usoskin, I.
2019ICRC...36.1123M    Altcode: 2019PoS...358.1123M
  No abstract at ADS

---------------------------------------------------------
Title: Multi-NM spectral slope analysis of long-term cosmic-ray
    variations at Earth
Authors: Usoskin, I.; Väisänen, P.; Mursula, K.
2019ICRC...36.1165U    Altcode: 2019PoS...358.1165U
  No abstract at ADS

---------------------------------------------------------
Title: Cosmic-ray variability on the multi-millennial time scale:
    A new multi-proxy reconstruction
Authors: Usoskin, I.; Wu, C. J.; Krivova, N.; Solanki, S. K.;
   Kovaltsov, G.; Baroni, M.; Bard, E.
2019ICRC...36.1164U    Altcode: 2019PoS...358.1164U
  No abstract at ADS

---------------------------------------------------------
Title: Validation of the neutron monitor yield functions using data
    from AMS-02 and PAMELA experiments, 2006-2017
Authors: Koldobskiy, S.; Bindi, V.; Corti, C.; Kovaltsov, G.;
   Usoskin, I.
2019ICRC...36.1094K    Altcode: 2019PoS...358.1094K
  No abstract at ADS

---------------------------------------------------------
Title: Spectra of solar energetic particle and galactic cosmic rays
    over a million years reconstructed using aluminium-26 data from
    lunar rocks
Authors: Poluianov, S.; Kovaltsov, G.; Usoskin, I.
2019ICRC...36.1139P    Altcode: 2019PoS...358.1139P
  No abstract at ADS

---------------------------------------------------------
Title: Neutron monitor yield function at several altitudes above
sea level: new improved computation
Authors: Mishev, A.; Kovaltsov, G.; Usoskin, I.
2019ICRC...36.1125M    Altcode: 2019PoS...358.1125M
  No abstract at ADS

---------------------------------------------------------
Title: Spectra of extreme GLEs derived using neutron monitor network
    records
Authors: Mishev, A.; Usoskin, I.
2019ICRC...36.1124M    Altcode: 2019PoS...358.1124M
  No abstract at ADS

---------------------------------------------------------
Title: Historical astronomical data: urgent need for preservation,
    digitization enabling scientific exploration
Authors: Pevtsov, Alexei; Griffin, Elizabeth; Grindlay, Jonathan;
   Kafka, Stella; Bartlett, Jennifer; Usoskin, Ilya; Mursula, Kalevi;
   Gibson, Sarah; Pillet, Valentín; Burkepile, Joan; Webb, David; Clette,
   Frédéric; Hesser, James; Stetson, Peter; Muñoz-Jaramillo, Andres;
   Hill, Frank; Bogart, Rick; Osborn, Wayne; Longcope, Dana
2019BAAS...51c.190P    Altcode: 2019arXiv190304839P; 2019astro2020T.190P
  This white paper emphasizes critical importance of preservation,
  digitization and scientific exploration of historical astronomical
  data. It outlines the rationale, provides examples of new science
  with such data, and reviews the potential losses to science if nothing
  it done.

---------------------------------------------------------
Title: Normalization of the neutron monitor response to cosmic rays
    using AMS-02 measurements
Authors: Usoskin, Ilya; Koldobsky, Sergey; Kovaltsov, Gennady
2019EGUGA..21.4226U    Altcode:
  A network of ground-based neutron monitors (NMs) is the main tool to
  study cosmic ray variability on long-term scales. However, still there
  is a systematic uncertainty related to the yield function of a NM to
  cosmic ray variability, as several presently used yield functions offer
  different results. Until recently, it was hardly possible to directly
  verify and validate the NM yield functions, but the new measurements
  of cosmic ray spectra by AMS-02 experiment give, for the first time,
  such a possibility. Here we present a detailed analysis of the NM
  data and AMS02-base spectra for the period May 2011 through May 2017,
  and validate the existing yield functions. We show that the yield
  function by Mishev et al. (2013) provides the results which yields the
  best agreement with data. We also provide a new way to parameterize
  contribution of heavier cosmic ray species (helium to iron) to NM
  count rate.

---------------------------------------------------------
Title: An analysis of the spectral properties of long-term galactic
    cosmic ray variability in the heliosphere via a multiple-dataset study
Authors: Väisänen, Pauli; Usoskin, Ilya; Mursula, Kalevi
2019EGUGA..2117690V    Altcode:
  The heliosphere is formed by the open solar magnetic field and
  solar wind flow, modulating galactic cosmic rays (GCR) from galactic
  sources. Changes in the Sun and the heliosphere affect this solar
  modulation of GCR. The most prominent type of variation in the Sun
  is the 22-year solar cycle, caused by the Sun's magnetic activity
  including changing polarity, which influences the path of the GCR in
  the heliosphere. Other shorter- and longer-term variations are also
  observable and affect processes in the heliosphere, the near-Earth
  space and on Earth. These variations can also be identified from
  the power spectral density (PSD) of GCR variability. Analysing the
  PSD can also reveal information about the distribution of power
  between different scales, observed as different power laws of the
  spectrum. Earlier work has identified spectral peaks using data,
  e.g., from neutron monitors. Less effort has been given to analyse
  data from in-situ spacecraft. Spectral peaks observed at Earth
  include, e.g., the 11-year solar cycle variation, the 1.75-year
  midterm quasiperiodicity, the 155-day Rieger periodicity, the 27-day
  solar rotational periodicity and the diurnal periodicity. Using high
  quality long-term GCR data from instruments aboard various spacecraft
  (such as CRIS on ACE, CRS on Voyager 1&amp;2, and COSPIN on Ulysses)
  and on Earth (neutron monitors), we extend the earlier Earth-based
  studies to in-situ heliospheric data and compare and analyse the
  spectral properties of GCR variability over long time scales. In
  addition to changes in time, we also look at GCR variability across
  different parts of the heliosphere. We identify spectral peaks and
  calculate the spectral index for undisturbed frequency ranges. With
  this comprehensive analysis, we can provide a reliable depiction of
  the heliospheric GCR variation in time, which helps us understand the
  process of solar modulation and the underlying space climate evolution.

---------------------------------------------------------
Title: Validation of the Neutron Monitor Yield Function Using Data
    From AMS-02 Experiment, 2011-2017
Authors: Koldobskiy, Sergey A.; Bindi, Veronica; Corti, Claudio;
   Kovaltsov, Gennady A.; Usoskin, Ilya G.
2019JGRA..124.2367K    Altcode: 2019arXiv190401929K
  The newly published spectra of protons and helium over time directly
  measured in space by the Alpha Magnetic Spectrometer (AMS-02)
  experiment for the period 2011-2017 provide a unique opportunity to
  calibrate ground-based neutron monitors (NMs). Here, calibration
  of several stable sea level NMs (Inuvik, Apatity, Oulu, Newark,
  Moscow, Hermanus, and Athens) was performed using these spectra. Four
  modern NM yield functions were verified: Mi13 (Mishev et al., 2013, <A
  href="https://doi.org/10.1002/jgra.50325">https://doi.org/10.1002/jgra.50325</A>),
  Ma16 (Mangeard et al., 2016, <A
  href="https://doi.org/10.1002/2016JA023515">https://doi.org/10.1002/2016JA023515</A>),
  CM12 (Caballero-Lopez &amp; Moraal, 2012, <A
  href="https://doi.org/10.1029/2012JA017794">https://doi.org/10.1029/2012JA017794</A>),
  and CD00 (Clem &amp; Dorman, 2000, <A
  href="https://doi.org/10.1023/A:1026508915269">https://doi.org/10.1023/A:1026508915269</A>),
  on the basis of the cosmic ray spectra measured by AMS-02. The Mi13
  yield function was found to realistically represent the NM response
  to galactic cosmic rays. CM12 yield function leads to a small skew
  in the solar cycle dependence of the scaling factor. In contrast,
  Ma16 and CD00 yield functions tend to overestimate the NM sensitivity
  to low-rigidity (&lt;10 GV) cosmic rays. This effect may be important
  for an analysis of ground level enhancements, leading to a potential
  underestimate of fluxes of solar energetic particles as based on NM
  data. The Mi13 yield function is recommended for quantitative analyses
  of NM data, especially for ground level enhancements. The validity of
  the force field approximation was studied, and it was found that it
  fits well the directly measured proton spectra, within a few percent
  for periods of low to moderate activity and up to ≈10% for active
  periods. The results of this work strengthen and validate the method
  of the cosmic ray variability analysis based on the NM data and yield
  function formalism and improve its accuracy.

---------------------------------------------------------
Title: Long-Term and Solar Cycle Variation of Galactic Cosmic Rays:
    Evidence for Variable Heliospheric Turbulence
Authors: Väisänen, Pauli; Usoskin, Ilya; Mursula, Kalevi
2019JGRA..124..804V    Altcode:
  The Sun modulates the flux of galactic cosmic rays (GCR) reaching the
  Earth's orbit. GCR flux has been measured by ground-based neutron
  monitors (NMs) for several decades, which provides an interesting
  long-term monitor of solar activity and the heliospheric magnetic
  field. Here we study the long-term evolution of the power spectrum
  of GCR over the last six solar cycles, using the power law slope in
  the frequency range 5.56·10<SUP>-6</SUP> to 2.14·10<SUP>-6</SUP> Hz
  (between 50 and 130 hr). We use data from 31 neutron monitors during
  1953-2016. We show that the power law slopes vary within the solar
  cycle, with a Kolmogorov-type slope observed at solar minimum and a
  random-walk-type slope observed at solar maximum. This implies that
  the different conditions in the different phases of the solar cycle
  affect the scaling properties of heliospheric turbulence and, thereby,
  cosmic ray variability.

---------------------------------------------------------
Title: Solar total and spectral irradiance reconstruction over the
    last 9000 years
Authors: Wu, C. -J.; Krivova, N. A.; Solanki, S. K.; Usoskin, I. G.
2018A&A...620A.120W    Altcode: 2018arXiv181103464W
  Context. Changes in solar irradiance and in its spectral distribution
  are among the main natural drivers of the climate on Earth. However,
  irradiance measurements are only available for less than four decades,
  while assessment of solar influence on Earth requires much longer
  records. <BR /> Aims: The aim of this work is to provide the most
  up-to-date physics-based reconstruction of the solar total and spectral
  irradiance (TSI/SSI) over the last nine millennia. <BR /> Methods:
  The concentrations of the cosmogenic isotopes <SUP>14</SUP>C and
  <SUP>10</SUP>Be in natural archives have been converted to decadally
  averaged sunspot numbers through a chain of physics-based models. TSI
  and SSI are reconstructed with an updated SATIRE model. Reconstructions
  are carried out for each isotope record separately, as well as
  for their composite. <BR /> Results: We present the first ever
  SSI reconstruction over the last 9000 years from the individual
  <SUP>14</SUP>C and <SUP>10</SUP>Be records as well as from their
  newest composite. The reconstruction employs physics-based models to
  describe the involved processes at each step of the procedure. <BR
  /> Conclusions: Irradiance reconstructions based on two different
  cosmogenic isotope records, those of <SUP>14</SUP>C and <SUP>10</SUP>Be,
  agree well with each other in their long-term trends despite their
  different geochemical paths in the atmosphere of Earth. Over the last
  9000 years, the reconstructed secular variability in TSI is of the
  order of 0.11%, or 1.5 W m<SUP>-2</SUP>. After the Maunder minimum,
  the reconstruction from the cosmogenic isotopes is consistent with
  that from the direct sunspot number observation. Furthermore, over
  the nineteenth century, the agreement of irradiance reconstructions
  using isotope records with the reconstruction from the sunspot number
  by Chatzistergos et al. (2017, A&amp;A, 602, A69) is better than that
  with the reconstruction from the WDC-SILSO series (Clette et al. 2014,
  Space Sci. Rev., 186, 35), with a lower χ<SUP>2</SUP>-value.

---------------------------------------------------------
Title: An Anisotropic Cosmic-Ray Enhancement Event on 07-June-2015:
    A Possible Origin
Authors: Gil, Agnieszka; Kovaltsov, Gennady A.; Mikhailov, Vladimir
   V.; Mishev, Alexander; Poluianov, Stepan; Usoskin, Ilya G.
2018SoPh..293..154G    Altcode:
  A usual event, called anisotropic cosmic-ray enhancement (ACRE), was
  observed as a small increase (≤5 % ) in the count rates of polar
  neutron monitors during 12 - 19 UT on 07 June 2015. The enhancement
  was highly anisotropic, as detected only by neutron monitors with
  asymptotic directions in the southwest quadrant in geocentric solar
  ecliptic (GSE) coordinates. The estimated rigidity of the corresponding
  particles is ≤1 GV. No associated detectable increase was found in
  the space-borne data from the Geostationary Operational Environmental
  Satellite (GOES), the Energetic and Relativistic Nuclei and Electron
  (ERNE) on board the Solar and Heliospheric Observatory (SOHO), or the
  Payload for Antimatter Matter Exploration and Light-nuclei Astrophysics
  (PAMELA) instruments, whose sensitivity was not sufficient to detect
  the event. No solar energetic particles were present during that time
  interval. The heliospheric conditions were slightly disturbed, so
  that the interplanetary magnetic field strength gradually increased
  during the event, followed by an increase of the solar wind speed
  after the event. It is proposed that the event was related to a
  crossing of the boundary layer between two regions with different
  heliospheric parameters, with a strong gradient of low-rigidity
  (&lt;1 GV) particles. It was apparently similar to another cosmic-ray
  enhancement (e.g., on 22 June 2015) that is thought to have been caused
  by the local anisotropy of Forbush decreases, with the difference that
  in our case, the interplanetary disturbance was not observed at Earth,
  but passed by southward for this event.

---------------------------------------------------------
Title: Solar energetic particles and galactic cosmic rays over
    millions of years as inferred from data on cosmogenic <SUP>26</SUP>Al
    in lunar samples
Authors: Poluianov, S.; Kovaltsov, G. A.; Usoskin, I. G.
2018A&A...618A..96P    Altcode: 2018arXiv180710153P
  <BR /> Aims: Lunar soil and rocks are not protected by a magnetic
  field or an atmosphere and are continuously irradiated by energetic
  particles that can produce cosmogenic radioisotopes directly inside
  rocks at different depths depending on the particle's energy. This
  allows the mean fluxes of solar and galactic cosmic rays to be assessed
  on the very long timescales of millions of years. <BR /> Methods: Here
  we show that lunar rocks can serve as a very good particle integral
  spectrometer in the energy range 20-80 MeV. We have developed a new
  method based on precise modeling, that is applied to measurements
  of <SUP>26</SUP>Al (half-life ≈0.7 megayears) in lunar samples
  from the Apollo mission, and present the first direct reconstruction
  (i.e., without any a priori assumptions) of the mean energy spectrum of
  solar and galactic energetic particles over a million of years. <BR />
  Results: We show that the reconstructed spectrum of solar energetic
  particles is totally consistent with that over the last decades,
  despite the very different levels of solar modulation of galactic
  cosmic rays (ϕ = 496 ± 40 MV over a million years versus (ϕ =
  660 ± 20 MV for the modern epoch). We also estimated the occurrence
  probability of extreme solar events and argue that no events with the
  F(&gt;30 MeV) fluence exceeding 5×10<SUP>10</SUP> and 10<SUP>11</SUP>
  cm<SUP>-2</SUP> are expected on timescales of a thousand and million
  years, respectively. <BR /> Conclusions: We conclude that the mean
  flux of solar energetic particles hardly depends on the level of solar
  activity, in contrast to the solar modulation of galactic cosmic
  rays. This puts new observational constraints on solar physics and
  becomes important for assessing radiation hazards for the planned
  space missions.

---------------------------------------------------------
Title: Neutron monitor count rate increase as a proxy for dose rate
    assessment at aviation altitudes during GLEs
Authors: Mishev, Alexander; Tuohino, Sasu; Usoskin, Ilya
2018JSWSC...8A..46M    Altcode:
  Radiation exposure due to cosmic rays, specifically at cruising aviation
  altitudes, is an important topic in the field of space weather. While
  the effect of galactic cosmic rays can be easily assessed on the basis
  of recent models, estimate of the dose rate during strong solar particle
  events is rather complicated and time consuming. Here we compute the
  maximum effective dose rates at a typical commercial flight altitude
  of 35 kft (≈11 000 m above sea level) during ground level enhancement
  events, where the necessary information, namely derived energy/rigidity
  spectra of solar energetic particles, is available. The computations are
  carried out using different reconstructions of the solar proton spectra,
  available in bibliographic sources, leading to multiple results for
  some events. The computations were performed employing a recent model
  for effective dose and/or ambient dose equivalent due to cosmic ray
  particles. A conservative approach for the computation was assumed. A
  highly significant correlation between the maximum effective dose
  rate and peak NM count rate increase during ground level enhancement
  events is derived. Hence, we propose to use the peak NM count rate
  increase as a proxy in order to assess the peak effective dose rate
  at flight altitude during strong solar particle events using the real
  time records of the worldwide global neutron monitor network.

---------------------------------------------------------
Title: First Analysis of Ground-Level Enhancement (GLE) 72 on 10
September 2017: Spectral and Anisotropy Characteristics
Authors: Mishev, A.; Usoskin, I.; Raukunen, O.; Paassilta, M.;
   Valtonen, E.; Kocharov, L.; Vainio, R.
2018SoPh..293..136M    Altcode: 2018arXiv181010536M
  Using data obtained with neutron monitors and space-borne instruments,
  we analyzed the second ground-level enhancement (GLE) of Solar Cycle 24,
  namely the event of 10 September 2017 (GLE 72), and derived the spectral
  and angular characteristics of associated GLE particles. We employed
  a new neutron-monitor yield function and a recently proposed model
  based on an optimization procedure. The method consists of simulating
  particle propagation in a model magnetosphere in order to derive the
  cutoff rigidity and neutron-monitor asymptotic directions. Subsequently,
  the rigidity spectrum and anisotropy of GLE particles are obtained
  in their dynamical evolution during the event on the basis of an
  inverse-problem solution. The derived angular distribution and spectra
  are discussed briefly.

---------------------------------------------------------
Title: Comment on the paper by Popova et al. "On a role of quadruple
    component of magnetic field in defining solar activity in grand
    cycles"
Authors: Usoskin, Ilya G.
2018JASTP.176...69U    Altcode: 2017arXiv171005203U
  The paper by Popova et al. presents an oversimplified mathematical
  model of solar activity with a claim of predicting/postdicting it
  for several millennia ahead/backwards. The work contains several
  flaws devaluating the results: (1) the method is unreliable from the
  point of view of signal processing (it is impossible to make harmonic
  predictions for thousands of years based on only 35 years of data)
  and lacks quality control; (2) the result of post-diction apparently
  contradicts the observational data. (3) theoretical speculations
  make little sense. To summarize, a multi-harmonic mathematical model,
  hardly related to full solar dynamo theory, is presented, which is not
  applicable to realistic solar conditions because of the significant
  chaotic/stochastic intrinsic component and strong non-stationarity of
  solar activity. The obtained result is apparently inconsistent with the
  data in the past and thus cannot be trusted for the future predictions.

---------------------------------------------------------
Title: Solar superstorm of AD 774 recorded subannually by Arctic
    tree rings
Authors: Uusitalo, J.; Arppe, L.; Hackman, T.; Helama, S.; Kovaltsov,
   G.; Mielikäinen, K.; Mäkinen, H.; Nöjd, P.; Palonen, V.; Usoskin,
   I.; Oinonen, M.
2018NatCo...9.3495U    Altcode:
  Recently, a rapid increase in radiocarbon (<SUP>14</SUP>C) was observed
  in Japanese tree rings at AD 774/775. Various explanations for the
  anomaly have been offered, such as a supernova, a γ-ray burst,
  a cometary impact, or an exceptionally large Solar Particle Event
  (SPE). However, evidence of the origin and exact timing of the event
  remains incomplete. In particular, a key issue of latitudinal dependence
  of the <SUP>14</SUP>C intensity has not been addressed yet. Here, we
  show that the event was most likely caused by the Sun and occurred
  during the spring of AD 774. Particularly, the event intensities
  from various locations show a strong correlation with the latitude,
  demonstrating a particle-induced <SUP>14</SUP>C poleward increase,
  in accord with the solar origin of the event. Furthermore, both annual
  <SUP>14</SUP>C data and carbon cycle modelling, and separate earlywood
  and latewood <SUP>14</SUP>C measurements, confine the photosynthetic
  carbon fixation to around the midsummer.

---------------------------------------------------------
Title: Structure of the Power Spectral Density of Galactic Cosmic
    Ray Variation during 1953-2016
Authors: Väisänen, Pauli; Usoskin, Ilya; Mursula, Kalevi
2018IAUS..335...82V    Altcode:
  Fluxes of galactic cosmic rays (GCR) observed at 1 AU are modulated
  inside the heliosphere at different time scales. Here we study the
  properties of the power spectral density (PSD) of galactic cosmic
  ray variability using hourly data from 31 neutron monitors (NM)
  from 1953 to 2016. We pay particular attention to the reliability of
  the used datasets and methods. We present the overall PSD and discuss
  different parts of the spectrum and the related periodicities. We find
  significant spectral peaks at the periods of 11 years, 1.75 years,
  155 days, 27 days and 24 hours and the harmonics of the latter two
  peaks. We calculate a power law slope of -1.79 +/- 0.13 for the period
  range between 50 and 130 hours and a slope of -1.34 +/- 0.17 for the
  period range between 40 days and 3.4 years (1000 - 30000 h).

---------------------------------------------------------
Title: Spatial Organization of Seven Extreme Solar Energetic
    Particle Events
Authors: Kocharov, Leon; Pohjolainen, Silja; Reiner, Mike J.; Mishev,
   Alexander; Wang, Haimin; Usoskin, Ilya; Vainio, Rami
2018ApJ...862L..20K    Altcode:
  Emission of relativistic protons and helium responsible for extreme
  solar particle events (ground level enhancements (GLEs)) is often
  structured. We investigate its organization depending on the eruption
  stage characterized by the heliocentric height of associated coronal
  mass ejections (CMEs). Seven GLEs are considered: events on 1997
  November 6, 1998 May 2, 2000 July 14, 2001 December 26, 2003 November
  2, 2006 December 13, and 2012 May 17, which are half of the SOlar
  and Heliospheric Observatory (SOHO )-era GLEs, excluding very weak
  events. Count-rate profiles of the GLEs plotted as a function of the CME
  height reveal two types (or two components) of the high-energy particle
  emission. The first component rises in a step-like manner during
  the CME transit from 2 R <SUB>⊙</SUB> to 3 R <SUB>⊙</SUB>, when
  the CME exits from predominantly closed coronal magnetic structures,
  irrespective of the CME speed (type H). This component is of coronal
  origin. The second component of the GLE-producing particles starts to
  rise when CME is at about 4 R <SUB>⊙</SUB>, achieves its maximum at
  6-10 R <SUB>⊙</SUB>, and declines shortly after that (type J). The
  type J particle injection into the interplanetary space coincides with
  the decametric-hectometric radio burst complex that includes enhanced
  emission of type II and concurrent low-frequency type III bursts,
  indicative of the CME interaction with a streamer-like structure at
  a few solar radii from the Sun. Those could be delayed particles
  from the flare region. A possible additional contribution of the
  CME-bow-shock acceleration in unstructured solar wind is not large in
  the two considered types of events.

---------------------------------------------------------
Title: Effective Rigidity of a Polar Neutron Monitor for Recording
    Ground-Level Enhancements
Authors: Koldobskiy, Sergey A.; Kovaltsov, Gennady A.; Usoskin, Ilya G.
2018SoPh..293..110K    Altcode:
  The "effective" rigidity of a neutron monitor for a ground-level
  enhancement (GLE) event is defined so that the event-integrated
  fluence of solar energetic protons with rigidity above it is directly
  proportional to the integral intensity of the GLE as recorded by a
  polar neutron monitor, within a wide range of solar energetic-proton
  spectra. This provides a direct way to assess the integral fluence
  of a GLE event based solely on neutron-monitor data. The effective
  rigidity/energy was found to be 1.13 - 1.42 GV (550 - 800 MeV). A
  small model-dependent, systematic uncertainty in the value of the
  effective rigidity is caused by uncertainties in the low-energy range
  of the neutron-monitor yield function, which requires more detailed
  computations of the latter.

---------------------------------------------------------
Title: Upgrade of GLE database: Assessment of effective dose rate
    at flight altitude
Authors: Tuohino, S.; Ibragimov, A.; Usoskin, I.; Mishev, A.
2018AdSpR..62..398T    Altcode:
  A new database for assessment of radiation doses at cruise
  flight altitude in the Earth atmosphere, related to ground level
  enhancement (GLE) events is created under VarSiTi/SCOSTEP support
  and incorporated to the International ground level enhancement (GLE)
  database (gle.oulu.fi). The upgraded database provides, for each GLE
  event, where possible, information on the estimated energy/rigidity
  spectra of solar energetic particles and the corresponding computed
  effective doses at cruise flight altitude of 35 kft (10,668 m above
  sea level). The computations are performed for various reconstructions
  of solar energetic particles spectra, available in literature, thus
  for some events there are several results. Computations were performed
  using a recent model for assessment of effective dose due to cosmic ray
  particles, applied specifically in the polar region, where the exposure
  is maximal. This upgrade allows one to estimate the radiation effects at
  cruise flight altitude caused by major GLE events over several decades.

---------------------------------------------------------
Title: Solar Activity and Irradiance Reconstruction over the Holocene
Authors: Wu, Chi-Ju; Usoskin, Ilya; Krivova, Natalie; Solanki, Sami
   K.; Kovaltsov, Gennady A.; Baroni, Melanie; Bard, Edouard
2018cosp...42E3695W    Altcode:
  Direct measurements of the solar irradiance are only available since
  1978. To understand the solar influence on Earth's climate, longer
  records and thus reconstructions of the solar variability in the past
  are needed. The directly observed sunspot number allows going back
  to 1610 A.D, although with progressively increasing uncertainty. To
  assess solar variability at earlier times, one has to rely on indirect
  proxies of solar activity, such as concentrations of cosmogenic isotopes
  10Be and 14C in terrestrial archives. They are produced mostly in
  the upper atmosphere by impinging galactic cosmic rays (GCRs). The
  flux of GCRs is modulated by both the heliospheric magnetic field and
  the geomagnetic field. Therefore, the isotope signals retrieved from
  various sites around the globe show a very high degree of similarity,
  reflecting changes in the solar activity. Still, short-and mid-term
  deviations can be observed due to various systematic effects, such as
  different geochemical production, atmospheric distribution processes
  and local climatic conditions. To account for these differences, we
  have constructed a state-of-the-art consistent multi-isotope composite
  from one global 14C and six regional 10Be data sets. This composite is
  then used to reconstruct decadal values of the total and spectral solar
  irradiance over the Holocene with the semi-empirical SATIRE-M model,
  while the quasi-11 year solar cycle has been simulated statistically.

---------------------------------------------------------
Title: The effective energy for neutron monitors and cosmogenic
    isotopes-redefined concept
Authors: Gil, Agnieszka; Usoskin, Ilya; Kovaltsov, Gennady A.;
   Asvestari, Eleanna
2018cosp...42E1207G    Altcode:
  Cosmic ray variability is often described in terms of the modulation
  potential (φ) changes. Based on measurements of ground-based
  energy-integrating detectors, such as neutron monitors for the recent
  decades, and by cosmogenic isotopes stored in natural archives for
  the millennial timescale, variability of φ can be reconstructed. Here
  we defined the effective energy of an energy-integrating detector as
  energy at which the cosmic ray flux changeability is straightforward
  proportional to that of the detector's response. We calculated that
  the effective energy for the standard sea-level polar neutron monitor
  is around 11-12 GeV/nucleon, while for cosmic ray reconstruction
  based on cosmogenic isotopes it is around 6-7 GeV/nucleon and 5.5-6
  GeV/nucleon for 14C data and 10Be, respectively. We compared results
  based on different models of local interstellar spectrum (LIS) of
  galactic cosmic rays, showing that the effective energy is determined
  robustly against the particular LIS model.

---------------------------------------------------------
Title: Solar activity over nine millennia: A consistent multi-proxy
    reconstruction
Authors: Wu, C. J.; Usoskin, I. G.; Krivova, N.; Kovaltsov, G. A.;
   Baroni, M.; Bard, E.; Solanki, S. K.
2018A&A...615A..93W    Altcode: 2018arXiv180401302W
  <BR /> Aims: The solar activity in the past millennia can only
  be reconstructed from cosmogenic radionuclide proxy records in
  terrestrial archives. However, because of the diversity of the proxy
  archives, it is difficult to build a homogeneous reconstruction. All
  previous studies were based on individual, sometimes statistically
  averaged, proxy datasets. Here we aim to provide a new consistent
  multi-proxy reconstruction of the solar activity over the last 9000
  yr, using all available long-span datasets of <SUP>10</SUP>Be and
  <SUP>14</SUP>C in terrestrial archives. <BR /> Methods: A new method,
  based on a Bayesian approach, was applied for the first time to solar
  activity reconstruction. A Monte Carlo search (using the χ<SUP>2</SUP>
  statistic) for the most probable value of the modulation potential was
  performed to match data from different datasets for a given time. This
  provides a straightforward estimate of the related uncertainties. We
  used six <SUP>10</SUP>Be series of different lengths (from 500-10
  000 yr) from Greenland and Antarctica, and the global <SUP>14</SUP>C
  production series. The <SUP>10</SUP>Be series were resampled to match
  wiggles related to the grand minima in the <SUP>14</SUP>C reference
  dataset. The stability of the long data series was tested. <BR />
  Results: The Greenland Ice-core Project (GRIP) and the Antarctic EDML
  (EPICA Dronning Maud Land) <SUP>10</SUP>Be series diverge from each
  other during the second half of the Holocene, while the <SUP>14</SUP>C
  series lies in between them. A likely reason for the discrepancy is the
  insufficiently precise beryllium transport and deposition model for
  Greenland, which leads to an undercorrection of the GRIP series for
  the geomagnetic shielding effect. A slow 6-7 millennia variability
  with lows at ca. 5500 BC and 1500 AD in the long-term evolution
  of solar activity is found. Two components of solar activity can
  be statistically distinguished: the main component, corresponding
  to the "normal" moderate level, and a component corresponding to
  grand minima. A possible existence of a component representing
  grand maxima is indicated, but it cannot be separated from the main
  component in a statistically significant manner. <BR /> Conclusions:
  A new consistent reconstruction of solar activity over the last nine
  millennia is presented with the most probable values of decadal sunspot
  numbers and their realistic uncertainties. Independent components
  of solar activity corresponding to the main moderate activity
  and the grand-minimum state are identified; they may be related
  to different operation modes of the dynamo. <P />A table with the
  reconstructed SN series is available at the CDS via anonymous ftp to <A
  href="http://cdsarc.u-strasbg.fr">http://cdsarc.u-strasbg.fr</A>(ftp://130.79.128.5)
  or via <A
  href="http://cdsarc.u-strasbg.fr/viz-bin/qcat?J/A+A/615/A93">http://cdsarc.u-strasbg.fr/viz-bin/qcat?J/A+A/615/A93</A>

---------------------------------------------------------
Title: Extreme solar particle events: historical prospective
Authors: Usoskin, Ilya
2018cosp...42E3472U    Altcode:
  The era of space-borne or ground-based observations of solar energetic
  particle events (SPEs) covers several decades, respectively. About 70
  strong energetic events (ground-level enhancements, GLEs) have been
  recorded by ground-based instrumentations, the greatest being GLE No.5
  on 23-Feb-1956. However, the statistic is still insufficient to conclude
  whether the Sun can produce stronger events, how much stronger and what
  the expected rate of their occurrence can be. Of special importance
  is the question of the worst-case scenario. In order to answer these
  questions, one has to exploit data on much longer time scales, covering
  millennia and millions of years, which can be done only using proxy
  data of cosmogenic radionuclides. Here we present an brief overview
  of the present state of the art in the study of extreme SEP events
  and an assessment of the worst case scenario for the SEP fluence in
  the vicinity of Earth.

---------------------------------------------------------
Title: Revised historical solar irradiance forcing
Authors: Egorova, T.; Schmutz, W.; Rozanov, E.; Shapiro, A. I.;
   Usoskin, I.; Beer, J.; Tagirov, R. V.; Peter, T.
2018A&A...615A..85E    Altcode: 2018arXiv180400287E
  Context. There is no consensus on the amplitude of historical solar
  forcing. The estimated magnitude of the total solar irradiance (TSI)
  difference between the Maunder minimum and the present time ranges
  from 0.1 to 6 W m<SUP>-2</SUP> making the simulation of the past and
  future climate uncertain. One reason for this disagreement is the
  applied evolution of the quiet Sun brightness in solar irradiance
  reconstruction models. This work addresses the role of the quiet Sun
  model choice and updated solar magnetic activity proxies on the solar
  forcing reconstruction. <BR /> Aims: We aim to establish a plausible
  range for the solar irradiance variability on decadal to millennial
  timescales. <BR /> Methods: The spectral solar irradiance (SSI) is
  calculated as a weighted sum of the contributions from sunspot umbra,
  sunspot penumbra, faculae, and quiet Sun, which are pre-calculated with
  the NLTE Spectral SYnthesis code (NESSY). We introduce activity belts
  of the contributions from sunspots and faculae and a new structure
  model for the quietest state of the Sun. We assume that the brightness
  of the quiet Sun varies in time proportionally to the secular (22-yr
  smoothed) variation of the solar modulation potential. <BR /> Results:
  A new reconstruction of the TSI and SSI covering the period 6000 BCE -
  2015 CE is presented. The model simulates solar irradiance variability
  during the satellite era well. The TSI change between the Maunder and
  recent minima ranges between 3.7 and 4.5 W m<SUP>-2</SUP> depending
  on the applied solar modulation potential. The implementation of
  a new quietest Sun model reduces, by approximately a factor of two,
  the relative solar forcing compared to the largest previous estimation,
  while the application of an updated solar modulation potential increases
  the forcing difference between the Maunder minimum and the present
  by 25-40%.

---------------------------------------------------------
Title: Global NM network - a usefull tool to assess radiation hazard
    at flight altitudes
Authors: Mishev, Alexander; Usoskin, Ilya
2018cosp...42E2299M    Altcode:
  An important topic in the field of space weather is the assessment of
  radiation exposure at commercial flight altitudes. A specific interest
  is related to the contribution of solar energetic particles. For this
  purpose a precise information about solar energetic particle (SEP)
  characteristics, namely rigidity spectrum and angular distribution
  is necessary. Direct measurements with space-borne instruments can
  provide precise information of SEPs. However, they are constrained in
  some cases, because the specifics of spacecraft orbits. On the other
  hand ground based detectors, namely the global neutron monitor network
  provides a continuous operation. SEP characteristics can be derived
  using neutron monitor (NM) data during a special class of SEP events
  - the ground level enhancements (GLEs). A precise analysis of SEP
  spectral and angular characteristics using NM data requires several
  steps: detailed computation of assymptotic cones and cut-off rigidity
  of NMs used for the analysis, modeling of global NM network response
  using NM yield function and optimization procedure in order to derive
  spectral and angular characteristics of SEPs. Similar procedure with
  modifications, namely simplification of the model is applied for
  sub-GLEs analysis. Subsequently on the basis of the derived spectra
  and angular characteristics and using recent model based on previously
  computed yield functions we calculate the effective dose during the GLEs
  and sub-GLEs at typical commercial flight altitude of 35 kft. Several
  examples are shown. Hence, we demonstrated that the global NM network
  is a useful tool to assess the radiation exposure of aircrew due to CR
  of galactic and solar origin. In addition, we created a new database
  for assessment of radiation doses in the Earth atmosphere, related
  to GLE events created under VarSiTi/SCOSTEP support and incorporated
  to the International GLE database. The upgraded database provides,
  for each GLE event, where possible, information on the estimated SEP
  energy/rigidity spectra, the corresponding computed effective doses
  and bibliography. The effective dose rates were computed for altitude
  of 35 kft in a polar region, where the exposure is maximal.

---------------------------------------------------------
Title: An updated definition of GLE and sub-GLE events
Authors: Usoskin, Ilya; Shea, Margaret; Smart, Don; Poluianov, Stepan;
   Mishev, Alexander
2018cosp...42E3473U    Altcode:
  The concept of the ground-level enhancement (GLE, http://gle.oulu.fi)
  of the neutron monitor (NM) count rate, caused by solar energetic
  particles (SEP), plays an important role for many statistical and
  scientific studies. The classical definition says that a GLE has been
  identified when a near simultaneous increase (typically associated with
  solar activity) is registered by at least two differently located NMs
  regardless of their atmospheric and geomagnetic cutoff properties. This
  included NMs at a high-altitude polar site with the reduced total
  cutoff (SOPO/B at the Amundsen-Scott station, South Pole, Antarctica,
  elevation 2835 m asl), and Vostok NM (Vostok station, 3500 m, operating
  only 1963-1969). However, a new high-altitude polar NM (DOMC/B)
  was installed at Concordia station (Dome C, Antarctica, elevation
  3233 m asl) in 2015. As a result, there is a pair of exceptionally
  sensitive instruments (SOPO/B and DOMC/B) that can formally register
  a near simultaneous increase from a relatively weak SEP event below
  the full atmospheric cutoff, which would have not been detected at
  any other NM station and, accordingly, not accepted as a GLE before
  2015. This would potentially distort the homogeneity of the present
  GLE list by more frequent detections due to the enhanced sensitivity
  of the global NM network.In order to maintain the homogeneity of the
  events previously listed as ground-level enhancements, we propose to
  modify the presently used GLE definition as follows: “A GLE event
  is registered when there are near-time coincident and statistically
  significant enhancements of the count rates of at least two differently
  located neutron monitors, including at least one neutron monitor near
  sea level and a corresponding enhancement in the proton flux measured
  by a space-borne instrument(s).” We also propose to classify SEP
  events under the full atmospheric cutoff, which are seen only in data
  of high-altitude polar NMs, as sub-GLEs. We note that this definition
  does not affect the present list of GLEs.

---------------------------------------------------------
Title: GLE 72 on 10 September 2017 - an analysis using neutron
    monitor and space-borne data
Authors: Mishev, Alexander; Usoskin, Ilya; Valtonen, Eino; Kocharov,
   Leon; Vainio, Rami; Raukunen, Osku; Paassilta, Miikka
2018cosp...42E2298M    Altcode:
  The first ten days of September 2017 were characterized by intense
  solar activity, producing several X-class flares and coronal mass
  ejections (CMEs). The second ground level enhancement (GLE) event of
  solar cycle 24, namely GLE 72 on 10 September 2017, was related to a
  X8.2 solar flare. The flare peaked at 16:06 UT, leading to a gradual
  solar energetic particle event measured by spacecraft up to proton
  energies exceeding 700 MeV and to a very fast CME erupting over the
  west limb. The GLE onset was observed by several neutron monitor
  (NM) stations at about 16:15 UT (FSMT and INVK). However, a clearly
  distinguishable signal, which allows one to derive the spectral
  and angular characteristics of SEPs with sufficient precision, was
  observed at 16:30 UT. The strongest increases were observed at the
  DOMC/DOMB 10-15 %, SOPO/SOPB 5-8 % and FSMT 6%, above the pre-increase
  levels. The event was characterized by a typical gradual increase. Here
  we perform a precise analysis of spectral and angular features
  of solar energetic particles (SEPs) on the basis of NM data. The
  method includes several consequitive steps: detailed computation of
  assymptotic cones and cut-off rigidity of each NM station used in
  the analysis, an initial guess of the inverse problem by assuming
  the apparent source position in a convenient way, application of the
  NM yield function for detector response modelling and optimization
  procedure in order to derive spectral and angular characteristics
  of SEPs. In this study we use the Planetocosmics code and realistic
  magnetospheric models for computations of assymptotic directions and
  rigidity cut-offs. Here we present results from analysis of GLE 72,
  namely SEP spectra and pitch angle distributions, which are obtained
  in their dynamical development throughout the event. An interpretation
  of the derived findings is performed.

---------------------------------------------------------
Title: Variation of the PSD slopes of cosmic rays in 1953-2016
Authors: Väisänen, Pauli; Usoskin, Ilya; Mursula, Kalevi
2018cosp...42E3483V    Altcode:
  The flux of cosmic rays observed at the Earth is modulated by the
  Sun and the heliosphere. Modulation of the galactic cosmic rays
  (GCR) is mostly caused by scattering on the inhomogeneities of the
  heliospheric magnetic field (HMF). Sporadic solar events like coronal
  mass ejections and merged interaction regions affect the HMF and scatter
  GCR. Turbulent variations are another source of inhomogeneities of the,
  causing scattering at different scales. The variability of the cosmic
  ray flux as measured ground-based neutron monitors (NMs) can serve as a
  probe for heliospheric turbulence and its scaling. Turbulent phenomena
  are often characterized by a power-law type power spectral density (PSD)
  of the measured variable. Using 1-hour resolution data from the global
  NM network in 1953-2016, we have studied the power-law slope in the
  frequency range between 5.56*10^{-6} and 2.14*10^{-6} Hz, corresponding
  to time scales of 50 and 130 hours. The mean power-law slope was found
  to be -1.81±0.02. We have studied the temporal variation of this
  power-law slope and found that the slope values differ for different
  solar cycles and different cycle phases, with steeper slopes observed
  usually during the ascending and maximum phases, and less steep slopes
  during the declining and minimum phases. This implies that the scaling
  of HMF turbulence varies in the course of the solar cycle, reflecting
  different physical processes affecting GCR modulation.

---------------------------------------------------------
Title: A Solar Cycle of Cosmic Ray Fluxes for 2006-2014: Comparison
    between PAMELA and Neutron Monitors
Authors: Koldobskiy, Sergey A.; Kovaltsov, Gennady A.; Usoskin, Ilya G.
2018JGRA..123.4479K    Altcode:
  A comparison of cosmic proton spectra directly measured by the Payload
  for Antimatter Matter Exploration and Light-nuclei Astrophysics (PAMELA)
  experiment during 2006-2014 with data of polar neutron monitors for the
  same time interval is presented. It is shown that the measured spectra
  are well described by the force-field model for the modulation potential
  range 350-750 MV. The obtained modulation potential agrees with that
  calculated from the data of the world neutron monitor network for low
  solar activity between 2006 and 2012 but diverges during the maximum
  of solar cycle. The empirical relation between the modulation potential
  and the (inverted) neutron monitor count rate appears somewhat steeper
  than the modeled one, as confirmed also by data from fragmentary
  balloon-borne measurements. A reason for the discrepancy is unclear
  and calls for additional study using independent data sets.

---------------------------------------------------------
Title: Long-term evolution of the power-law spectrum of galactic
    cosmic rays in 1953-2016
Authors: Väisänen, Pauli; Usoskin, Ilya; Mursula, Kalevi
2018EGUGA..20.6021V    Altcode:
  The power spectrum of galactic cosmic ray (GCR) variability is
  modulated by the heliospheric magnetic field and solar wind. The GCR
  power spectrum consists of a number of important peaks (related e.g.,
  to solar cycle, solar rotation and diurnal variation) and the background
  power-law spectrum. The slope of the background power-law spectrum is
  often used as a quantitative indicator of energy scaling of the signal,
  indicating chaotic or stochastic behaviour like turbulence or Brownian
  motion. We present a study of the statistical properties and long-term
  evolution of the power-law slope of the spectral density of cosmic
  rays calculated from 31 neutron monitors covering the time period from
  1953 to 2016. We limit here the analysis of the slope to within the
  time scales of 50 to 130 hours (frequency range 5.56*10-6 to 2.14*10-6
  Hz), where the power spectrum has the most perfect power-law behaviour
  outside the main spectral peaks. The mean power-law slope was found to
  be -1.81. We studied the slopes in different phases of the solar cycle,
  and found that they vary systematically within the solar cycle. Higher
  (less steep) slopes of around -1.67 (corresponding to the Kolmogorov
  spectrum) were observed during solar minima and steeper slopes of
  around -2 (corresponding to random processes) during solar maxima.

---------------------------------------------------------
Title: Extreme Solar Particle Storms: How hostile can the Sun be?
Authors: Usoskin, Ilya
2018EGUGA..20.4306U    Altcode:
  It is recognized now that strong sporadic events (called solar particle
  storms) with high fluxes of solar energetic particles (SEP) produced
  during eruptive solar flares and coronal mass ejections form a serious
  issue for Space Weather and pose deadly hazards for technological
  devices and even human lives outside the protective Earth's atmosphere
  and magnetosphere. The strongest directly observed solar particle storm
  took place on 23-Feb-1956 with a 50-x enhancement over the galactic
  background as recorded on the ground. Can stronger storms appear? How
  often? Can we assess the "worst case scenario"? Knowing answers to
  these questions is of great importance, not only purely academic but
  also societal and technological. The era of direct measurements of SEP
  events by space-borne detectors covers 40-50 years, and by ground-based
  instruments about 70 years. Because of the limited dataset we possess,
  these questions can be answered only using indirect methods. An overview
  of different method is presented here with a search for extreme SEP
  events. First we discuss the method of cosmogenic radionuclides (14C,
  10Be, 36Cl) measured in independently dateable natural archives,
  that forms a reliable proxy of cosmic ray variability on the
  centennial-millennial time scale. So far, three extreme SEP events
  have been identified during the Holocene: the strongest known event of
  775 AD, which was a factor 40-50 stronger than that of 23-Feb-1956,
  and a couple of slightly weaker event of 994 AD an 3372 BC. Next we
  discuss the method of cosmogenic isotopes (primarily 26Al) measured
  in lunar rocks, which does not allow to identify individual events but
  provides evaluation of the mean flux of SEP over a million of years. We
  also critically discuss a statistical study of the large ensemble of
  sun-like stars, some of which exhibit super-flares. Considering all
  data in their diversity and recent achievements in this field, we
  argue that the event of 775 AD may serve as the worst case scenario
  of an extreme solar particle storm, and that we do not expect much
  stronger events on the megayear timescale.

---------------------------------------------------------
Title: Effective Energy of Neutron Monitors and Cosmogenic Isotopes
Authors: Gil, Agnieszka; Asvestari, Eleanna; Kovaltsov, Gennady;
   Usoskin, Ilya
2018EGUGA..2010485G    Altcode:
  Galactic cosmic ray variations are often quantified with the aid of the
  modulation potential (φ). For more than sixty years φ is typically
  computed using measurements of ground-based energy-integrating
  detectors, such as neutron monitors, and for the millennial scale
  by cosmogenic isotopes stored in natural archives. Here we redefine
  the effective energy of a detector, considering it as the energy
  at which the cosmic ray flux variability is straightforwardly
  proportional to that of the detector's count rate. We found that for
  the standard sea-level polar neutron monitor the effective energy
  is 11-12 GeV/nucleon, for cosmic ray reconstruction based on 14C
  data 6-7 GeV/nucleon and for 10Be data 5.5-6 GeV/nucleon. We present
  results based on various models of local interstellar spectrum (LIS)
  of galactic cosmic rays, showing that the effective energy is defined
  robustly against exact LIS model.

---------------------------------------------------------
Title: Effective energy of solar energetic particles causing a
    ground-level enhancement
Authors: Koldobsky, Sergey; Kovaltsov, Gennady; Usoskin, Ilya
2018EGUGA..20.4376K    Altcode:
  Ground level enhancements (GLEs) are short sporadic events when the
  count rate of a ground-based neutron monitor (NM) is significantly
  enhanced over the background of galactic cosmic rays due to high
  fluxes of solar energetic particles (SEPs). It is difficult to measure
  the spectrum of SEPs directly, since the measurements should be
  performed outside the shielding effect of the Earth magnetosphere and
  atmosphere. On the other hand, a quick estimate of the total fluence of
  SEP above some effective energy Eeff can be made based on the observed
  GLE response. Here we define such effective energy that the SEP fluence
  above it is directly proportional to the GLE strength as recorded by
  polar NMs. We show, using data from the International GLE database
  (http://gle.oulu.fi) and applying a recent yield function of NM that
  the response of a polar NM to a GLE is directly proportional to the
  SEP fluence above 600-800 MeV. Thus, the effective energy of SEP as
  detected by ground-based NMs is Eeff=600-880 MeV.

---------------------------------------------------------
Title: A Test of the Active-Day Fraction Method of Sunspot Group
Number Calibration: Dependence on the Level of Solar Activity
Authors: Willamo, T.; Usoskin, I. G.; Kovaltsov, G. A.
2018SoPh..293...69W    Altcode: 2018arXiv180310501W
  The method of active-day fraction (ADF) was proposed recently
  to calibrate different solar observers to standard observational
  conditions. The result of the calibration may depend on the overall
  level of solar activity during the observational period. This dependency
  is studied quantitatively using data of the Royal Greenwich Observatory
  by formally calibrating synthetic pseudo-observers to the full reference
  dataset. It is shown that the sunspot group number is precisely
  estimated by the ADF method for periods of moderate activity, may
  be slightly underestimated by 0.5 - 1.5 groups (≤10 % ) for strong
  and very strong activity, and is strongly overestimated by up to 2.5
  groups (≤30 % ) for weak-to-moderate activity. The ADF method becomes
  inapplicable for the periods of grand minima of activity. In general,
  the ADF method tends to overestimate the overall level of activity
  and to reduce the long-term trends.

---------------------------------------------------------
Title: VizieR Online Data Catalog: Reconstructed decadal sunspot
    numbers (Wu+, 2018)
Authors: Wu, C. J.; Usoskin, I. G.; Krivova, N.; Kovaltsov, G. A.;
   Baroni, M.; Bard, E.; Solanki, S. K.
2018yCat..36150093W    Altcode:
  The file contains the decadal numbers of sunspot groups including
  the decade central year [Y], the low [S<SUB>l], the mean [S</SUB>M]
  and the upper [S_u] 1-sigma (68% bounds). <P />(1 data file).

---------------------------------------------------------
Title: Extreme Value Theory Applied to the Millennial Sunspot
    Number Series
Authors: Acero, F. J.; Gallego, M. C.; García, J. A.; Usoskin, I. G.;
   Vaquero, J. M.
2018ApJ...853...80A    Altcode: 2018arXiv180109776A
  In this work, we use two decadal sunspot number series reconstructed
  from cosmogenic radionuclide data (<SUP>14</SUP>C in tree trunks, SN
  14C, and <SUP>10</SUP>Be in polar ice, SN 10Be) and the extreme value
  theory to study variability of solar activity during the last nine
  millennia. The peaks-over-threshold technique was used to compute, in
  particular, the shape parameter of the generalized Pareto distribution
  for different thresholds. Its negative value implies an upper bound
  of the extreme SN 10Be and SN 14C timeseries. The return level for
  1000 and 10,000 years were estimated leading to values lower than
  the maximum observed values, expected for the 1000 year, but not for
  the 10,000 year return levels, for both series. A comparison of these
  results with those obtained using the observed sunspot numbers from
  telescopic observations during the last four centuries suggests that
  the main characteristics of solar activity have already been recorded
  in the telescopic period (from 1610 to nowadays) which covers the full
  range of solar variability from a Grand minimum to a Grand maximum.

---------------------------------------------------------
Title: Can Superflares Occur on the Sun? A View from Dynamo Theory
Authors: Katsova, M. M.; Kitchatinov, L. L.; Livshits, M. A.; Moss,
   D. L.; Sokoloff, D. D.; Usoskin, I. G.
2018ARep...62...72K    Altcode: 2017arXiv171000015K
  Recent data from the Kepler mission has revealed the occurrence
  of superflares in Sun-like stars which exceed by far any observed
  solar flares in released energy. Radionuclide data do not provide
  evidence for occurrence of superflares on the Sun over the past eleven
  millennia. Stellar data for a subgroup of superflaring Kepler stars are
  analysed in an attempt to find possible progenitors of their abnormal
  magnetic activity. A natural idea is that the dynamo mechanism in
  superflaring stars differs in some respect from that in the Sun. We
  search for a difference in the dynamo-related parameters between
  superflaring stars and the Sun to suggest a dynamo mechanism as close
  as possible to the conventional solar/stellar dynamo but capable of
  providing much higher magnetic energy. Dynamo based on joint action of
  differential rotation and mirror asymmetric motions can in principle
  result in excitation of two types of magnetic fields. First of all,
  it is well-known in solar physics dynamo waves. The point is that
  another magnetic configuration with initial growth and further
  stabilisation can also be excited. For comparable conditions,
  magnetic field of second configuration is much stronger than that
  of the first one just because dynamo does not spend its energy for
  periodic magnetic field inversions but uses it for magnetic field
  growth. We analysed available data from the Kepler mission concerning
  the superflaring stars in order to find tracers of anomalous magnetic
  activity. As suggested in a recent paper [1], we find that anti-solar
  differential rotation or anti-solar sign of the mirror-asymmetry of
  stellar convection can provide the desired strong magnetic field in
  dynamo models. We confirm this concept by numerical models of stellar
  dynamos with corresponding governing parameters. We conclude that the
  proposed mechanism can plausibly explain the superflaring events at
  least for some cool stars, including binaries, subgiants and, possibly,
  low-mass stars and young rapid rotators.

---------------------------------------------------------
Title: Solar Spectral Irradiance Reconstruction over 9 Millennia
    from a Composite 14C and 10Be Series
Authors: Wu, C. J.; Usoskin, I. G.; Krivova, N.; Kovaltsov, G.;
   Solanki, S. K.
2017AGUFMSH42A..03W    Altcode:
  The Sun is the main external energy source to the Earth and thus the
  knowledge of solar variability on different time scales is important
  for understanding the solar influence on the terrestrial atmosphere
  and climate. The overall energy input and its spectral distribution
  are described by the total (TSI) and spectral (SSI) solar irradiance,
  respectively. Direct measurements of the solar irradiance provide
  information on solar variability on the decadal and shorter time
  scales, while the sunspot number record covers four centuries. On
  yet longer time scales only indirect proxies can be used, such
  as the concentrations of the cosmogenic isotopes 10Be and 14C in
  terrestrial archives. These isotopes are produced in the terrestrial
  atmosphere by impinging cosmic rays, whose flux is modulated by solar
  activity. Therefore the isotope data retrieved from various natural
  archives around the globe show a very high degree of similarity
  reflecting changes in the solar activity. Nevertheless, significant
  short-term deviations can be observed due to the different geochemical
  production processes and local climatic conditions. We will present
  the newest TSI/SSI reconstruction over the last 9000 years based
  on a new consistent composite multi-isotope proxy series. The solar
  irradiance reconstruction reveals the global and robust pattern of
  solar variability in the past.

---------------------------------------------------------
Title: The Maunder minimum and the Little Ice Age: an update from
    recent reconstructions and climate simulations
Authors: Owens, Mathew J.; Lockwood, Mike; Hawkins, Ed; Usoskin,
   Ilya; Jones, Gareth S.; Barnard, Luke; Schurer, Andrew; Fasullo, John
2017JSWSC...7A..33O    Altcode:
  The Maunder minimum (MM) was a period of extremely low solar activity
  from approximately AD 1650 to 1715. In the solar physics literature, the
  MM is sometimes associated with a period of cooler global temperatures,
  referred to as the Little Ice Age (LIA), and thus taken as compelling
  evidence of a large, direct solar influence on climate. In this
  study, we bring together existing simulation and observational
  studies, particularly the most recent solar activity and paleoclimate
  reconstructions, to examine this relation. Using northern hemisphere
  surface air temperature reconstructions, the LIA can be most readily
  defined as an approximately 480 year period spanning AD 1440-1920,
  although not all of this period was notably cold. While the MM occurred
  within the much longer LIA period, the timing of the features are
  not suggestive of causation and should not, in isolation, be used
  as evidence of significant solar forcing of climate. Climate model
  simulations suggest multiple factors, particularly volcanic activity,
  were crucial for causing the cooler temperatures in the northern
  hemisphere during the LIA. A reduction in total solar irradiance likely
  contributed to the LIA at a level comparable to changing land use.

---------------------------------------------------------
Title: GLE and Sub-GLE Redefinition in the Light of High-Altitude
    Polar Neutron Monitors
Authors: Poluianov, S. V.; Usoskin, I. G.; Mishev, A. L.; Shea, M. A.;
   Smart, D. F.
2017SoPh..292..176P    Altcode: 2017arXiv171106161P
  The conventional definition of ground-level enhancement (GLE) events
  requires a detection of solar energetic particles (SEP) by at least two
  differently located neutron monitors. Some places are exceptionally
  well suitable for ground-based detection of SEP - high-elevation
  polar regions with negligible geomagnetic and reduced atmospheric
  energy/rigidity cutoffs. At present, there are two neutron-monitor
  stations in such locations on the Antarctic plateau: SOPO/SOPB (at
  Amundsen-Scott station, 2835 m elevation), and DOMC/DOMB (at Concordia
  station, 3233 m elevation). Since 2015, when the DOMC/DOMB station
  started continuous operation, a relatively weak SEP event that was
  not detected by sea-level neutron-monitor stations was registered
  by both SOPO/SOPB and DOMC/DOMB, and it was accordingly classified
  as a GLE. This would lead to a distortion of the homogeneity of the
  historic GLE list and the corresponding statistics. To address this
  issue, we propose to modify the GLE definition so that it maintains
  the homogeneity: A GLE event is registered when there are near-time
  coincident and statistically significant enhancements of the count rates
  of at least two differently located neutron monitors, including at least
  one neutron monitor near sea level and a corresponding enhancement in
  the proton flux measured by a space-borne instrument(s). Relatively weak
  SEP events registered only by high-altitude polar neutron monitors,
  but with no response from cosmic-ray stations at sea level, can be
  classified as sub-GLEs.

---------------------------------------------------------
Title: Assessment of spectral and angular characteristics of sub-GLE
    events using the global neutron monitor network
Authors: Mishev, Alexander; Poluianov, Stepan; Usoskin, Ilya
2017JSWSC...7A..28M    Altcode:
  New recently installed high-altitude polar neutron monitors (NMs)
  have made the worldwide NM network more sensitive to strong solar
  energetic particle (SEP) events, registered at ground level, namely
  ground-level enhancement (GLE) events. The DOMC/B and South Pole NMs in
  addition to marginal cut-off rigidity also possess lower atmospheric
  cut-off compared to the sea level. As a result, the two high-altitude
  polar NM stations are able to detect lower energy SEP events, which
  most likely would not be registered by the other (near sea level)
  NMs. Here, we consider several candidates for such type of events
  called sub-GLEs. Using the worldwide NM database (NMDB) records and
  an optimization procedure combined with simulation of the global NM
  network response, we assess the spectral and angular characteristics
  of sub-GLE particles. With the estimated spectral characteristics as
  an input, we evaluate the effective dose rate in polar and sub-polar
  regions at typical commercial flight altitude. Hence, we demonstrate
  that the global NM network is a useful tool to estimate important
  space weather effects, e.g., the aircrew exposure due to cosmic rays
  of galactic and/or solar origins.

---------------------------------------------------------
Title: Neutron Monitors and Cosmogenic Isotopes as Cosmic Ray
Energy-Integration Detectors: Effective Yield Functions, Effective
    Energy, and Its Dependence on the Local Interstellar Spectrum
Authors: Asvestari, Eleanna; Gil, Agnieszka; Kovaltsov, Gennady A.;
   Usoskin, Ilya G.
2017JGRA..122.9790A    Altcode:
  The method of assessment of galactic cosmic rays (GCR) variability over
  different timescales, using energy-integrating ground-based detectors
  such as a neutron monitor and cosmogenic isotopes <SUP>10</SUP>Be
  and <SUP>14</SUP>C stored in natural archives is revisited here. The
  effective yield functions for cosmogenic <SUP>14</SUP>C (globally
  mixed in the atmosphere) and <SUP>10</SUP>Be (realistically deposited
  in the polar region) are calculated and provided, in a tabulated form,
  in the supporting information. The effective energy of a detector is
  redefined so that the variability of the flux of GCR particles at this
  energy is equal to that of the detector's count rate. The effective
  energy is found as 11-12 GeV/nucleon for the standard polar neutron
  monitor, and 6-7 GeV/nucleon and 5.5-6 GeV/nucleon for <SUP>14</SUP>C
  and <SUP>10</SUP>Be, respectively. New "calibration" relations between
  the force-field modulation potentials, based on different models of
  local interstellar spectra (LIS) are provided. While such relations
  are typically based on refitting the modeled cosmic ray spectra with
  a prescribed LIS model, the method introduced here straightforwardly
  accounts for the exact type of the detector used to assess the
  spectrum. The relations are given separately for ground-based neutron
  monitors and cosmogenic isotopes. This work allows for harmonization
  of different works related to variability of galactic cosmic ray flux
  in the vicinity of Earth, on long-term scale.

---------------------------------------------------------
Title: Analysis of Ground Level Enhancements (GLE): Extreme solar
    energetic particle events have hard spectra
Authors: Asvestari, E.; Willamo, T.; Gil, A.; Usoskin, I. G.;
   Kovaltsov, G. A.; Mikhailov, V. V.; Mayorov, A.
2017AdSpR..60..781A    Altcode: 2016arXiv161202446A
  Nearly 70 Ground Level Enhancements (GLEs) of cosmic rays have
  been recorded by the worldwide neutron monitor network since the
  1950s depicting a big variety of energy spectra of solar energetic
  particles (SEP). Here we studied a statistical relation between
  the event-integrated intensity of GLEs (calculated as count-rate
  relative excess, averaged over all available polar neutron monitors,
  and expressed in percent-hours) and the hardness of the solar
  particle energy spectra. For each event the integral omnidirectional
  event-integrated fluences of particles with energy above 30 MeV
  (F<SUB>30</SUB>) and above 200 MeV (F<SUB>200</SUB>) were computed using
  the reconstructed spectra, and the ratio between the two fluences was
  considered as a simple index of the event's hardness. We also provided a
  justification of the spectrum estimate in the form of the Band-function,
  using direct PAMELA data for GLE 71 (17-May-2012). We found that, while
  there is no clear relation between the intensity and the hardness for
  weak events, all strong events with the intensity greater 100 %∗h
  are characterized by a very hard spectrum. This implies that a hard
  spectrum can be securely assumed for all extreme GLE events, e.g.,
  those studied using cosmogenic isotope data in the past.

---------------------------------------------------------
Title: New reconstruction of the sunspot group numbers since 1739
    using direct calibration and "backbone" methods
Authors: Chatzistergos, Theodosios; Usoskin, Ilya G.; Kovaltsov,
   Gennady A.; Krivova, Natalie A.; Solanki, Sami K.
2017A&A...602A..69C    Altcode: 2017arXiv170206183C
  Context. The group sunspot number (GSN) series constitute the longest
  instrumental astronomical database providing information on solar
  activity. This database is a compilation of observations by many
  individual observers, and their inter-calibration has usually been
  performed using linear rescaling. There are multiple published series
  that show different long-term trends for solar activity. <BR /> Aims:
  We aim at producing a GSN series, with a non-linear non-parametric
  calibration. The only underlying assumptions are that the differences
  between the various series are due to different acuity thresholds
  of the observers, and that the threshold of each observer remains
  constant throughout the observing period. <BR /> Methods: We used a
  daisy chain process with backbone (BB) observers and calibrated all
  overlapping observers to them. We performed the calibration of each
  individual observer with a probability distribution function (PDF)
  matrix constructed considering all daily values for the overlapping
  period with the BB. The calibration of the BBs was carried out in a
  similar manner. The final series was constructed by merging different
  BB series. We modelled the propagation of errors straightforwardly
  with Monte Carlo simulations. A potential bias due to the selection
  of BBs was investigated and the effect was shown to lie within the 1σ
  interval of the produced series. The exact selection of the reference
  period was shown to have a rather small effect on our calibration
  as well. <BR /> Results: The final series extends back to 1739 and
  includes data from 314 observers. This series suggests moderate
  activity during the 18th and 19th century, which is significantly
  lower than the high level of solar activity predicted by other recent
  reconstructions applying linear regressions. <BR /> Conclusions:
  The new series provides a robust reconstruction, based on modern and
  non-parametric methods, of sunspot group numbers since 1739, and it
  confirms the existence of the modern grand maximum of solar activity in
  the second half of the 20th century. <P />Values of the group sunspot
  number series are only available at the CDS via anonymous ftp to <A
  href="http://cdsarc.u-strasbg.fr">http://cdsarc.u-strasbg.fr</A>
  (<A href="http://130.79.128.5">http://130.79.128.5</A>) or via <A
  href="http://cdsarc.u-strasbg.fr/viz-bin/qcat?J/A+A/602/A69">http://cdsarc.u-strasbg.fr/viz-bin/qcat?J/A+A/602/A69</A>

---------------------------------------------------------
Title: Updated sunspot group number reconstruction for 1749-1996
    using the active day fraction method
Authors: Willamo, T.; Usoskin, I. G.; Kovaltsov, G. A.
2017A&A...601A.109W    Altcode: 2017arXiv170505109W
  <BR /> Aims: Sunspot number series are composed from observations of
  hundreds of different observers that require careful normalization to
  standard conditions. Here we present a new normalized series of the
  number of sunspot groups for the period 1749-1996. <BR /> Methods:
  The reconstruction is based on the active day fraction (ADF) method,
  which is slightly updated with respect to previous works, and a revised
  database of sunspot group observations. <BR /> Results: Stability of
  some key solar observers has been evaluated against the composite
  series. The Royal Greenwich Observatory dataset appears relatively
  stable since the 1890s but is approximately 10% too low before that. A
  declining trend of 10-15% in the quality of Wolfer's observations
  is found between the 1880s and 1920s, suggesting that using him as
  the reference observer may lead to additional uncertainties. Wolf
  (small telescope) appears relatively stable between the 1860s and
  1890s, without any obvious trend. The new reconstruction reflects
  the centennial variability of solar activity as evaluated using the
  singular spectrum analysis method. It depicts a highly significant
  feature of the modern grand maximum of solar activity in the second
  half of the 20th century, being a factor 1.33-1.77 higher than during
  the 18 and 19th centuries. <BR /> Conclusions: The new series of
  the sunspot group numbers with monthly and annual resolution is
  provided forming a basis for new studies of the solar variability
  and solar dynamo for the last 250 yr. <P />Monthly values of the
  reconstructed sunspot are available at the CDS via anonymous ftp to
  <A href="http://cdsarc.u-strasbg.fr">http://cdsarc.u-strasbg.fr</A>
  (<A href="http://130.79.128.5">http://130.79.128.5</A>) or via <A
  href="http://cdsarc.u-strasbg.fr/viz-bin/qcat?J/A+A/601/A109">http://cdsarc.u-strasbg.fr/viz-bin/qcat?J/A+A/601/A109</A>

---------------------------------------------------------
Title: Assessment of different sunspot number series using the
    cosmogenic isotope <SUP>44</SUP>Ti in meteorites
Authors: Asvestari, Eleanna; Usoskin, Ilya G.; Kovaltsov, Gennady A.;
   Owens, Mathew J.; Krivova, Natalie A.; Rubinetti, Sara; Taricco, Carla
2017MNRAS.467.1608A    Altcode: 2017MNRAS.tmp..193A
  Many sunspot number series exist suggesting different levels of
  solar activity during the past centuries. Their reliability can be
  assessed only by comparing them with alternative indirect proxies. We
  test different sunspot number series against the updated record of
  cosmogenic radionuclide <SUP>44</SUP>Ti measured in meteorites. Two
  bounding scenarios of solar activity changes have been considered:
  the HH-scenario (based on the series by Svalgaard and Schatten), in
  particular, predicting moderate activity during the Maunder minimum,
  and the LL-scenario (based on the R<SUB>G</SUB> series by Lockwood et
  al.) predicting moderate activity for the 18th-19th centuries and the
  very low activity level for the Maunder minimum. For each scenario,
  the magnetic open solar flux, the heliospheric modulation potential and
  the expected production of <SUP>44</SUP>Ti were computed. The calculated
  production rates were compared with the corresponding measurements of
  <SUP>44</SUP>Ti activity in stony meteorites fallen since 1766. The
  analysis reveals that the LL-scenario is fully consistent with the
  measured <SUP>44</SUP>Ti data, in particular, recovering the observed
  secular trend between the 17th century and the Modern grand maximum. On
  the contrary, the HH-scenario appears significantly inconsistent with
  the data, mostly due to the moderate level of activity during the
  Maunder minimum. It is concluded that the HH-scenario sunspot number
  reconstruction significantly overestimates solar activity prior to the
  mid-18th century, especially during the Maunder minimum. The exact level
  of solar activity after 1750 cannot be distinguished with this method,
  since both H- and L- scenarios appear statistically consistent with
  the data.

---------------------------------------------------------
Title: Investigating the Origins of Two Extreme Solar Particle Events:
    Proton Source Profile and Associated Electromagnetic Emissions
Authors: Kocharov, Leon; Pohjolainen, Silja; Mishev, Alexander; Reiner,
   Mike J.; Lee, Jeongwoo; Laitinen, Timo; Didkovsky, Leonid V.; Pizzo,
   Victor J.; Kim, Roksoon; Klassen, Andreas; Karlicky, Marian; Cho,
   Kyung-Suk; Gary, Dale E.; Usoskin, Ilya; Valtonen, Eino; Vainio, Rami
2017ApJ...839...79K    Altcode:
  We analyze the high-energy particle emission from the Sun in two
  extreme solar particle events in which protons are accelerated to
  relativistic energies and can cause a significant signal even in the
  ground-based particle detectors. Analysis of a relativistic proton event
  is based on modeling of the particle transport and interaction, from a
  near-Sun source through the solar wind and the Earth’s magnetosphere
  and atmosphere to a detector on the ground. This allows us to deduce
  the time profile of the proton source at the Sun and compare it with
  observed electromagnetic emissions. The 1998 May 2 event is associated
  with a flare and a coronal mass ejection (CME), which were well
  observed by the Nançay Radioheliograph, thus the images of the radio
  sources are available. For the 2003 November 2 event, the low corona
  images of the CME liftoff obtained at the Mauna Loa Solar Observatory
  are available. Those complementary data sets are analyzed jointly
  with the broadband dynamic radio spectra, EUV images, and other data
  available for both events. We find a common scenario for both eruptions,
  including the flare’s dual impulsive phase, the CME-launch-associated
  decimetric-continuum burst, and the late, low-frequency type III
  radio bursts at the time of the relativistic proton injection into
  the interplanetary medium. The analysis supports the idea that the
  two considered events start with emission of relativistic protons
  previously accelerated during the flare and CME launch, then trapped
  in large-scale magnetic loops and later released by the expanding CME.

---------------------------------------------------------
Title: Heliospheric modulation of cosmic rays during the neutron
monitor era: Calibration using PAMELA data for 2006-2010
Authors: Usoskin, Ilya G.; Gil, Agnieszka; Kovaltsov, Gennady A.;
   Mishev, Alexander L.; Mikhailov, Vladimir V.
2017JGRA..122.3875U    Altcode: 2017arXiv170507197U
  A new reconstruction of the heliospheric modulation potential for
  galactic cosmic rays is presented for the neutron monitor era, since
  1951. The new reconstruction is based on an updated methodology
  in comparison to previous reconstructions: (1) the use of the
  new-generation neutron monitor yield function; (2) the use of the
  new model of the local interstellar spectrum, employing in particular
  direct data from the distant missions; and (3) the calibration of the
  neutron monitor responses to direct measurements of the cosmic ray
  spectrum performed by the Payload for Antimatter Matter Exploration and
  Light-nuclei Astrophysics (PAMELA) spaceborne spectrometer over 47 time
  intervals during 2006-2010. The reconstruction is based on data from six
  standard NM64-type neutron monitors (Apatity, Inuvik, Kergulen, Moscow,
  Newark, and Oulu) since 1965 and two International Geophysical Year-type
  ground-based detectors (Climax and Mount Washington) for 1951-1964. The
  new reconstruction, along with the estimated uncertainties is tabulated
  in the paper. The presented series forms a benchmark record of the
  cosmic ray variability (in the energy range between 1 and 30 GeV) for
  the last 60 years and can be used in long-term studies in the fields
  of solar, heliospheric, and solar-terrestrial physics.

---------------------------------------------------------
Title: A history of solar activity over millennia
Authors: Usoskin, Ilya G.
2017LRSP...14....3U    Altcode:
  Presented here is a review of present knowledge of the long-term
  behavior of solar activity on a multi-millennial timescale, as
  reconstructed using the indirect proxy method. The concept of solar
  activity is discussed along with an overview of the special indices
  used to quantify different aspects of variable solar activity, with
  special emphasis upon sunspot number. Over long timescales, quantitative
  information about past solar activity can only be obtained using a
  method based upon indirect proxies, such as the cosmogenic isotopes
  ^{14}C and ^{10}Be in natural stratified archives (e.g., tree rings
  or ice cores). We give an historical overview of the development of
  the proxy-based method for past solar-activity reconstruction over
  millennia, as well as a description of the modern state. Special
  attention is paid to the verification and cross-calibration of
  reconstructions. It is argued that this method of cosmogenic isotopes
  makes a solid basis for studies of solar variability in the past on a
  long timescale (centuries to millennia) during the Holocene. A separate
  section is devoted to reconstructions of strong solar energetic-particle
  (SEP) events in the past, that suggest that the present-day average
  SEP flux is broadly consistent with estimates on longer timescales,
  and that the occurrence of extra-strong events is unlikely. Finally,
  the main features of the long-term evolution of solar magnetic activity,
  including the statistics of grand minima and maxima occurrence, are
  summarized and their possible implications, especially for solar/stellar
  dynamo theory, are discussed.

---------------------------------------------------------
Title: VizieR Online Data Catalog: Monthly numbers of sunspot groups
    1749-1996 (Usoskin+, 2017)
Authors: Usoskin, I. G.; Gallet, Y.; Lopes, F.; Kovaltsov, G. A.;
   Hulot, G.; Willamo, T.; Usoskin, I. G.; Kovaltsov, G. A.
2017yCat..36010109U    Altcode:
  The file contain the monthly numbers of sunspot groups including the
  fractional year [Y], the Mean value [G<SUB>M], the low [G</SUB>l]
  and upper [G_u] 1-sigma (68% bounds). <P />(1 data file).

---------------------------------------------------------
Title: VizieR Online Data Catalog: Monthly numbers of sunspot groups
    1749-1996 (Willamo+, 2017)
Authors: Willamo, T.; Usoskin, I. G.; Kovaltsov, G. A.
2017yCat..36010109W    Altcode:
  The file contain the monthly numbers of sunspot groups including the
  fractional year [Y], the Mean value [G<SUB>M], the low [G</SUB>l]
  and upper [G_u] 1-sigma (68% bounds). <P />(1 data file).

---------------------------------------------------------
Title: Wings of the butterfly: Sunspot groups for 1826-2015
Authors: Leussu, R.; Usoskin, I. G.; Senthamizh Pavai, V.; Diercke,
   A.; Arlt, R.; Denker, C.; Mursula, K.
2017A&A...599A.131L    Altcode:
  The spatio-temporal evolution of sunspot activity, the so-called Maunder
  butterfly diagram, has been continously available since 1874 using
  data from the Royal Greenwich Observatory, extended by SOON network
  data after 1976. Here we present a new extended butterfly diagram
  of sunspot group occurrence since 1826, using the recently digitized
  data from Schwabe (1826-1867) and Spörer (1866-1880). The wings of
  the diagram are separated using a recently developed method based
  on an analysis of long gaps in sunspot group occurrence in different
  latitude bands. We define characteristic latitudes, corresponding to
  the start, end, and the largest extent of the wings (the F, L, and
  H latitudes). The H latitudes (30°-45°) are highly significantly
  correlated with the strength of the wings (quantified by the total sum
  of the monthly numbers of sunspot groups). The F latitudes (20°-30°)
  depict a weak tendency, especially in the southern hemisphere, to follow
  the wing strength. The L latitudes (2°-10°) show no clear relation to
  the wing strength. Overall, stronger cycle wings tend to start at higher
  latitudes and have a greater wing extent. A strong (5-6)-cycle periodic
  oscillation is found in the start and end times of the wings and in the
  overlap and gaps between successive wings of one hemisphere. While the
  average wing overlap is zero in the southern hemisphere, it is two to
  three months in the north. A marginally significant oscillation of about
  ten solar cycles is found in the asymmetry of the L latitudes. The new
  long database of butterfly wings provides new observational constraints
  to solar dynamo models that discuss the spatio-temporal distribution
  of sunspot occurrence over the solar cycle and longer. <P />Digital
  data for Fig. 1 are available at the CDS via anonymous ftp to <A
  href="http://cdsarc.u-strasbg.fr">http://cdsarc.u-strasbg.fr</A>
  (<A href="http://130.79.128.5">http://130.79.128.5</A>) or via <A
  href="http://cdsarc.u-strasbg.fr/viz-bin/qcat?J/A+A/599/A131">http://cdsarc.u-strasbg.fr/viz-bin/qcat?J/A+A/599/A131</A>

---------------------------------------------------------
Title: VizieR Online Data Catalog: Group sunspot number series since
    1739 (Chatzistergos+, 2017)
Authors: Chatzistergos, T.; Usoskin, I. G.; Kovaltsov, G. A.; Krivova,
   N. A.; Solanki, S. K.
2017yCat..36020069C    Altcode:
  Annual, monthly, and daily values of the Group sunspot number series
  produced in the paper. <P />(3 data files).

---------------------------------------------------------
Title: Analysis of Ground-Level Enhancements: Strong events are hard
Authors: Usoskin, I.; Asvestari, E.; Willamo, T.; Gil, A.; Kovaltsov,
   G.; Mikhailov, V.; Mayorov, A.
2017ICRC...35..126U    Altcode: 2017PoS...301..126U
  No abstract at ADS

---------------------------------------------------------
Title: Cosmogenic isotopes Be-7, Be-10, C-14, Na-22 and Cl-36 in
the atmosphere: Altitudinal profiles of yield functions
Authors: Poluianov, S.; Kovaltsov, G.; Mishev, A.; Usoskin, I.
2017ICRC...35..124P    Altcode: 2017PoS...301..124P
  No abstract at ADS

---------------------------------------------------------
Title: Origin of two extreme solar particle events
Authors: Mishev, A.; Kocharov, L.; Pohjolainen, S.; Reiner, M. J.;
   Lee, J.; Laitinen, T.; Didkovsky, L. V.; Pizzo, V. J.; Kim, R.;
   Klassen, A.; Karlicky, M.; Choj, K. S.; Kovaltsov, G. A.; Usoskin,
   I. G.; Valtonen, E.; Vainio, R.
2017ICRC...35..146M    Altcode: 2017PoS...301..146M
  No abstract at ADS

---------------------------------------------------------
Title: Revisited definition of GLE
Authors: Poluianov, S.; Usoskin, I.; Mishev, A.; Smart, D. F.; Shea,
   M. A.
2017ICRC...35..125P    Altcode: 2017PoS...301..125P
  No abstract at ADS

---------------------------------------------------------
Title: Extreme solar particle events: Can we assess the worst case
    scenario?
Authors: Usoskin, I.
2017ICRC...35..127U    Altcode: 2017PoS...301..127U
  No abstract at ADS

---------------------------------------------------------
Title: The energetic particle intensity estimated from cosmogenic
    isotope Al-26 produced in lunar samples
Authors: Poluianov, S.; Kovaltsov, G.; Usoskin, I.
2017ICRC...35..123P    Altcode: 2017PoS...301..123P
  No abstract at ADS

---------------------------------------------------------
Title: Heliospheric modulation of galactic cosmic rays: Effective
    energy of ground-based detectors
Authors: Gil, A.; Asvestari, E.; Kovaltsov, G.; Usoskin, I.
2017ICRC...35...32G    Altcode: 2017PoS...301...32G
  No abstract at ADS

---------------------------------------------------------
Title: Computation of electron precipitation atmospheric ionization:
    updated model CRAC-EPII
Authors: Mishev, A.; Artamonov, A.; Kovaltsov, G.; Mironova, I.;
   Usoskin, I.
2017ICRC...35...86M    Altcode: 2017PoS...301...86M
  No abstract at ADS

---------------------------------------------------------
Title: Updated model CRAC:HEPII of atmospheric ionization due to
    high energy protons
Authors: Mishev, A.; Artamonov, A.; Kovalstov, G.; Usoskin, I.
2017ICRC...35...79M    Altcode: 2017PoS...301...79M
  No abstract at ADS

---------------------------------------------------------
Title: An Optical Atmospheric Phenomenon Observed in 1670 over the
    City of Astrakhan Was Not a Mid-Latitude Aurora
Authors: Usoskin, I. G.; Kovaltsov, G. A.; Mishina, L. N.; Sokoloff,
   D. D.; Vaquero, J.
2017SoPh..292...15U    Altcode: 2016arXiv161200705U
  It has recently been claimed (Zolotova and Ponyavin Solar Phys., 291,
  2869, 2016; ZP16 henceforth) that a mid-latitude optical phenomenon,
  which took place over the city of Astrakhan in July 1670, according to
  Russian chronicles, were a strong aurora borealis. If this were true,
  it would imply a very strong or even severe geomagnetic storm during
  the quietest part of the Maunder minimum. However, as we argue in this
  article, this conclusion is erroneous and caused by a misinterpretation
  of the chronicle record. As a result of a thorough analysis of the
  chronicle text, we show that the described phenomenon occurred during
  the daylight period of the day ("the last morning hour"), in the
  south ("towards noon"), and its description does not match that of an
  aurora. The date of the event was also interpreted incorrectly. We
  conclude that this phenomenon was not a mid-latitude aurora, but an
  atmospheric phenomenon, the so-called sundog (or parhelion), which is
  a particular type of solar halo. Accordingly, the claim of a strong
  mid-latitude aurora during the deep Maunder Minimum is not correct
  and should be dismissed.

---------------------------------------------------------
Title: Using global neutron monitor network data for GLE analysis:
    recent results
Authors: Mishev, A.; Usoskin, I.; Kocharov, L.
2017ICRC...35..147M    Altcode: 2017PoS...301..147M
  No abstract at ADS

---------------------------------------------------------
Title: Dependence of the Sunspot-Group Size on the Level of Solar
    Activity and its Influence on the Calibration of Solar Observers
Authors: Usoskin, I. G.; Kovaltsov, G. A.; Chatzistergos, T.
2016SoPh..291.3793U    Altcode: 2016SoPh..tmp..181U; 2016arXiv160900569U
  We study the distribution of the sunspot-group size (area) and its
  dependence on the level of solar activity. We show that the fraction
  of small groups is not constant but decreases with the level of
  solar activity so that high solar activity is mainly defined by
  large groups. We analyze the possible influence of solar activity
  on the ability of a realistic observer to see and report the daily
  number of sunspot groups. It is shown that the relation between the
  number of sunspot groups as seen by different observers with different
  observational acuity thresholds is strongly nonlinear and cannot be
  approximated by the traditionally used linear scaling (k -factors). The
  observational acuity threshold [A<SUB>th</SUB>] is considered to
  quantify the quality of each observer, instead of the traditional
  relative k -factor. A nonlinear c -factor based on A<SUB>th</SUB> is
  proposed, which can be used to correct each observer to the reference
  conditions. The method is tested on a pair of principal solar observers,
  Wolf and Wolfer, and it is shown that the traditional linear correction,
  with the constant k -factor of 1.66 to scale Wolf to Wolfer, leads to
  an overestimate of solar activity around solar maxima.

---------------------------------------------------------
Title: Solar Total and Spectral Irradiance Reconstruction over Last
    9000 Years
Authors: Wu, C. J.; Krivova, N.; Solanki, S. K.; Usoskin, I. G.
2016AGUFMSA51B2430W    Altcode:
  Although the mechanisms of solar influence on Earth climate system
  are not yet fully understood, solar total and spectral irradiance are
  considered to be among the main determinants. Solar total irradiance
  is the total flux of solar radiative energy entering Earth's climate
  system, whereas the spectral irradiance describes this energy is
  distributed over the spectrum. Solar irradiance in the UV band is of
  special importance since it governs chemical processes in the middle and
  upper atmosphere. On timescales of the 11-year solar cycle and shorter,
  solar irradiance is measured by space-based instruments while models
  are needed to reconstruct solar irradiance on longer timescale. The
  SATIRE-M model (Spectral And Total Irradiance Reconstruction over
  millennia) is employed in this study to reconstruct solar irradiance
  from decadal radionuclide isotope data such as 14C and 10Be stored in
  tree rings and ice cores, respectively. A reconstruction over the last
  9000 years will be presented.

---------------------------------------------------------
Title: Non-linear re-calibration of group sunspot number series back
    to 1819
Authors: Chatzistergos, T.; Usoskin, I. G.; Kovaltsov, G.; Solanki,
   S. K.; Krivova, N.
2016AGUFMSH31B2547C    Altcode:
  Sunspot numbers form the longest series of direct observations
  that give information about the activity of the Sun. It consists in
  numerous records from different observers with different instruments
  and techniques, and unavoidably requires a calibration of individual
  observers to a standard reference condition. Such calibrations pose a
  challenge and are still a subject of debate. Most of the calibration
  methods are based on a simple linear scaling of data from one observer
  to the other, proposed in the mid-19th century by Rudolf Wolf. This
  method is still used in many recent reconstructions. However, this
  linear method is shown, on both real and synthetic data, to be
  very rough and incorrect because of the essentially non-linearity
  of the relation.Here we present a new reconstruction of the
  group sunspot number series back to 1819 attempting to take into
  account the non-linearity of the relation between data of different
  observers. We use an approach incorporating several overlapping backbone
  observers (similar to Svalgaard and Schatten, 2016) and perform the
  straightforward non-linear calibration of each observer to the backbone
  (and the backbones with each other) based on the actual statistics of
  the common daily values.

---------------------------------------------------------
Title: Application of a full chain analysis using neutron monitor
    data for space weather studies
Authors: Mishev, A.; Usoskin, I.
2016arXiv161207043M    Altcode:
  An important topic in the field of space weather is the precise
  assessment of the contribution of galactic cosmic rays and solar
  energetic particles on air crew exposure, specifically during eruptive
  events on the Sun. Here we present a model, a full chain analysis based
  on ground based measurements of cosmic rays with neutron monitors,
  subsequent derivation of particle spectral and angular characteristics
  and computation of dose rate. The model uses method for ground level
  enhancement analysis and newly numerically computed yield functions
  for conversion of secondary particle fluence to effective dose and/or
  the ambient dose equivalent. The precise an adequate information
  about the solar energetic particle spectra (SEPs) is the basis of the
  model. Since SEPs possess an essential isotropic part, specifically
  during the event onset, the angular characteristics should be also
  derived with good precision. This can be achieved using neutron
  monitor data during a special class of SEP events the ground level
  enhancements (GLEs). On the basis of the method representing a sequence
  of consecutive steps: computation of the NM asymptotic cones, NM
  rigidity cut-off and application of convenient optimization procedure,
  we derive the rigidity spectra and anisotropy characteristics of GLE
  particles. For the computation we use newly computed yield function of
  the standard sea-level 6NM64 neutron monitor for primary proton and
  alpha CR nuclei as well as 6NM64 yield function at altitudes ranging
  from the sea level up to 5000 m above the sea level. We derive the SEP
  spectra and pitch angle distributions in their dynamical development
  throughout the event. Subsequently on the basis of the derived spectra
  and angular characteristics and previously computed yield functions
  we calculate the effective dose and/or ambient dose equivalent during
  the GLE. Several examples are shown.

---------------------------------------------------------
Title: Tests of Sunspot Number Sequences: 2. Using Geomagnetic and
    Auroral Data
Authors: Lockwood, M.; Owens, M. J.; Barnard, L.; Scott, C. J.;
   Usoskin, I. G.; Nevanlinna, H.
2016SoPh..291.2811L    Altcode: 2016SoPh..tmp...96L; 2016arXiv160501948L
  We compare four sunspot-number data sequences against geomagnetic
  and terrestrial auroral observations. The comparisons are made
  for the original Solar Influences Data Center (SIDC) composite of
  Wolf/Zürich/International sunspot number [R<SUB>ISNv1</SUB>],
  the group sunspot number [R<SUB>G</SUB>] by Hoyt and Schatten
  (Solar Phys. 181, 491, 1998), the new "backbone" group sunspot
  number [R<SUB>BB</SUB>] by Svalgaard and Schatten (Solar Phys.,
  DOI, 2016), and the "corrected" sunspot number [R<SUB>C</SUB>] by
  Lockwood, Owens, and Barnard (J. Geophys. Res. 119, 5172, 2014a). Each
  sunspot number is fitted with terrestrial observations, or parameters
  derived from terrestrial observations to be linearly proportional
  to sunspot number, over a 30-year calibration interval of 1982 -
  2012. The fits are then used to compute test sequences, which extend
  further back in time and which are compared to R<SUB>ISNv1</SUB>,
  R<SUB>G</SUB>, R<SUB>BB</SUB>, and R<SUB>C</SUB>. To study the long-term
  trends, comparisons are made using averages over whole solar cycles
  (minimum-to-minimum). The test variations are generated in four ways:
  i) using the IDV(1d) and IDV geomagnetic indices (for 1845 - 2013)
  fitted over the calibration interval using the various sunspot numbers
  and the phase of the solar cycle; ii) from the open solar flux (OSF)
  generated for 1845 - 2013 from four pairings of geomagnetic indices by
  Lockwood et al. (Ann. Geophys. 32, 383, 2014a) and analysed using the
  OSF continuity model of Solanki, Schüssler, and Fligge (Nature, 408,
  445, 2000), which employs a constant fractional OSF loss rate; iii)
  the same OSF data analysed using the OSF continuity model of Owens and
  Lockwood (J. Geophys. Res. 117, A04102, 2012), in which the fractional
  loss rate varies with the tilt of the heliospheric current sheet and
  hence with the phase of the solar cycle; iv) the occurrence frequency
  of low-latitude aurora for 1780 - 1980 from the survey of Legrand and
  Simon (Ann. Geophys. 5, 161, 1987). For all cases, R<SUB>BB</SUB>
  exceeds the test terrestrial series by an amount that increases as
  one goes back in time.

---------------------------------------------------------
Title: Atmospheric ionization induced by precipitating electrons:
Comparison of CRAC:EPII model with a parametrization model
Authors: Artamonov, A. A.; Mishev, A. L.; Usoskin, I. G.
2016JASTP.149..161A    Altcode: 2016arXiv160105910A
  Results of a comparison of a new model CRAC:EPII (Cosmic Ray Atmospheric
  Cascade: Electron Precipitation Induced Ionization) with a commonly used
  parametric model of atmospheric ionization is presented. The CRAC:EPII
  is based on a Monte Carlo simulation of precipitating electrons
  propagation and interaction with matter in the Earth's atmosphere. It
  explicitly considers energy deposit: ionization, pair production,
  Compton scattering, generation of Bremsstrahlung high energy photons,
  photo-ionization and annihilation of positrons, multiple scattering as
  physical processes accordingly. Propagation of precipitating electrons
  and their interactions with air is simulated with the GEANT4 simulation
  tool PLANETOCOSMICS code using NRLMSISE-00 atmospheric model. Ionization
  yields are computed and compared with a parametrization model for
  different energies of incident precipitating energetic electrons, using
  simulated fluxes of mono-energetic particles. A good agreement between
  the two models is achieved in the mesosphere but the contribution of
  Bremsstrahlung in the stratosphere, which is not accounted for in the
  parametric models, is found significant. As an example, we calculated
  profiles of the ion production rates in the middle and upper atmosphere
  (below 100 km) on the basis of balloon-born measured spectra of
  precipitating electrons for 30-October-2002 and 07-January-2004.

---------------------------------------------------------
Title: A New Calibrated Sunspot Group Series Since 1749: Statistics
    of Active Day Fractions
Authors: Usoskin, I. G.; Kovaltsov, G. A.; Lockwood, M.; Mursula,
   K.; Owens, M.; Solanki, S. K.
2016SoPh..291.2685U    Altcode: 2016SoPh..tmp....6U; 2015arXiv151206421U
  Although sunspot-number series have existed since the mid-nineteenth
  century, they are still the subject of intense debate, with the largest
  uncertainty being related to the "calibration" of the visual acuity
  of individual observers in the past. A daisy-chain regression method
  is usually applied to inter-calibrate the observers, which may lead
  to significant bias and error accumulation. Here we present a novel
  method for calibrating the visual acuity of the key observers to the
  reference data set of Royal Greenwich Observatory sunspot groups for the
  period 1900 - 1976, using the statistics of the active-day fraction. For
  each observer we independently evaluate their observational thresholds
  [S<SUB>S</SUB>] defined such that the observer is assumed to miss all
  of the groups with an area smaller than S<SUB>S</SUB> and report all
  the groups larger than S<SUB>S</SUB>. Next, using a Monte-Carlo method,
  we construct a correction matrix for each observer from the reference
  data set. The correction matrices are significantly non-linear and
  cannot be approximated by a linear regression or proportionality. We
  emphasize that corrections based on a linear proportionality between
  annually averaged data lead to serious biases and distortions of the
  data. The correction matrices are applied to the original sunspot-group
  records reported by the observers for each day, and finally the
  composite corrected series is produced for the period since 1748. The
  corrected series is provided as supplementary material in electronic
  form and displays secular minima around 1800 (Dalton Minimum) and 1900
  (Gleissberg Minimum), as well as the Modern Grand Maximum of activity in
  the second half of the twentieth century. The uniqueness of the grand
  maximum is confirmed for the last 250 years. We show that the adoption
  of a linear relationship between the data of Wolf and Wolfer results
  in grossly inflated group numbers in the eighteenth and nineteenth
  centuries in some reconstructions.

---------------------------------------------------------
Title: VizieR Online Data Catalog: Butterfly diagram wings (Leussu+,
    2017)
Authors: Leussu, R.; Usoskin, I. G.; Senthamizh Pavai, V.; Diercke,
   A.; Arlt, R.; Mursula, K.
2016yCat..35990131L    Altcode:
  fig1data.dat contains the separated wings in a butterfly diagram for
  sunspot groups from three different origins: Sunspot observations
  by S.H. Schwabe and G. Spoerer, and the RGO/SOON compilation. The
  latitudes for sunspot groups from the Schwabe and Spoerer data
  are given as size-weighted averages from sunspots belonging to each
  group. Latitudes for the RGO compilation are given as they are stated
  in the original data. The columns report the year, month, day, date
  [yr], latitude [deg], cycle, hemisphere, and data set tag. Northern
  hemisphere wings are tagged with "1" and southern hemisphere wings with
  "2". The data set tag is "1" for Schwabe data, "2" for Spoerer data and
  "3" for RGO data. <P />(1 data file).

---------------------------------------------------------
Title: Tests of Sunspot Number Sequences: 3. Effects of Regression
    Procedures on the Calibration of Historic Sunspot Data
Authors: Lockwood, M.; Owens, M. J.; Barnard, L.; Usoskin, I. G.
2016SoPh..291.2829L    Altcode: 2015arXiv151007809L; 2016SoPh..tmp...20L
  We use sunspot-group observations from the Royal Greenwich Observatory
  (RGO) to investigate the effects of intercalibrating data from observers
  with different visual acuities. The tests are made by counting the
  number of groups [R<SUB>B</SUB>] above a variable cut-off threshold
  of observed total whole spot area (uncorrected for foreshortening)
  to simulate what a lower-acuity observer would have seen. The
  synthesised annual means of R<SUB>B</SUB> are then re-scaled to
  the full observed RGO group number [R<SUB>A</SUB>] using a variety
  of regression techniques. It is found that a very high correlation
  between R<SUB>A</SUB> and R<SUB>B</SUB> (r<SUB>AB</SUB>&gt;0.98 )
  does not prevent large errors in the intercalibration (for example
  sunspot-maximum values can be over 30 % too large even for such
  levels of r<SUB>AB</SUB>). In generating the backbone sunspot number
  [R<SUB>BB</SUB>], Svalgaard and Schatten (Solar Phys., 2016) force
  regression fits to pass through the scatter-plot origin, which generates
  unreliable fits (the residuals do not form a normal distribution) and
  causes sunspot-cycle amplitudes to be exaggerated in the intercalibrated
  data. It is demonstrated that the use of Quantile-Quantile ("Q-Q") plots
  to test for a normal distribution is a useful indicator of erroneous
  and misleading regression fits. Ordinary least-squares linear fits,
  not forced to pass through the origin, are sometimes reliable (although
  the optimum method used is shown to be different when matching peak
  and average sunspot-group numbers). However, other fits are only
  reliable if non-linear regression is used. From these results it is
  entirely possible that the inflation of solar-cycle amplitudes in the
  backbone group sunspot number as one goes back in time, relative to
  related solar-terrestrial parameters, is entirely caused by the use
  of inappropriate and non-robust regression techniques to calibrate
  the sunspot data.

---------------------------------------------------------
Title: Balloon measurements of the vertical ionization profile over
    southern Israel and comparison to mid-latitude observations
Authors: Yaniv, Roy; Yair, Yoav; Price, Colin; Nicoll, Keri; Harrison,
   Giles; Artamonov, Anton; Usoskin, Ilya
2016JASTP.149...87Y    Altcode:
  Airborne measurements using meteorological balloons were conducted
  for the first time from southern Israel (geographic 30°35'N, 34°45'E
  geomagnetic 27°6'N 112°23'E) for measuring the vertical ionization
  profile during solar cycle 24. The results show the differences
  (increase of 30%) in count rates as we proceed from solar maximum
  toward solar minimum. The observed altitude of maximum ionization
  (the Regener-Pfotzer maximum) was between 17-20 km, and it agrees
  well with results from other simultaneous measurements conducted at
  different latitudes (Reading, UK and Zaragoza-Barcelona, Spain). When
  compared with predictions of an analytical model, we find a highly
  significant correlation (R<SUP>2</SUP>=0.97) between our observations
  and the computed ionization profiles. The difference in count rates can
  be attributed to the height of the tropopause due to the model using
  a US standard atmosphere that differs from the measured atmospheric
  parameters above Israel.

---------------------------------------------------------
Title: Properties of sunspot cycles and hemispheric wings since the
    19th century
Authors: Leussu, Raisa; Usoskin, Ilya G.; Arlt, Rainer; Mursula, Kalevi
2016A&A...592A.160L    Altcode:
  <BR /> Aims: The latitudinal evolution of sunspot emergence over
  the course of the solar cycle, the so-called butterfly diagram, is a
  fundamental property of the solar dynamo. Here we present a study of
  the butterfly diagram of sunspot group occurrence for cycles 7-10 and
  11-23 using data from a recently digitized sunspot drawings by Samuel
  Heinrich Schwabe in 1825-1867, and from RGO/USAF/NOAA(SOON) compilation
  of sunspot groups in 1874-2015. <BR /> Methods: We developed a new,
  robust method of hemispheric wing separation based on an analysis of
  long gaps in sunspot group occurrence in different latitude bands. The
  method makes it possible to ascribe each sunspot group to a certain
  wing (solar cycle and hemisphere), and separate the old and new cycle
  during their overlap. This allows for an improved study of solar
  cycles compared to the common way of separating the cycles. <BR />
  Results: We separated each hemispheric wing of the butterfly diagram
  and analysed them with respect to the number of groups appearing in
  each wing, their lengths, hemispheric differences, and overlaps. <BR
  /> Conclusions: The overlaps of successive wings were found to be
  systematically longer in the northern hemisphere for cycles 7-10,
  but in the southern hemisphere for cycles 16-22. The occurrence of
  sunspot groups depicts a systematic long-term variation between the
  two hemispheres. During Schwabe time, the hemispheric asymmetry was
  north-dominated during cycle 9 and south-dominated during cycle 10.

---------------------------------------------------------
Title: Corrigendum to 'A review of Holocene solar-linked climatic
variation on centennial to millennial timescales: Physical processes,
    interpretative frameworks and a new multiple cross-wavelet transform
    algorithm' Earth Sci. Rev. 134 [1-15]
Authors: Soon, Willie; Velasco Herrera, Victor M.; Selvaraj, Kandasamy;
   Traversi, Rita; Usoskin, Ilya; Arthur Chen, Chen-Tung; Lou, Jiann-Yuh;
   Kao, Shuh-Ji; Carter, Robert M.; Pipin, Valery; Severi, Mirko;
   Becagli, Silvia
2016ESRv..159..462S    Altcode:
  In the article "A review of Holocene solar-linked climatic variation on
  centennial to millennial timescales: Physical processes, interpretative
  frameworks and a new multiple cross-wavelet transform algorithm",
  published in Earth-Science Reviews 134 (2014) 1, it was omitted to
  state that at the time this article was submitted the corresponding
  author Dr. Soon received funding from the Southern Company Services and
  Donors Trust. We have no indication that this funding has influenced
  the results presented in the article.

---------------------------------------------------------
Title: Production of cosmogenic isotopes <SUP>7</SUP>Be,
    <SUP>10</SUP>Be, <SUP>14</SUP>C, <SUP>22</SUP>Na, and <SUP>36</SUP>Cl
in the atmosphere: Altitudinal profiles of yield functions
Authors: Poluianov, S. V.; Kovaltsov, G. A.; Mishev, A. L.; Usoskin,
   I. G.
2016JGRD..121.8125P    Altcode: 2016arXiv160605899P
  New consistent and precise computations of the production of
  five cosmogenic radioisotopes, <SUP>7</SUP>Be, <SUP>10</SUP>Be,
  <SUP>14</SUP>C, <SUP>22</SUP>Na, and <SUP>36</SUP>Cl, in the Earth's
  atmosphere by cosmic rays are presented in the form of tabulated yield
  functions. For the first time, a detailed set of the altitude profiles
  of the production functions is provided which makes it possible to apply
  the results directly as input for atmospheric transport models. Good
  agreement with most of the earlier published works for columnar and
  global isotopic production rates is shown. Altitude profiles of the
  production are important, in particular for such tasks as studies of
  strong solar particle events in the past, precise reconstructions of
  solar activity on long-term scale, tracing air mass dynamics using
  cosmogenic radioisotopes, etc. As an example, computations of the
  <SUP>10</SUP>Be deposition flux in the polar region are shown for the
  last decades and also for a period around 780 A.D. and confronted with
  the actual measurements in Greenland and Antarctic ice cores.

---------------------------------------------------------
Title: Solar total and spectral irradiance reconstruction over last
    9000 years
Authors: Wu, Chi-Ju; Usoskin, Ilya; Krivova, Natalie; Solanki, Sami K.
2016cosp...41E2072W    Altcode:
  Although the mechanisms of solar influence on Earth climate system
  are not yet fully understood, solar total and spectral irradiance are
  considered to be among the main determinants. Solar total irradiance
  is the total flux of solar radiative energy entering Earth's climate
  system, whereas the spectral irradiance describes this energy is
  distributed over the spectrum. Solar irradiance in the UV band is of
  special importance since it governs chemical processes in the middle and
  upper atmosphere. On timescales of the 11-year solar cycle and shorter,
  solar irradiance is measured by space-based instruments while models
  are needed to reconstruct solar irradiance on longer timescale. The
  SATIRE-M model (Spectral And Total Irradiance Reconstruction over
  millennia) is employed in this study to reconstruct solar irradiance
  from decadal radionuclide isotope data such as 14C and 10Be stored in
  tree rings and ice cores, respectively. A reconstruction over the last
  9000 years will be presented.

---------------------------------------------------------
Title: Near-Earth heliospheric magnetic field intensity since 1750:
    2. Cosmogenic radionuclide reconstructions
Authors: Owens, M. J.; Cliver, E.; McCracken, K. G.; Beer, J.; Barnard,
   L.; Lockwood, M.; Rouillard, A.; Passos, D.; Riley, P.; Usoskin, I.;
   Wang, Y. -M.
2016JGRA..121.6064O    Altcode:
  This is Part 2 of a study of the near-Earth heliospheric magnetic field
  strength, B, since 1750. Part 1 produced composite estimates of B from
  geomagnetic and sunspot data over the period 1750-2013. Sunspot-based
  reconstructions can be extended back to 1610, but the paleocosmic ray
  (PCR) record is the only data set capable of providing a record of
  solar activity on millennial timescales. The process for converting
  <SUP>10</SUP>Be concentrations measured in ice cores to B is more
  complex than with geomagnetic and sunspot data, and the uncertainties
  in B derived from cosmogenic nuclides (~20% for any individual year)
  are much larger. Within this level of uncertainty, we find reasonable
  overall agreement between PCR-based B and the geomagnetic- and sunspot
  number-based series. This agreement was enhanced by excising low values
  in PCR-based B attributed to high-energy solar proton events. Other
  discordant intervals, with as yet unspecified causes remain included in
  our analysis. Comparison of 3 year averages centered on sunspot minimum
  yields reasonable agreement between the three estimates, providing a
  means to investigate the long-term changes in the heliospheric magnetic
  field into the past even without a means to remove solar proton events
  from the records.

---------------------------------------------------------
Title: Near-Earth heliospheric magnetic field intensity since 1750:
    1. Sunspot and geomagnetic reconstructions
Authors: Owens, M. J.; Cliver, E.; McCracken, K. G.; Beer, J.; Barnard,
   L.; Lockwood, M.; Rouillard, A.; Passos, D.; Riley, P.; Usoskin, I.;
   Wang, Y. -M.
2016JGRA..121.6048O    Altcode:
  We present two separate time series of the near-Earth heliospheric
  magnetic field strength (B) based on geomagnetic data and sunspot number
  (SSN). The geomagnetic-based B series from 1845 to 2013 is a weighted
  composite of two series that employ the interdiurnal variability index;
  this series is highly correlated with in situ spacecraft measurements
  of B (correlation coefficient, r = 0.94; mean square error, MSE =
  0.16 nT<SUP>2</SUP>). The SSN-based estimate of B, from 1750 to 2013,
  is a weighted composite of eight time series derived from two separate
  reconstruction methods applied to four different SSN time series,
  allowing determination of the uncertainty from both the underlying
  sunspot records and the B reconstruction methods. The SSN-based
  composite is highly correlated with direct spacecraft measurements of B
  and with the composite geomagnetic B time series from 1845 to 2013 (r =
  0.91; MSE = 0.24 nT<SUP>2</SUP>), demonstrating that B can accurately
  reconstructed by both geomagnetic and sunspot-based methods. The
  composite sunspot and geomagnetic B time series, with uncertainties,
  are provided as supporting information.

---------------------------------------------------------
Title: Application of the new neutron monitor yield function computed
    for different altitudes to an analysis of GLEs
Authors: Mishev, Alexander; Usoskin, Ilya
2016cosp...41E1310M    Altcode:
  A precise analysis of SEP (solar energetic particle) spectral and
  angular characteristics using neutron monitor (NM) data requires
  realistic modeling of propagation of those particles in the Earth's
  magnetosphere and atmosphere. On the basis of the method including a
  sequence of consecutive steps, namely a detailed computation of the
  SEP assymptotic cones of acceptance, and application of a neutron
  monitor yield function and convenient optimization procedure, we
  derived the rigidity spectra and anisotropy characteristics of several
  major GLEs. Here we present several major GLEs of the solar cycle 23:
  the Bastille day event on 14 July 2000 (GLE 59), GLE 69 on 20 January
  2005, and GLE 70 on 13 December 2006. The SEP spectra and pitch angle
  distributions were computed in their dynamical development. For the
  computation we use the newly computed yield function of the standard
  6NM64 neutron monitor for primary proton and alpha CR nuclei. In
  addition, we present new computations of NM yield function for the
  altitudes of 3000 m and 5000 m above the sea level The computations
  were carried out with Planetocosmics and CORSIKA codes as standardized
  Monte-Carlo tools for atmospheric cascade simulations. The flux of
  secondary neutrons and protons was computed using the Planetocosmics
  code appliyng a realistic curved atmospheric. Updated information
  concerning the NM registration efficiency for secondary neutrons
  and protons was used. The derived results for spectral and angular
  characteristics using the newly computed NM yield function at several
  altitudes are compared with the previously obtained ones using the
  double attenuation method.

---------------------------------------------------------
Title: Modeling impact ionization of precipitating particles in the
    upper and middle atmosphere
Authors: Mishev, Alexander; Usoskin, Ilya; Artamonov, Anton
2016cosp...41E1309M    Altcode:
  An extension of the cosmic ray ionization model CRAC:EPII (Cosmic
  Ray Atmospheric Cascade: Electron Precipitation Induced Ionization)
  is presented. It aims computation of electron impact ionization in
  the atmosphere. The CRAC:EPII is based on Monte Carlo simulations of
  electron propagation and interaction with matter, namely atmospheric
  molecules. It explicitly considers various physical process, namely pair
  production, Compton scattering, generation of Bremsstrahlung photons,
  photo-ionization, annihilation of positrons, multiple scattering
  as well as energy deposit and accordingly ionization. Propagation
  of precipitating electrons and their interactions with atmospheric
  molecules is modelled with the the PLANETOCOSMICS code. The atmospheric
  model NRLMSISE 2000 is used. The yield functions for computation of
  electron impact ionization are presented. A quantitative comparison
  with a parameterization driven model of the atmospheric ionization
  induced by precipitating electronsis is carried out. A good agreement
  is demonstrated. Several example electron spectra based on balloon-born
  measurements are used as input in the model in order to compute ion
  production in the upper and middle atmosphere. An updated ionization
  yield function by primary cosmic ray protons in the upper/middle
  atmosphere is also presented. Several examples of ion production in the
  upper and middle atmosphere due to precipitating particles are shown.

---------------------------------------------------------
Title: An Assessment of Sunspot Number Data Composites over 1845-2014
Authors: Lockwood, M.; Owens, M. J.; Barnard, L.; Usoskin, I. G.
2016ApJ...824...54L    Altcode: 2016arXiv160404538L
  New sunspot data composites, some of which are radically different in
  the character of their long-term variation, are evaluated over the
  interval 1845-2014. The method commonly used to calibrate historic
  sunspot data, relative to modern-day data, is “daisy-chaining,”
  whereby calibration is passed from one data subset to the neighboring
  one, usually using regressions of the data subsets for the intervals
  of their overlap. Recent studies have illustrated serious pitfalls in
  these regressions, and the resulting errors can be compounded by their
  repeated use as the data sequence is extended back in time. Hence, the
  recent composite data series by Usoskin et al., R <SUB>UEA</SUB>, is a
  very important advance because it avoids regressions, daisy-chaining,
  and other common, but invalid, assumptions: this is achieved by
  comparing the statistics of “active-day” fractions to those
  for a single reference data set. We study six sunspot data series,
  including R <SUB>UEA</SUB> and the new “backbone” data series
  (R <SUB>BB</SUB>, recently generated by Svalgaard &amp; Schatten by
  employing both regression and daisy-chaining). We show that all six
  can be used with a continuity model to reproduce the main features
  of the open solar flux variation for 1845-2014, as reconstructed from
  geomagnetic activity data. However, some differences can be identified
  that are consistent with tests using a basket of other proxies for
  solar magnetic fields. Using data from a variety of sunspot observers,
  we illustrate problems with the method employed in generating R
  <SUB>BB</SUB> that cause it to increasingly overestimate sunspot
  numbers going back in time, and we recommend using R <SUB>UEA</SUB>
  because it employs more robust procedures that avoid such problems.

---------------------------------------------------------
Title: Erratum: Erratum to: Analysis of the ground level enhancements
    on 14 July 2000 and on 13 December 2006 using neutron monitor data
Authors: Mishev, A.; Usoskin, I.
2016SoPh..291.1579M    Altcode: 2016SoPh..tmp..106M
  No abstract at ADS

---------------------------------------------------------
Title: Semi-empirical Long-term Reconstruction of the Heliospheric
Parameters: Validation by Cosmogenic Radionuclide Records
Authors: Asvestari, E.; Usoskin, I. G.; Cameron, R. H.; Krivova, N. A.
2016ASPC..504..269A    Altcode:
  We have developed a semi-empirical model that describes the heliospheric
  modulation of galactic cosmic rays considering different heliospheric
  parameters. This model is an improvement of a previous model. The
  parameters of the model are fitted using the observations and
  reconstructions of the heliospheric parameters for the period 1976 -
  2013, which includes the latest very weak solar minimum. The modulation
  potential is computed since 1610 using different reconstructions of the
  open solar magnetic flux and it is then used to compute the production
  and distribution of cosmogenic isotope <SUP>14</SUP>C, which was
  subsequently compared with terrestrial archives in tree rings. It is
  shown that the group sunspot number series by Svalgaard &amp; Schatten
  (2015) is inconsistent with the data, while other series agree well.

---------------------------------------------------------
Title: Extreme solar particle events: The worst case scenario
Authors: Usoskin, Ilya; Kovaltsov, Gennady
2016EGUGA..18.3898U    Altcode:
  Sporadic eruptive energetic events on the Sun may occur during
  periods of high solar activity. Sometimes such events can be strong
  or even extreme posing serious hazards for the modern technology
  and communication dependent society. It is important to asses the
  worst case scenario for an extreme solar particle event and what the
  probability of its occurrence. The era of direct scientific exploration
  of the Sun is short - from few decades to a century, and yet several
  strong harmful events took place during that time. Can we expect even
  greater events? How often? What shall we prepare for? In order to answer
  these questions, one has to rely upon indirect methods by analyzing
  natural proxy archives. Here we present an overview of the history of
  extreme solar events in the past, from hundreds to millions of year,
  based on an analysis of cosmogenic isotopes in terrestrial archives
  (polar ice cores and tree rings) and in lunar rocks.

---------------------------------------------------------
Title: Analysis of the Ground-Level Enhancements on 14 July 2000
    and 13 December 2006 Using Neutron Monitor Data
Authors: Mishev, A.; Usoskin, I.
2016SoPh..291.1225M    Altcode: 2016SoPh..tmp...46M; 2016arXiv160308918M
  On the basis of neutron monitor data, we estimate the energy spectrum,
  anisotropy axis direction, and pitch-angle distribution of solar
  energetic particles during two major ground-level enhancements (GLE
  59 on 14 July 2000 and GLE 70 on 13 December 2006). For the analysis
  we used a newly computed neutron monitor yield function. The method
  consists of several consecutive steps: definition of the asymptotic
  viewing cones of neutron monitor stations considered for the data
  analysis by computing the cosmic ray particle propagation in a
  model magnetosphere with the MAGNETOCOSMICS code, computing the
  neutron monitor model responses, and deriving the solar energetic
  particle characteristics on the basis of inverse problem solution. The
  pitch-angle distribution and rigidity spectrum of high-energy protons
  are obtained as a function of time in the course of ground-level
  enhancements. A comparison with previously reported results is performed
  and reasonable agreement is achieved. A discussion of the obtained
  results is included.

---------------------------------------------------------
Title: Solar activity during the Holocene: the Hallstatt cycle and
    its consequence for grand minima and maxima
Authors: Usoskin, I. G.; Gallet, Y.; Lopes, F.; Kovaltsov, G. A.;
   Hulot, G.
2016A&A...587A.150U    Altcode: 2016arXiv160202483U
  <BR /> Aims: Cosmogenic isotopes provide the only quantitative proxy
  for analyzing the long-term solar variability over a centennial
  timescale. While essential progress has been achieved in both
  measurements and modeling of the cosmogenic proxy, uncertainties
  still remain in the determination of the geomagnetic dipole
  moment evolution. Here we aim at improving the reconstruction of
  solar activity over the past nine millennia using a multi-proxy
  approach. <BR /> Methods: We used records of the <SUP>14</SUP>C and
  <SUP>10</SUP>Be cosmogenic isotopes, current numerical models of the
  isotope production and transport in Earth's atmosphere, and available
  geomagnetic field reconstructions, including a new reconstruction
  relying on an updated archeo- and paleointensity database. The
  obtained series were analyzed using the singular spectrum analysis
  (SSA) method to study the millennial-scale trends. <BR /> Results:
  A new reconstruction of the geomagnetic dipole field moment,
  referred to as GMAG.9k, is built for the last nine millennia. New
  reconstructions of solar activity covering the last nine millennia,
  quantified in terms of sunspot numbers, are presented and analyzed. A
  conservative list of grand minima and maxima is also provided. <BR />
  Conclusions: The primary components of the reconstructed solar activity,
  as determined using the SSA method, are different for the series that
  are based on <SUP>14</SUP>C and <SUP>10</SUP>Be. This shows that
  these primary components can only be ascribed to long-term changes
  in the terrestrial system and not to the Sun. These components have
  therefore been removed from the reconstructed series. In contrast,
  the secondary SSA components of the reconstructed solar activity are
  found to be dominated by a common ≈2400-year quasi-periodicity,
  the so-called Hallstatt cycle, in both the <SUP>14</SUP>C and
  <SUP>10</SUP>Be based series. This Hallstatt cycle thus appears to be
  related to solar activity. Finally, we show that the grand minima and
  maxima occurred intermittently over the studied period, with clustering
  near lows and highs of the Hallstatt cycle, respectively. <P />Tables
  C.1 and C.2 are only available at the CDS via anonymous ftp to <A
  href="http://cdsarc.u-strasbg.fr">http://cdsarc.u-strasbg.fr</A>
  (ftp://130.79.128.5) or via <A
  href="http://cdsarc.u-strasbg.fr/viz-bin/qcat?J/A+A/587/A150">http://cdsarc.u-strasbg.fr/viz-bin/qcat?J/A+A/587/A150</A>

---------------------------------------------------------
Title: An empirical model of heliospheric cosmic ray modulation on
    long-term time scale
Authors: Asvestari, Eleanna; Usoskin, Ilya G.
2016JSWSC...6A..15A    Altcode:
  Galactic Cosmic Rays (GCRs) entering the heliosphere are subject to
  modulation processes due to variable solar magnetic activity. Finding
  a relationship between cosmic-ray variations and the heliospheric
  parameters is important for reconstruction of solar activity in
  the past. Here, we develop a semi-empirical model describing
  the heliospheric modulation of GCRs in terms of heliospheric
  parameters such as the open solar magnetic flux, the tilt angle of
  the heliospheric current sheet and the polarity of the large scale
  solar magnetic field. Our model is fitted using annual data obtained
  for the period 1976-2013, which includes the very weak solar minimum
  during 2008-2010. The model shows a good agreement with the data,
  and therefore, can be used for reconstructions of the modulation
  potential at different levels of solar activity. The model's validity
  is also tested using the cosmogenic radionuclides <SUP>14</SUP>C
  and <SUP>10</SUP>Be stored in terrestrial archives. The tilt angle
  used to fit the parameters in our semi-empirical modulation model is
  reconstructed by a mathematical model described here.

---------------------------------------------------------
Title: Model CRAC:EPII for atmospheric ionization due to precipitating
electrons: Yield function and applications
Authors: Artamonov, A. A.; Mishev, A. L.; Usoskin, I. G.
2016JGRA..121.1736A    Altcode:
  A new model of the family of CRAC models, CRAC:EPII (Cosmic Ray
  Atmospheric Cascade: Electron Precipitation Induced Ionization),
  is presented. The model calculates atmospheric ionization induced
  by precipitating electrons and uses the formalism of ionization
  yield functions. The CRAC:EPII model is based on a full Monte Carlo
  simulation of electron propagation and interaction with the air
  molecules. It explicitly considers various physical processes, namely,
  pair production, Compton scattering, generation of bremsstrahlung
  high-energy photons, photoionization, annihilation of positrons,
  and multiple scattering. The simulations were performed using GEANT 4
  simulation tool PLANETOCOSMICS with NRLMSISE 00 atmospheric model. The
  CRAC:EPII model is applicable to the entire atmosphere. The results from
  the simulations are given as look-up table representing the ionization
  yield function. The table allows one to compute ionization due to
  precipitating electrons for a given altitude and location considering
  a given electron spectrum. Application of the model for computation
  of ion production during electron precipitation events using spectra
  from balloon-borne measurements is presented.

---------------------------------------------------------
Title: VizieR Online Data Catalog: Solar activity during the Holocene
    (Usoskin+, 2016)
Authors: Usoskin, I. G.; Gallet, Y.; Lopes, F.; Kovaltsov, G. A.;
   Hulot, G.
2016yCat..35870150U    Altcode:
  tables1.dat contains axial dipole evolution between 1500 BC and 1900
  AD as constrained by Virtual Axial Dipole Moments (VADM) averaged over
  sliding windows of 200 years shifted every 10 years. <P />tables2.dat
  contains axial dipole evolution between 6750 BC and 1500 BC as
  constrained by Virtual Axial Dipole Moments (VADM) averaged over
  sliding windows of 500 years shifted every 10 years. <P />Details on
  the computations are provided in Appendix A. <P />The columns report
  the epoch [yr], the mean VADM [Gmean] (in units of 10<SUP>22</SUP>
  Am<SUP>2</SUP>), the standard deviation [SD] and the maximum [Gmax]
  and minimum [Gmin] values defining the envelope of possible VADM
  results. <P />(2 data files).

---------------------------------------------------------
Title: Neutron monitor yield function for solar neutrons: A new
    computation
Authors: Artamonov, A. A.; Kovaltsov, G. A.; Mishev, A. L.; Usoskin,
   I. G.
2016JGRA..121..117A    Altcode:
  A new yield function of a standard neutron monitor 6NM64 for
  solar neutrons is presented and tabulated in the attached lookup
  tables. It corresponds to a wide range of altitudes of the neutron
  monitor locations and angles of incidence for neutrons entering the
  Earth's atmosphere. The computations were made by Monte Carlo using
  the GEANT4-based PLANETOCOSMICS tool. The yield function was validated
  against the measured data for solar neutron events of 3 June 1982 and
  24 May 1990, and good agreement was found within a wide range of the
  altitudes of the neutron monitor location and angles of incidence of
  solar neutron arrival. The sensitivity of the world neutron monitor
  network for registration of solar neutron events was reassessed. The
  neutron monitor network is shown to be, in addition to other methods,
  a sensitive tool for monitoring of high-energy solar-flare neutrons
  with ≈95% probability to detect statistically significantly (&gt;5σ)
  a solar neutron event similar to that of 3 June 1982.

---------------------------------------------------------
Title: A two-wave dynamo model by Zharkova et al. (2015) disagrees
    with data on long-term solar variability
Authors: Usoskin, I.; Kovaltsov, G.
2015arXiv151205516U    Altcode:
  A two-wave dynamo model was recently proposed by Zharkova et al. (2015,
  Zh15 henceforth), which aims at long-term predictions of solar activity
  for millennia ahead and backwards. Here we confront the backward
  model predictions for the last 800 years with known variability of
  solar activity, using both direct sunspot observations since 1610 and
  reconstructions based on cosmogenic radionuclide data. We show that
  the Zh15 model fails to reproduce the well-established features of
  the solar activity evolution during the last millennium. This means
  that the predictive part for the future is not reliable either.

---------------------------------------------------------
Title: Mini Neutron Monitors at Concordia Research Station, Central
    Antarctica
Authors: Poluianov, Stepan; Usoskin, Ilya; Mishev, Alexander; Moraal,
   Harm; Kruger, Helena; Casasanta, Giampietro; Traversi, Rita; Udisti,
   Roberto
2015JASS...32..281P    Altcode:
  Two mini neutron monitors are installed at Concordia research
  station (Dome C, Central Antarctica, 75° 06' S, 123° 23' E,
  3,233 m.a.s.l.). The site has unique properties ideal for cosmic ray
  measurements, especially for the detection of solar energetic particles:
  very low cutoff rigidity &lt; 0.01 GV, high elevation and poleward
  asymptotic acceptance cones pointing to geographical latitudes &gt;
  75° S. The instruments consist of a standard neutron monitor and a
  "bare" (lead-free) neutron monitor. The instrument operation started in
  mid-January 2015. The barometric correction coefficients were computed
  for the period from 1 February to 31 July 2015. Several interesting
  events, including two notable Forbush decreases on 17 March 2015
  and 22 June 2015, and a solar particle event of 29 October 2015
  were registered. The data sets are available at cosmicrays.oulu.fi
  and nmdb.eu.

---------------------------------------------------------
Title: The carbon-14 spike in the 8th century was not caused by a
    cometary impact on Earth
Authors: Usoskin, Ilya G.; Kovaltsov, Gennady A.
2015Icar..260..475U    Altcode: 2014arXiv1401.5945U
  A mysterious increase of radiocarbon 1<SUP>4</SUP> C ca. 775 AD in the
  Earth's atmosphere has been recently found by Miyake et al. (Miyake,
  F., Nagaya, K., Masuda, K., Nakamura, T. [2012]. Nature, 486,
  240). A possible source of this event has been discussed widely,
  the most likely being an extreme solar energetic particle event. A
  new exotic hypothesis has been presented recently by Liu et al. (Liu,
  Y. [2014]. Sci. Rep., 4, 3728) who proposed that the event was caused
  by a cometary impact on Earth bringing additional 1<SUP>4</SUP> C to
  the atmosphere. Here we calculated a realistic mass and size of such
  a comet to show that it would have been huge (≈100 km across and
  10<SUP>17</SUP>-10<SUP>20</SUP> g of mass) and would have produced a
  disastrous geological/biological impact on Earth. The absence of an
  evidence for such a dramatic event makes this hypothesis invalid.

---------------------------------------------------------
Title: Energetic Particle Influence on the Earth's Atmosphere
Authors: Mironova, Irina A.; Aplin, Karen L.; Arnold, Frank;
   Bazilevskaya, Galina A.; Harrison, R. Giles; Krivolutsky, Alexei A.;
   Nicoll, Keri A.; Rozanov, Eugene V.; Turunen, Esa; Usoskin, Ilya G.
2015SSRv..194....1M    Altcode: 2015SSRv..tmp...78M
  This manuscript gives an up-to-date and comprehensive overview
  of the effects of energetic particle precipitation (EPP) onto the
  whole atmosphere, from the lower thermosphere/mesosphere through the
  stratosphere and troposphere, to the surface. The paper summarizes the
  different sources and energies of particles, principally galactic cosmic
  rays (GCRs), solar energetic particles (SEPs) and energetic electron
  precipitation (EEP). All the proposed mechanisms by which EPP can
  affect the atmosphere are discussed, including chemical changes in the
  upper atmosphere and lower thermosphere, chemistry-dynamics feedbacks,
  the global electric circuit and cloud formation. The role of energetic
  particles in Earth's atmosphere is a multi-disciplinary problem that
  requires expertise from a range of scientific backgrounds. To assist
  with this synergy, summary tables are provided, which are intended to
  evaluate the level of current knowledge of the effects of energetic
  particles on processes in the entire atmosphere.

---------------------------------------------------------
Title: The Maunder minimum (1645-1715) was indeed a grand minimum:
    A reassessment of multiple datasets
Authors: Usoskin, Ilya G.; Arlt, Rainer; Asvestari, Eleanna; Hawkins,
   Ed; Käpylä, Maarit; Kovaltsov, Gennady A.; Krivova, Natalie;
   Lockwood, Michael; Mursula, Kalevi; O'Reilly, Jezebel; Owens, Matthew;
   Scott, Chris J.; Sokoloff, Dmitry D.; Solanki, Sami K.; Soon, Willie;
   Vaquero, José M.
2015A&A...581A..95U    Altcode: 2015arXiv150705191U
  <BR /> Aims: Although the time of the Maunder minimum (1645-1715) is
  widely known as a period of extremely low solar activity, it is still
  being debated whether solar activity during that period might have
  been moderate or even higher than the current solar cycle #24. We have
  revisited all existing evidence and datasets, both direct and indirect,
  to assess the level of solar activity during the Maunder minimum. <BR />
  Methods: We discuss the East Asian naked-eye sunspot observations, the
  telescopic solar observations, the fraction of sunspot active days,
  the latitudinal extent of sunspot positions, auroral sightings at
  high latitudes, cosmogenic radionuclide data as well as solar eclipse
  observations for that period. We also consider peculiar features of
  the Sun (very strong hemispheric asymmetry of the sunspot location,
  unusual differential rotation and the lack of the K-corona) that imply
  a special mode of solar activity during the Maunder minimum. <BR />
  Results: The level of solar activity during the Maunder minimum is
  reassessed on the basis of all available datasets. <BR /> Conclusions:
  We conclude that solar activity was indeed at an exceptionally low
  level during the Maunder minimum. Although the exact level is still
  unclear, it was definitely lower than during the Dalton minimum of
  around 1800 and significantly below that of the current solar cycle
  #24. Claims of a moderate-to-high level of solar activity during the
  Maunder minimum are rejected with a high confidence level.

---------------------------------------------------------
Title: Comparative Morphology of Solar Relativistic Particle Events
Authors: Kocharov, Leon; Klassen, Andreas; Valtonen, Eino; Usoskin,
   Ilya; Ryan, James M.
2015ApJ...811L...9K    Altcode:
  Time profiles of the 0.25-10 MeV electrons and the ∼(0.1-1) GeV
  nucleon<SUP>-1</SUP> protons and helium associated with two solar
  coronal mass ejections (CMEs) are analyzed with a newly formulated
  method based on modeling of the particle transport in the interplanetary
  medium. With the modeling, we fit the observed angular distribution
  of solar particles and infer, for a particular particle instrument and
  magnetic field orientation, the time delay of the particle registration
  at 1 AU in respect to the solar source. Then, after the time offset
  removal, intensity re-normalization and background equalization, the
  time-intensity profiles of high-energy protons, helium and electrons in
  different energy channels are superposed and compared. The comparison
  reveals episodes of remarkable coincidence of different profiles, as
  well as episodes of essentially different behavior. It implies at least
  three sources of solar high-energy particles operating in a single
  event. The first, short-duration source emits electrons next to the
  flare's impulsive phase and CME liftoff. The second source gradually
  rises and continues for more than an hour, emitting electrons and
  lower energy protons, which is consistent with shock acceleration on
  open magnetic field lines extending to solar wind. An another, third
  source is the main source of relativistic ions in space. It is retarded
  in respect to the flare's impulsive phase and may be associated with
  a structure encountered by the shock within a few solar radii from
  the Sun.

---------------------------------------------------------
Title: Can we properly model the neutron monitor count rate?
Authors: Gil, Agnieszka; Usoskin, Ilya G.; Kovaltsov, Gennady A.;
   Mishev, Alexander L.; Corti, Claudio; Bindi, Veronica
2015JGRA..120.7172G    Altcode:
  Neutron monitors provide continuous measurements of secondary nucleonic
  particles produced in the atmosphere by the primary cosmic rays and form
  the main tool to study the heliospheric modulation of cosmic rays. In
  order to study cosmic rays using the world network of neutron monitor
  and needs to be able to model the neutron monitor count rate. Earlier
  it was difficult because of the poorly known yield function, which has
  been essentially revisited recently. We have presented a verification
  of the new yield function of the standard neutron monitor (NM) using
  a recently released data on the direct in situ measurements of the
  galactic cosmic rays energy spectrum during 2006-2009 (the period of
  the record high cosmic ray flux) by Payload for Antimatter Matter
  Exploration and Light-nuclei Astrophysics spaceborne spectrometer,
  and on NM latitude surveys performed during the period of 1994-2007,
  including periods of high solar activity. We found a very good agreement
  between the measured count rates of sea level NMs and the modeled
  ones in very different conditions: from low to high solar activity and
  from polar to tropical regions. This implies that the count rate of a
  sea level neutron monitor can be properly modeled in all conditions,
  using the new yield function.

---------------------------------------------------------
Title: The Maunder minimum: A reassessment from multiple dataset
Authors: Usoskin, Ilya; Arlt, Rainer; Asvestari, Eleanna; Kovaltsov,
   Gennady; Krivova, Natalie; Lockwood, Michael; Käpylä, Maarit; Owens,
   Matthew; Sokoloff, Dmitry D.; Solanki, Sami; Soon, Willie; Vaquero,
   Jose; Scott, Chris
2015IAUGA..2253036U    Altcode:
  The Maunder minimum (MM) in 1645-1715 was a period of the lowest ever
  known solar activity recorded via sunspot numbers since 1610. Since
  it is the only Grand minimum of solar activity directly observed,
  it forms a benchmark for the solar variability studies. Therefore,
  it is crucially important to assess the level and other features
  of temporal and spatial solar magnetic variability during that
  time. However, because of uncertainties related mostly to ambiguity
  of some historical sunspot observation records, the exact level of
  solar activity during the MM is somewhat unclear, leaving room for
  continuous discussions and speculations. Many of these issues have been
  addressed by Jack Eddy in his cornerstone papers of 1976 and 1983,
  but since then numerous new pieces of evidence and datasets have
  appeared, making it possible to verify the paradigm of the Maunder
  minimum with far greater certainty than before.Here we provide a full
  reassessment of the Maunder minimum using all the available datasets:
  augmented sunspot counts and drawings; revisited historical archives;
  both well-known and newly revealed records of auroral observations;
  cosmic ray variability via cosmogenic isotope records of <SUP>14</SUP>C
  in tree trunks, <SUP>10</SUP>Be in ice cores and<SUP> 44</SUP>Ti in
  fallen meteorites. We show that, while the exact level of the activity
  is not easy to determine, the Sun indeed exhibited exceptionally low
  magnetic activity during the MM, in comparison to other periods of
  moderate or decreased activity, such as the Dalton minimum (ca. 1800),
  the Gleissberg minimum (ca. 1900) and the present weak solar cycle #
  24. We show that a scenario of moderate or strong activity during the
  MM contradicts all the available datasets.Thus, we confirm, using
  all the presently available datasets of different nature, that the
  period of the Maunder minimum in 1645-1715 was indeed a Grand minimum,
  with very low solar surface magnetic activity, low intensity of the
  interplanetary magnetic field, as well as lower frequency and higher
  geographical latitude of auroral occurrence. Meanwhile some indications
  of the continuation, but at a very low level, of the 11-year solar
  cycle can be found in the data.

---------------------------------------------------------
Title: A mini neutron monitor in Central Antarctica (Dome Concordia)
Authors: Usoskin, I.; Poluianov, S.; Moraal, H.; Krüger, H.;
   Casasanta, G.; Traversi, R.; Udisty, R.
2015ICRC...34..217U    Altcode: 2015PoS...236..217U
  No abstract at ADS

---------------------------------------------------------
Title: Has the Earth been exposed to numerous supernovae within the
    last 300 kyr?
Authors: Melott, Adrian L.; Usoskin, Ilya G.; Kovaltsov, Gennady A.;
   Laird, Claude M.
2015IJAsB..14..375M    Altcode: 2014arXiv1406.5141M
  Firestone (2014) asserted evidence for numerous (23) nearby (d &lt; 300
  pc) supernovae (SNe) within the Middle and Late Pleistocene. If true,
  this would have strong implications for the irradiation of the Earth;
  at this rate, the mass extinction level events due to SNe would be
  more frequent than 100 Myr. However, there are numerous errors in the
  application of past research. The paper overestimates likely nitrate
  and <SUP>14</SUP>C production from moderately nearby SNe by about four
  orders of magnitude. Moreover, the results are based on wrongly selected
  (obsolete) nitrate and <SUP>14</SUP>C datasets. The use of correct and
  up-to-date datasets does not confirm the claimed results. The claims
  in the paper are invalid.

---------------------------------------------------------
Title: A New neutron monitor yield function computed for different
altitudes: Application for a GLE analysis
Authors: Mishev, A.; Usoskin, I.; Kovaltsov, G.
2015ICRC...34..159M    Altcode: 2015PoS...236..159M
  No abstract at ADS

---------------------------------------------------------
Title: Database of Ground Level Enhancements (GLE) of High Energy
    Solar Proton Events
Authors: Usoskin, I.; Ibragimov, A.; Shea, M. A.; Smart, D. F.
2015ICRC...34...54U    Altcode: 2015PoS...236...54U
  No abstract at ADS

---------------------------------------------------------
Title: Effective dose calculation at flight altitudes with the newly
    computed yield function
Authors: Mishev, A.; Usoskin, I.
2015ICRC...34..158M    Altcode: 2015PoS...236..158M
  No abstract at ADS

---------------------------------------------------------
Title: Use of cosmogenic radionuclides 14C and 10Be to verify
    empirically reconstructed cosmic ray modulation since 1616
Authors: Asvestari, E.; Usoskin, I.; Kovaltsov, G.
2015ICRC...34...53A    Altcode: 2015PoS...236...53A
  No abstract at ADS

---------------------------------------------------------
Title: Assessment of F200 fluence for major solar energetic particle
    events on the multi-millennial time scale
Authors: Usoskin, I.; Kovaltsov, G.; Cliver, E.; Dietrich, W. F.;
   Tylka, A.
2015ICRC...34...18U    Altcode: 2015PoS...236...18U
  No abstract at ADS

---------------------------------------------------------
Title: Flux of solar energetic particles in the distant past: Data
    from lunar rocks
Authors: Poluianov, S.; Artamonov, A.; Kovaltsov, G.; Usoskin, I.
2015ICRC...34...51P    Altcode: 2015PoS...236...51P
  No abstract at ADS

---------------------------------------------------------
Title: Resolving multiple sources of solar relativistic particles
Authors: Kocharov, L.; Klassen, A.; Usoskin, I.; Valtonen, E.
2015ICRC...34...57K    Altcode: 2015PoS...236...57K
  No abstract at ADS

---------------------------------------------------------
Title: Sensitivity of the world-wide neutron monitor network to
solar neutrons: A revised approach
Authors: Artamonov, A.; Kovaltsov, G.; Mishev, A. Alexander;
   Usoskin, I.
2015ICRC...34..163A    Altcode: 2015PoS...236..163A
  No abstract at ADS

---------------------------------------------------------
Title: Force-field parameterization of the galactic cosmic ray
spectrum: Validation for Forbush decreases
Authors: Usoskin, I. G.; Kovaltsov, G. A.; Adriani, O.; Barbarino,
   G. C.; Bazilevskaya, G. A.; Bellotti, R.; Boezio, M.; Bogomolov,
   E. A.; Bongi, M.; Bonvicini, V.; Bottai, S.; Bruno, A.; Cafagna, F.;
   Campana, D.; Carbone, R.; Carlson, P.; Casolino, M.; Castellini, G.;
   De Donato, C.; De Santis, C.; De Simone, N.; Di Felice, V.; Formato,
   V.; Galper, A. M.; Karelin, A. V.; Koldashov, S. V.; Koldobskiy, S.;
   Krutkov, S. Y.; Kvashnin, A. N.; Leonov, A.; Malakhov, V.; Marcelli,
   L.; Martucci, M.; Mayorov, A. G.; Menn, W.; Mergé, M.; Mikhailov,
   V. V.; Mocchiutti, E.; Monaco, A.; Mori, N.; Munini, R.; Osteria,
   G.; Palma, F.; Panico, B.; Papini, P.; Pearce, M.; Picozza, P.;
   Pizzolotto, C.; Ricci, M.; Ricciarini, S. B.; Rossetto, L.; Sarkar,
   R.; Scotti, V.; Simon, M.; Sparvoli, R.; Spillantini, P.; Stozhkov,
   Y. I.; Vacchi, A.; Vannuccini, E.; Vasilyev, G. I.; Voronov, S. A.;
   Yurkin, Y. T.; Zampa, G.; Zampa, N.; Zverev, V. G.
2015AdSpR..55.2940U    Altcode:
  A useful parametrization of the energy spectrum of galactic cosmic rays
  (GCR) near Earth is offered by the so-called force-field model which
  describes the shape of the entire spectrum with a single parameter,
  the modulation potential. While the usefulness of the force-field
  approximation has been confirmed for regular periods of solar
  modulation, it was not tested explicitly for disturbed periods, when
  GCR are locally modulated by strong interplanetary transients. Here
  we use direct measurements of protons and α -particles performed by
  the PAMELA space-borne instrument during December 2006, including a
  major Forbush decrease, in order to directly test the validity of the
  force-field parameterization. We conclude that (1) The force-field
  parametrization works very well in describing the energy spectra of
  protons and α -particles directly measured by PAMELA outside the Earths
  atmosphere; (2) The energy spectrum of GCR can be well parameterized
  by the force-field model also during a strong Forbush decrease; (3)
  The estimate of the GCR modulation parameter, obtained using data from
  the world-wide neutron monitor network, is in good agreement with the
  spectra directly measured by PAMELA during the studied interval. This
  result is obtained on the basis of a single event analysis, more events
  need to be analyzed.

---------------------------------------------------------
Title: Long-term variation in the Sun's activity caused by magnetic
    Rossby waves in the tachocline
Authors: Zaqarashvili, Teimuraz V.; Oliver, Ramon; Hanslmeier, Arnold;
   Carbonell, Marc; Ballester, Jose Luis; Gachechiladze, Tamar; Usoskin,
   Ilya G.
2015ApJ...805L..14Z    Altcode: 2015arXiv150502652Z
  Long-term records of sunspot number and concentrations of cosmogenic
  radionuclides (10Be and 14C) on the Earth reveal the variation of
  the Sun's magnetic activity over hundreds and thousands of years. We
  identify several clear periods in sunspot, 10Be, and 14C data as
  1000, 500, 350, 200, and 100 years. We found that the periods of the
  first five spherical harmonics of the slow magnetic Rossby mode in
  the presence of a steady toroidal magnetic field of 1200-1300 G in
  the lower tachocline are in perfect agreement with the timescales of
  observed variations. The steady toroidal magnetic field can be generated
  in the lower tachocline either due to the steady dynamo magnetic field
  for low magnetic diffusivity or due to the action of the latitudinal
  differential rotation on the weak poloidal primordial magnetic field,
  which penetrates from the radiative interior. The slow magnetic Rossby
  waves lead to variations of the steady toroidal magnetic field in
  the lower tachocline, which modulate the dynamo magnetic field and
  consequently the solar cycle strength. This result constitutes a key
  point for long-term prediction of the cycle strength. According to our
  model, the next deep minimum in solar activity is expected during the
  first half of this century.

---------------------------------------------------------
Title: Numerical model for computation of effective and ambient
    dose equivalent at flight altitudes. Application for dose assessment
    during GLEs
Authors: Mishev, Alexander; Usoskin, Ilya
2015JSWSC...5A..10M    Altcode:
  A numerical model for assessment of the effective dose and ambient dose
  equivalent produced by secondary cosmic ray particles of galactic and
  solar origin at commercial aircraft altitudes is presented. The model
  represents a full chain analysis based on ground-based measurements
  of cosmic rays, from particle spectral and angular characteristics to
  dose estimation. The model is based on newly numerically computed
  yield functions and realistic propagation of cosmic ray in the
  Earth magnetosphere. The yield functions are computed using a
  straightforward full Monte Carlo simulation of the atmospheric
  cascade induced by primary protons and α-particles and subsequent
  conversion of secondary particle fluence (neutrons, protons, gammas,
  electrons, positrons, muons and charged pions) to effective dose or
  the ambient dose equivalent. The ambient dose equivalent is compared
  with reference data at various conditions such as rigidity cut-off
  and level of solar activity. The method is applied for computation
  of the effective dose rate at flight altitude during the ground level
  enhancement of 13 December 2006. The solar proton spectra are derived
  using neutron monitor data. The computation of the effective dose
  rate during the event explicitly considers the derived anisotropy
  i.e. the pitch angle distribution as well as the propagation of the
  solar protons in the magnetosphere of the Earth.

---------------------------------------------------------
Title: Level and length of cyclic solar activity during the Maunder
    minimum as deduced from the active-day statistics
Authors: Vaquero, J. M.; Kovaltsov, G. A.; Usoskin, I. G.; Carrasco,
   V. M. S.; Gallego, M. C.
2015A&A...577A..71V    Altcode: 2015arXiv150307664V
  <BR /> Aims: The Maunder minimum (MM) of greatly reduced solar activity
  took place in 1645-1715, but the exact level of sunspot activity is
  uncertain because it is based, to a large extent, on historical generic
  statements of the absence of spots on the Sun. Using a conservative
  approach, we aim to assess the level and length of solar cycle during
  the MM on the basis of direct historical records by astronomers of that
  time. <BR /> Methods: A database of the active and inactive days (days
  with and without recorded sunspots on the solar disc) is constructed
  for three models of different levels of conservatism (loose, optimum,
  and strict models) regarding generic no-spot records. We used the
  active day fraction to estimate the group sunspot number during the
  MM. <BR /> Results: A clear cyclic variability is found throughout
  the MM with peaks at around 1655-1657, 1675, 1684, 1705, and possibly
  1666, with the active-day fraction not exceeding 0.2, 0.3, or 0.4
  during the core MM, for the three models. Estimated sunspot numbers
  are found to be very low in accordance with a grand minimum of solar
  activity. <BR /> Conclusions: For the core MM (1650-1700), we have
  found that (1) A large portion of no-spot records, which correspond to
  the solar meridian observations, may be unreliable in the conventional
  database. (2) The active-day fraction remained low (below 0.3-0.4)
  throughout the MM, indicating the low level of sunspot activity. (3)
  The solar cycle appears clearly during the core MM. (4) The length
  of the solar cycle during the core MM appears for 9 ± 1 years, but
  this is uncertain. (5) The magnitude of the sunspot cycle during MM
  is assessed to be below 5-10 in sunspot numbers. A hypothesis of the
  high solar cycles during the MM is not confirmed.

---------------------------------------------------------
Title: Inferring the Structure of the Solar Corona and Inner
    Heliosphere During the Maunder Minimum Using Global Thermodynamic
    Magnetohydrodynamic Simulations
Authors: Riley, Pete; Lionello, Roberto; Linker, Jon A.; Cliver,
   Ed; Balogh, Andre; Beer, Jürg; Charbonneau, Paul; Crooker, Nancy;
   DeRosa, Marc; Lockwood, Mike; Owens, Matt; McCracken, Ken; Usoskin,
   Ilya; Koutchmy, S.
2015ApJ...802..105R    Altcode:
  Observations of the Sun’s corona during the space era have led to
  a picture of relatively constant, but cyclically varying solar output
  and structure. Longer-term, more indirect measurements, such as from
  <SUP>10</SUP>Be, coupled by other albeit less reliable contemporaneous
  reports, however, suggest periods of significant departure from this
  standard. The Maunder Minimum was one such epoch where: (1) sunspots
  effectively disappeared for long intervals during a 70 yr period; (2)
  eclipse observations suggested the distinct lack of a visible K-corona
  but possible appearance of the F-corona; (3) reports of aurora were
  notably reduced; and (4) cosmic ray intensities at Earth were inferred
  to be substantially higher. Using a global thermodynamic MHD model,
  we have constructed a range of possible coronal configurations for the
  Maunder Minimum period and compared their predictions with these limited
  observational constraints. We conclude that the most likely state of the
  corona during—at least—the later portion of the Maunder Minimum was
  not merely that of the 2008/2009 solar minimum, as has been suggested
  recently, but rather a state devoid of any large-scale structure,
  driven by a photospheric field composed of only ephemeral regions,
  and likely substantially reduced in strength. Moreover, we suggest
  that the Sun evolved from a 2008/2009-like configuration at the start
  of the Maunder Minimum toward an ephemeral-only configuration by the
  end of it, supporting a prediction that we may be on the cusp of a
  new grand solar minimum.

---------------------------------------------------------
Title: The impact of geomagnetic spikes on the production rates
    of cosmogenic <SUP>14</SUP>C and <SUP>10</SUP>Be in the Earth's
    atmosphere
Authors: Fournier, Alexandre; Gallet, Yves; Usoskin, Ilya; Livermore,
   Philip W.; Kovaltsov, Gennady A.
2015GeoRL..42.2759F    Altcode:
  We seek corroborative evidence of the geomagnetic spikes detected
  in the Near East ca. 980 BC and 890 BC in the records of the past
  production rates of the cosmogenic nuclides <SUP>14</SUP>C and
  <SUP>10</SUP>Be. Our forward modeling strategy rests on global,
  time-dependent, geomagnetic spike field models feeding state-of-the-art
  models of cosmogenic nuclide production. We find that spike models with
  an energy budget in line with presently inferred large-scale flow at
  Earth's core surface fail to produce a visible imprint in the nuclide
  record. Spike models able to reproduce the intensity changes reported
  in the Near East require an unaccountably high-magnitude core flow,
  yet their computed impact on cosmogenic isotope production rates
  remains ambiguous. No simple and unequivocal agreement is obtained
  between the observed and modeled nuclide records at the epochs of
  interest. This indicates that cosmogenic nuclides cannot immediately
  be used to confirm the occurrence of these two geomagnetic spikes.

---------------------------------------------------------
Title: Solar surface rotation: N-S asymmetry and recent speed-up
Authors: Zhang, L.; Mursula, K.; Usoskin, I.
2015A&A...575L...2Z    Altcode: 2015arXiv150102698Z
  Context. The relation between solar surface rotation and sunspot
  activity is still not fully resolved. The sunspot activity has
  been significantly reduced in solar cycle 24, and several solar
  activity indices and flux measurements experienced unprecedentedly
  low levels during the last solar minimum. <BR /> Aims: We aim to
  reveal the momentary variation of solar surface rotation, especially
  during the recent years of reduced solar activity. <BR /> Methods:
  We used a dynamic, differentially rotating reference system to
  determine the best-fit annual values of the differential rotation
  parameters of active longitudes of solar X-ray flares and sunspots
  in 1977-2012. <BR /> Results: The evolution of the rotation of solar
  active longitudes obtained from observing X-ray flares and sunspots is
  very similar. Both hemispheres have increased their rotation rate since
  the late 1990s, with the southern hemisphere rotating slightly faster
  than the north. In the 1980s, rotation in the northern hemisphere
  was considerably faster, but it experienced a major decrease in
  the early 1990s. On the other hand, little change was found in the
  rotation of the southern hemisphere during these decades. This led
  to a positive asymmetry in the north-south rotation rate in the early
  part of the time interval studied. <BR /> Conclusions: The rotation of
  both hemispheres has been speeding up at roughly the same rate since
  the late 1990s, with the southern hemisphere rotating slightly faster
  than the northern hemisphere. This period coincides with the start of
  a significant weakening of the solar activity, as observed in sunspots
  and several other solar, interplanetary, and geomagnetic parameters.

---------------------------------------------------------
Title: An Unusual Pattern of Cosmic-Ray Modulation During Solar
    Cycles 23 and 24
Authors: Pacini, A. A.; Usoskin, I. G.
2015SoPh..290..943P    Altcode: 2014SoPh..tmp..195P
  By means of an analysis of data from eight neutron monitor (NM)
  stations with different geomagnetic cutoff rigidities, we found an
  unusual latitudinal effect observed in the cosmic-ray (CR) modulation
  during the last solar cycles. Since the beginning of the ground-based
  cosmic-ray monitoring, it is known that the solar-cycle modulation
  is more evident in data from high latitude than from the medium
  and low latitudes, showing an expected geomagnetic cutoff rigidity
  effect. However, a more detailed look shows a new latitudinal effect
  in cycle 24: while the magnitude of the solar modulation in the
  low-latitude data remains the same for the last three solar minima,
  the last solar minimum caused a more intense peak in the polar NM
  data than in the previous cycles. After correcting the data for
  the geomagnetic changes of the period, we found an anomalous solar
  modulation in the last cycle. This suggests a weaker heliospheric
  modulation at low-energy particles (responsible for the NM counting
  in polar sites) now than in the previous cycles, while there is no
  significant difference of the modulation for the more energetic part
  of the CR spectrum. Our result can be associated with changes of the
  solar wind turbulence, which would corroborate some recent studies
  about the last solar minimum phase, and indicates that this new solar
  modulation feature is still present in the current solar maximum stage.

---------------------------------------------------------
Title: Solar Cycle in the Heliosphere and Cosmic Rays
Authors: Bazilevskaya, Galina A.; Cliver, Edward W.; Kovaltsov,
   Gennady A.; Ling, Alan G.; Shea, M. A.; Smart, D. F.; Usoskin, Ilya G.
2015sac..book..409B    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: Computation of dose rate at flight altitudes during ground
    level enhancements no. 69, 70 and 71
Authors: Mishev, A. L.; Adibpour, F.; Usoskin, I. G.; Felsberger, E.
2015AdSpR..55..354M    Altcode:
  A new numerical model of estimating and monitoring the exposure
  of personnel due to secondary cosmic radiation onboard aircraft,
  in accordance with radiation safety standards as well as European
  and national regulations, has been developed. The model aims to
  calculate the effective dose at flight altitude (39,000 ft) due to
  secondary cosmic radiation of galactic and solar origin. In addition,
  the model allows the estimation of ambient dose equivalent at typical
  commercial airline altitudes in order to provide comparison with
  reference data. The basics, structure and function of the model are
  described. The model is based on a straightforward full Monte Carlo
  simulation of the cosmic ray induced atmospheric cascade. The cascade
  simulation is performed with the PLANETOCOSMICS code. The flux of
  secondary particles, namely neutrons, protons, gammas, electrons,
  positrons, muons and charged pions is calculated. A subsequent
  conversion of the particle fluence into the effective dose or ambient
  dose equivalent is performed as well as a comparison with reference
  data. An application of the model is demonstrated, using a computation
  of the effective dose rate at flight altitude during the ground level
  enhancements of 20 January 2005, 13 December 2006 and 17 May 2012.

---------------------------------------------------------
Title: Solar Cycle in the Heliosphere and Cosmic Rays
Authors: Bazilevskaya, Galina A.; Cliver, Edward W.; Kovaltsov,
   Gennady A.; Ling, Alan G.; Shea, M. A.; Smart, D. F.; Usoskin, Ilya G.
2014SSRv..186..409B    Altcode: 2014SSRv..tmp...44B
  Manifestations of the 11-year solar cycle and longer time-scale
  variability in the heliosphere and cosmic rays are considered. We
  briefly review the cyclic variability of such heliospheric parameters
  as solar wind speed and density and heliospheric magnetic field, open
  magnetic flux and latitude variations of the heliospheric current
  sheet. It is discussed whether the local in-situ observation near
  Earth can represent the global 3D heliospheric pattern. Variability
  of cosmic rays near Earth provides an indirect useful tool to study
  the heliosphere. We discuss details of the heliospheric modulation
  of galactic cosmic rays, as recorded at and near Earth, and their
  relation to the heliospheric conditions in the outer heliosphere. On
  the other hand, solar energetic particles can serve as probes for
  explosive phenomena on the Sun and conditions in the corona and inner
  heliosphere. The occurrence of major solar proton events depicts an
  overall tendency to follow the solar cycle but individual events may
  appear at different phases of the solar cycle, as defined by various
  factors. The solar cycle in the heliosphere and cosmic rays depicts
  a complex pattern which includes different processes and cannot be
  described by a simple correlation with sunspot number.

---------------------------------------------------------
Title: Cosmogenic production and climate contributions to nitrate
    record in the TALDICE Antarctic ice core
Authors: Poluianov, S.; Traversi, R.; Usoskin, I.
2014JASTP.121...50P    Altcode:
  This paper presents the results of a comparative wavelet coherence
  analysis of a multimillennial nitrate record with a number of climatic
  and solar activity proxies. Distinguishing between these factors
  is important in the view of a possibility of nitrate deposited in a
  polar region to represent galactic cosmic ray flux and, consequently,
  solar activity. We used the data from the TALDICE drilling project
  (Talos Dome, Antarctica), which covers the age range 12,000-700
  BP (years before present, i.e. before 1950) and includes records
  of nitrate as well as climatic proxies, such as Na<SUP>+</SUP>,
  Ca<SUP>2+</SUP>, MSA (methanesulphonic acid), δ<SUP>18</SUP>O,
  SO<SUB>4</SUB><SUP>2-</SUP>. The solar activity series is represented
  by reconstructions of the heliospheric modulation parameter from the
  <SUP>14</SUP>C and <SUP>10</SUP>Be data. We found (1) a confirmation of
  multimillennial relation between nitrate and galactic cosmic ray flux;
  (2) no clear signature of long-term variations of nitrate transport
  from lower latitudes. We suggest that variations in the nitrate record
  in the time scale of hundreds-thousands years are most likely caused
  by local production, deposition and post-deposition processes.

---------------------------------------------------------
Title: Cosmogenic Isotope Variability During the Maunder Minimum:
    Normal 11-year Cycles Are Expected
Authors: Poluianov, S. V.; Usoskin, I. G.; Kovaltsov, G. A.
2014SoPh..289.4701P    Altcode: 2014SoPh..tmp..119P
  The amplitude of the 11-year cycle measured in the cosmogenic isotope
  <SUP>10</SUP>Be during the Maunder Minimum is comparable to that
  during the recent epoch of high solar activity. Because of the virtual
  absence of the cyclic variability of sunspot activity during the Maunder
  Minimum this seemingly contradicts an intuitive expectation that lower
  activity would result in smaller solar-cycle variations in cosmogenic
  radio-isotope data, or in none, leading to confusing and misleading
  conclusions. It is shown here that large 11-year solar cycles in
  cosmogenic data observed during periods of suppressed sunspot activity
  do not necessarily imply strong heliospheric fields. Normal-amplitude
  cycles in the cosmogenic radio-isotopes observed during the Maunder
  Minimum are consistent with theoretical expectations because of the
  nonlinear relation between solar activity and isotope production. Thus,
  cosmogenic-isotope data provide a good tool to study solar-cycle
  variability even during grand minima of solar activity.

---------------------------------------------------------
Title: Fluence Ordering of Solar Energetic Proton Events Using
    Cosmogenic Radionuclide Data
Authors: Kovaltsov, G. A.; Usoskin, I. G.; Cliver, E. W.; Dietrich,
   W. F.; Tylka, A. J.
2014SoPh..289.4691K    Altcode: 2014SoPh..tmp..129K
  While data on the cosmogenic isotopes <SUP>14</SUP>C and <SUP>10</SUP>Be
  made it possible to evaluate extreme solar proton events (SPEs) in
  the past, their relation to standard parameters quantifying the SPE
  strengths, viz. the integrated fluence of protons with energy above
  30 MeV, F<SUB>30</SUB>, is ambiguous and strongly depends on the
  assumed shape of the energy spectrum. Here we propose a new index,
  the integral fluence of an SPE above 200 MeV, F<SUB>200</SUB>, which
  is related to the production of the cosmogenic isotopes <SUP>14</SUP>C
  and <SUP>10</SUP>Be in the Earth atmosphere, independently of the
  assumptions on the energy spectrum of the event. The F<SUB>200</SUB>
  fluence is reconstructed from past cosmogenic isotope data, which
  provides an assessment of the occurrence probability density function
  for extreme SPEs. In particular, we evaluate that extreme SPEs with
  F<SUB>200</SUB>&gt;10<SUP>10</SUP> cm<SUP>−2</SUP> occur no more
  frequently than once per 10 - 15 kyr.

---------------------------------------------------------
Title: Release timescales of solar energetic particles in the
    low corona
Authors: Agueda, N.; Klein, K. -L.; Vilmer, N.; Rodríguez-Gasén,
   R.; Malandraki, O. E.; Papaioannou, A.; Subirà, M.; Sanahuja, B.;
   Valtonen, E.; Dröge, W.; Nindos, A.; Heber, B.; Braune, S.; Usoskin,
   I. G.; Heynderickx, D.; Talew, E.; Vainio, R.
2014A&A...570A...5A    Altcode:
  <BR /> Aims: We present a systematic study of the timing and duration of
  the release processes of near-relativistic (NR; &gt;50 keV) electrons
  in the low corona. <BR /> Methods: We analyze seven well-observed
  events using in situ measurements by both the ACE and Wind spacecraft
  and context electromagnetic observations in soft X-rays, radio, hard
  X-rays and white light. We make use of velocity dispersion analysis to
  estimate the release time of the first arriving electrons and compare
  with the results obtained by using a simulation-based approach,
  taking interplanetary transport effects into account to unfold the
  NR electron release time history from in situ measurements. <BR />
  Results: The NR electrons observed in interplanetary space appear
  to be released during either short (&lt;30 min) or long (&gt;2
  h) periods. The observation of NR electron events showing beamed
  pitch-angle distributions (PADs) during several hours is the clearest
  observational signature of sustained release in the corona. On the
  other hand, the in situ observation of PADs isotropizing in less
  than a couple of hours is a clear signature of a prompt release of
  electrons in the low corona. Short release episodes appear to originate
  in solar flares, in coincidence with the timing of the observed type
  III radio bursts. Magnetic connectivity plays an important role. Only
  type III radio bursts reaching the local plasma line measured at 1 AU
  are found to be related with an associated release episode in the low
  corona. Other type III bursts may also have a release of NR electrons
  associated with them, but these electrons do not reach L1. Long
  release episodes appear associated with signatures of long acceleration
  processes in the low corona (long decay of the soft X-ray emission,
  type IV radio bursts, and time-extended microwave emission). Type II
  radio bursts are reported for most of the events and do not provide
  a clear discrimination between short and long release timescales.

---------------------------------------------------------
Title: A review of Holocene solar-linked climatic variation
on centennial to millennial timescales: Physical processes,
    interpretative frameworks and a new multiple cross-wavelet transform
    algorithm
Authors: Soon, Willie; Velasco Herrera, Victor M.; Selvaraj, Kandasamy;
   Traversi, Rita; Usoskin, Ilya; Chen, Chen-Tung Arthur; Lou, Jiann-Yuh;
   Kao, Shuh-Ji; Carter, Robert M.; Pipin, Valery; Severi, Mirko;
   Becagli, Silvia
2014ESRv..134....1S    Altcode:
  We report on the existence and nature of Holocene solar and climatic
  variations on centennial to millennial timescales. We introduce a new
  solar activity proxy, based on nitrate (NO<SUB>3</SUB><SUP>-</SUP>)
  concentration from the Talos Dome ice core, East Antarctica. We also
  use a new algorithm for computing multiple-cross wavelet spectra in
  time-frequency space that is generalized for multiple time series
  (beyond two). Our results provide a new interpretive framework for
  relating Holocene solar activity variations on centennial to millennial
  timescales to co-varying climate proxies drawn from a widespread
  area around the globe. Climatic proxies used represent variation in
  the North Atlantic Ocean, Western Pacific Warm Pool, Southern Ocean
  and the East Asian monsoon regions. Our wavelet analysis identifies
  fundamental solar modes at 2300-yr (Hallstattzeit), 1000-yr (Eddy),
  and 500-yr (unnamed) periodicities, leaves open the possibility
  that the 1500-1800-yr cycle may either be fundamental or derived,
  and identifies intermediary derived cycles at 700-yr and 300-yr that
  may mark rectified responses of the Atlantic thermohaline circulation
  to external solar modulation and pacing. Dating uncertainties suggest
  that the 1500-yr and 1800-yr cycles described in the literature may
  represent either the same or two separate cycles, but in either case,
  and irrespective too of whether it is a fundamental or derived mode in
  the sense of Dima and Lohmann (2009), the 1500-1800-yr periodicity is
  widely represented in a large number of paleoclimate proxy records. It
  is obviously premature to reject possible links between changing solar
  activity at these multiple scales and the variations that are commonly
  observed in paleoclimatic records.

---------------------------------------------------------
Title: Critical Analysis of a Hypothesis of the Planetary Tidal
    Influence on Solar Activity
Authors: Poluianov, S.; Usoskin, I.
2014SoPh..289.2333P    Altcode: 2014arXiv1401.3547P; 2014SoPh..tmp....5P
  The present work is a critical revision of the hypothesis of the
  planetary tidal influence on solar activity published by Abreu et
  al. (Astron. Astrophys.548, A88, 2012; called A12 here). A12 describes
  the hypothesis that planets can have an impact on the solar tachocline
  and therefore on solar activity. We checked the procedure and results
  of A12, namely the algorithm of planetary tidal torque calculation
  and the wavelet coherence between torque and heliospheric modulation
  potential. We found that the claimed peaks in long-period range of
  the torque spectrum are artefacts caused by the calculation algorithm
  (viz. aliasing effect). Also the statistical significance of the
  results of the wavelet coherence is found to be overestimated by an
  incorrect choice of the background assumption of red noise. Using a
  more conservative non-parametric random-phase method, we found that
  the long-period coherence between planetary torque and heliospheric
  modulation potential becomes insignificant. Thus we conclude that the
  considered hypothesis of planetary tidal influence on solar activity
  is not based on a solid ground.

---------------------------------------------------------
Title: Transmission and Emission of Solar Energetic Particles in
    Semi-transparent Shocks
Authors: Kocharov, Leon; Laitinen, Timo; Usoskin, Ilya; Vainio, Rami
2014ApJ...787L..21K    Altcode:
  While major solar energetic particle (SEP) events are associated with
  coronal mass ejection (CME)-driven shocks in solar wind, accurate SEP
  measurements reveal that more than one component of energetic ions
  exist in the beginning of the events. Solar electromagnetic emissions,
  including nuclear gamma-rays, suggest that high-energy ions could also
  be accelerated by coronal shocks, and some of those particles could
  contribute to SEPs in interplanetary space. However, the CME-driven
  shock in solar wind is thought to shield any particle source beneath the
  shock because of the strong scattering required for the diffusive shock
  acceleration. In this Letter, we consider a shock model that allows
  energetic particles from the possible behind-shock source to appear in
  front of the shock simultaneously with SEPs accelerated by the shock
  itself. We model the energetic particle transport in directions parallel
  and perpendicular to the magnetic field in a spherical shock expanding
  through the highly turbulent magnetic sector with an embedded quiet
  magnetic tube, which makes the shock semi-transparent for energetic
  particles. The model energy spectra and time profiles of energetic
  ions escaping far upstream of the shock are similar to the profiles
  observed during the first hour of some gradual SEP events.

---------------------------------------------------------
Title: Evidence for distinct modes of solar activity
Authors: Usoskin, I. G.; Hulot, G.; Gallet, Y.; Roth, R.; Licht, A.;
   Joos, F.; Kovaltsov, G. A.; Thébault, E.; Khokhlov, A.
2014A&A...562L..10U    Altcode: 2014arXiv1402.4720U
  <BR /> Aims: The Sun shows strong variability in its magnetic activity,
  from Grand minima to Grand maxima, but the nature of the variability is
  not fully understood, mostly because of the insufficient length of the
  directly observed solar activity records and of uncertainties related
  to long-term reconstructions. Here we present a new adjustment-free
  reconstruction of solar activity over three millennia and study its
  different modes. <BR /> Methods: We present a new adjustment-free,
  physical reconstruction of solar activity over the past three millennia,
  using the latest verified carbon cycle, <SUP>14</SUP>C production,
  and archeomagnetic field models. This great improvement allowed us to
  study different modes of solar activity at an unprecedented level of
  details. <BR /> Results: The distribution of solar activity is clearly
  bi-modal, implying the existence of distinct modes of activity. The
  main regular activity mode corresponds to moderate activity that varies
  in a relatively narrow band between sunspot numbers 20 and 67. The
  existence of a separate Grand minimum mode with reduced solar activity,
  which cannot be explained by random fluctuations of the regular mode,
  is confirmed at a high confidence level. The possible existence of a
  separate Grand maximum mode is also suggested, but the statistics is
  too low to reach a confident conclusion. <BR /> Conclusions: The Sun
  is shown to operate in distinct modes - a main general mode, a Grand
  minimum mode corresponding to an inactive Sun, and a possible Grand
  maximum mode corresponding to an unusually active Sun. These results
  provide important constraints for both dynamo models of Sun-like stars
  and investigations of possible solar influence on Earth's climate. <P
  />Data are only available at the CDS via anonymous ftp to <A
  href="http://cdsarc.u-strasbg.fr">http://cdsarc.u-strasbg.fr</A>
  (ftp://130.79.128.5) or via <A
  href="http://cdsarc.u-strasbg.fr/viz-bin/qcat?J/A+A/562/L10">http://cdsarc.u-strasbg.fr/viz-bin/qcat?J/A+A/562/L10</A>

---------------------------------------------------------
Title: VizieR Online Data Catalog: Solar activity reconstructed for
    3 millennia (Usoskin+, 2014)
Authors: Usoskin, I. G.; Hulot, G.; Gallet, Y.; Roth, R.; Licht, A.;
   Joos, F.; Kovaltsov, G. A.; Thebault, E.; Khokhlov, A.
2014yCat..35629010U    Altcode:
  Indices of solar activity reconstructed from <SUP>14</SUP>C using the
  m used in the paper. Two indices are provided - the sunspot number
  and the cosmic ray modulation potential, both with the 95% confidence
  intervals. The data sets are provided with decadal resolution, thus
  the individual solar cycles are not resolved. <P />(2 data files).

---------------------------------------------------------
Title: Analysis of the ground level enhancement on 17 May 2012 using
    data from the global neutron monitor network
Authors: Mishev, A. L.; Kocharov, L. G.; Usoskin, I. G.
2014JGRA..119..670M    Altcode:
  We have analyzed the data of the world neutron monitor network for the
  first ground level enhancement of solar cycle 24, the ground level
  enhancement (GLE) on 17 May 2012. A newly computed neutron monitor
  yield function and an inverse method are applied to estimate the energy
  spectrum, anisotropy axis direction, and pitch angle distribution of
  the high-energy solar particles in interplanetary space. The method
  includes the determination of the asymptotic viewing cones of neutron
  monitor stations through computations of trajectories of cosmic rays
  in a model magnetosphere. The cosmic ray particle trajectories are
  determined with the GEANT-based MAGNETOCOSMICS code using Tsyganenko
  1989 and International Geomagnetic Reference Field models. Subsequent
  calculation of the neutron monitor responses with the model function
  is carried out, that represents an initial guess of the inverse
  problem. Derivation of the solar energetic particle characteristics
  is fulfilled by fitting the data of the global neutron monitor network
  using the Levenberg-Marquardt method over the nine-dimensional parameter
  space. The pitch angle distribution and rigidity spectrum of high-energy
  protons are obtained as function of time in the course of the GLE. The
  angular distribution appears quite complicated. It comprises a focused
  beam along the interplanetary magnetic field line from the Sun and a
  loss-cone feature around the opposite direction, possibly indicative
  of the particle transport in interplanetary magnetic field structures
  associated with previous coronal mass ejections.

---------------------------------------------------------
Title: The world-wide neutron monitor network as a toll to detect
solar neutrons: a revisited approach
Authors: Mishev, Alexander; Usoskin, Ilya; Artamonov, Anton; Kovaltsov,
   Gennady A.
2014cosp...40E2127M    Altcode:
  When energetic protons are accelerated in solar flares, they may
  locally produce secondary neutrons, which can then escape and reach
  the Earth. Features of these neutrons carry direct information on the
  conditions at the flare site. The main tool to measure solar neutrons on
  ground was the world neutron monitor (NM) network, later complemented by
  a network of dedicated solar neutron telescopes. Although measurements
  of solar neutrons has long history, detailed computation of the specific
  yield function of the NM to solar neutrons was somewhat uncertain. Here
  we revise the computation of the NM yield function for solar neutrons,
  based on new Monte-Carlo simulation of the neutron-induced atmospheric
  cascade, and reassess the sensitivity of the world NM network to solar
  neutron events.

---------------------------------------------------------
Title: On the validity of force-field approximation for galactic
    cosmic ray spectrum during Forbush decreases using PAMELA data
Authors: Usoskin, Ilya; Kovaltsov, Gennady A.
2014cosp...40E3446U    Altcode:
  Precise measurements of galactic cosmic rays (GCR) are performed
  nowadays by space-based instruments, but they are limited in time
  from short-time campaigns to a half-solar cycle long PAMELA and a
  few-year long AMS-2 space missions. On the other hand, simple model
  approximations for the GCR spectrum, modulated by solar magnetic
  activity, are used in many practical applications. The most common is
  the so-called force-field model, which is often used in such fields as
  atmospheric physics, long-term solar studies, etc. The GCR spectrum
  is approximated by a prescribed form with the single parameter,
  the modulation potential, whose value can be determined from the
  ground-based neutron monitor data. In this way, GCR spectrum can
  be modelled for the last about 60 years. While the validity of the
  force-field model has been confirmed for regular periods of solar
  modulation, it was not known if it is still valid during Forbush
  decreases, when GCR are locally modulated by strong interplanetary
  transients. Accordingly, this led to essential uncertainty in applying
  this approach. The recent direct data from PAMELA instrument cover
  a major Forbush decrease in December 2006, which makes it possible
  to directly test the validity of the force-field model. We made a
  detailed study, by fitting the observed daily GCR spectra as measured
  by PAMELA during the Forbush decrease, separately for protons and
  alpha-particles, and comparing them with the modulation potential values
  assessed from the neutron monitor data. We conclude that even during a
  strong Forbush decrease, the force-field model based on neutron monitor
  data reasonably approximate the actual GCR spectrum at the daily time
  scale. This validate the use of the force-field approximation even
  during periods of greatly disturbed heliospheric conditions.

---------------------------------------------------------
Title: New improved reconstruction of solar activity over 3 millennia:
    Evidence for distinct solar dynamo modes
Authors: Usoskin, Ilya; Kovaltsov, Gennady; Hulot, Gauthier.; Gallet,
   Yves; Roth, Raphael; Licht, Alexis; Joos, Fortunat; Th, E.; Khokhlov,
   A.; Kovaltsov, Gennady A.
2014cosp...40E3445U    Altcode:
  The solar magnetic dynamo can operate in distinct modes - a main general
  mode, a Grand minimum mode corresponding to an inactive Sun, and a
  possible Grand maximum mode corresponding to an unusually active Sun,
  as e.g., observed recently. The reality of such mode separation has
  recently been the subject of much debate, with different theoretical
  speculations discussed. Here we present the first adjustment-free
  physical reconstruction of solar activity over the past three
  millennia, using the latest carbon cycle, (14) C production and
  archeomagnetic field models. This new improved reconstruction shows
  that the solar dynamo process indeed switches between different modes,
  either corresponding to different regimes of the dynamo or to changes
  in the driving parameters. These results provide important constraints
  for both dynamo models of Sun-like stars and investigations of possible
  solar influence on Earth’s climate.

---------------------------------------------------------
Title: The unusual solar minimum in relation to the Sun's history
Authors: Usoskin, Ilya
2014cosp...40E3443U    Altcode:
  The recent solar minimum of 2008-2010 was quite unusual for the space
  era with the very quiet solar and heliospheric conditions. On the
  other hand, such low activity minima are typical in the centennial
  and millennial history of the Sun. Here, a review is presented of the
  long-term evolution of solar/heliospheric activity as reconstructed
  from direct observations and indirect proxy. A special emphasis is
  given to the occurrence of Grand minima and maxima on the long-term
  scale, and their relation to the heliospheric modulation of cosmic
  rays. It is shown that, after the recent Grand maximum of activity,
  the Sun is now in the normal mode of activity.

---------------------------------------------------------
Title: Cosmogenic production vs. climate for the nitrate record in
    the TALDICE Antarctic ice core
Authors: Poluianov, Stepan; Usoskin, Ilya; Traversi, Rita
2014cosp...40E2583P    Altcode:
  Reconstructions of solar activity on the multimillennial scale are
  based usually on records of two cosmogenic isotopes (14) C and (10) Be,
  measured in tree trunks or ice cores. In addition to these well-known
  proxies, a chemical tracer was recently proposed (Traversi et al.,
  2012), viz. nitrate, measured in an Antarctic ice sheet with moderate
  snow deposition rate. Tropo-stratospheric production of nitrate by
  cosmic rays is significant in polar regions because of the effect
  of energetic galactic cosmic rays. However, some climatic factors
  can influence a nitrate record there. Since the strongest source of
  nitrate is located at low and middle latitudes as driven by thunderstorm
  activity, the possible air transport from the lower latitudes to the
  polar region may significantly distort the signal of solar activity
  in a nitrate record. The present work is focused on a statistical
  study of the relation between the air transport from low and middle
  latitudes and the nitrate deposition in the polar region. We used the
  data from the TALDICE drilling project (Talos Dome, Antarctica). As
  galactic cosmic ray indices we used the reconstructions of heliospheric
  moderation parameter based on (14) C from INTCAL09 and (10) Be from
  GRIP. The data series cover the age range from 675 till 12000 years BP
  (i.e. before 1950). We applied the wavelet coherence analysis to compare
  the nitrate series with a number of substances/proxies: Na(+) , Ca(2+)
  , MSA (methanesulphonic acid), delta(18) O, no-sea-salt-SO_4(2-) and
  reconstructions of heliospheric modulation parameter from the (14) C and
  (10) Be records. We found (1) a confirmation that the multimillennial
  variability of nitrate is in inverse relation with cosmic ray flux;
  (2) no sign of the nitrate transport from lower latitudes to the site
  of deposition. This suggests that variations in the nitrate record in
  the time scale of hundreds-thousands of years are most likely caused
  by local production and deposition processes.

---------------------------------------------------------
Title: Extreme event of cosmic rays in 775 AD: Data and hypotheses
Authors: Usoskin, Ilya; Kovaltsov, Gennady
2014cosp...40E3444U    Altcode:
  An interesting event has been found recently that took place around 775
  AD, as a peak in cosmogenic radionuclides: 14C, 10Be, and 36Cl. Detailed
  analysis of annual 14C data measured in several different tree trunks
  (from Japan and Europe) as well as in shallow sea coral skeletons
  is confirmed by lower resolution data of 10Be and 36Cl in polar ice
  cores. While the very existence of the event is beyond any doubts,
  its origin is not clear. We overview different hypotheses proposed
  as a cause of the event, including a gamma-ray burst, supernova,
  cometary impact and extreme solar flare. We discuss several errors made
  earlier in evaluating parameters of the event and the corresponding
  phenomena. We show that an extreme event in solar energetic particles
  remains the most probable reason for the event.

---------------------------------------------------------
Title: Occurrence Probability of Large Solar Energetic Particle
Events: Assessment from Data on Cosmogenic Radionuclides in Lunar
    Rocks
Authors: Kovaltsov, G. A.; Usoskin, I. G.
2014SoPh..289..211K    Altcode: 2013arXiv1305.5088K
  We revisited assessments of the occurrence probability distribution of
  large events in solar energetic particles (SEP), based on measurements
  of cosmogenic radionuclides in lunar rocks. We present a combined
  cumulative occurrence probability distribution of SEP events based
  on three timescales: directly measured SEP fluences for the past 60
  years; estimates based on the terrestrial cosmogenic radionuclides
  <SUP>10</SUP>Be and <SUP>14</SUP>C for the multi-millennial (Holocene)
  timescale; and cosmogenic radionuclides measured in lunar rocks on a
  timescale of up to 1 Myr. These three timescales yield a consistent
  distribution. The data suggest a strong roll-over of the occurrence
  probability, so that SEP events with a proton fluence with energy
  &gt; 30 MeV greater than 10<SUP>11</SUP> (protons cm<SUP>−2</SUP>
  yr<SUP>−1</SUP>) are not expected on a Myr timescale.

---------------------------------------------------------
Title: High energy particles and aerosol processes in the atmosphere
Authors: Mironova, Irina; Usoskin, Ilya
2014cosp...40E2114M    Altcode:
  The main ionization source of the middle and low Earth atmosphere
  is related to energetic particles coming from outer space. Usually
  it is ionization from cosmic rays that is always present in the
  atmosphere. However, in a case of a very strong solar eruption some
  solar energetic particles (SEP) can reach middle/low atmosphere
  increasing the ionization rate up to some orders of magnitude at
  polar latitudes. By means of case studies of solar protons events
  with different energies of particles and their influence on various
  atmospheric parameters it was possible to evaluate the effect of solar
  (SEP) and galactic (GCR) particles on polar microphysical processes. The
  case studies of the extreme SEP events show their possible applications
  for natural variations of the aerosol content. Nevertheless, the effect
  of the additional ambient air ionization on the aerosol formation is
  minor, in comparison with temperature effect, and can take place only in
  the cold polar atmospheric conditions. Possible accompanied temperature
  decreases can be connected with chemical changes of polar atmosphere
  that can be also reason of high energetic particles’ effect.

---------------------------------------------------------
Title: Method of Express Analysis of Temporal Evolution of the
    Spectral and Angular Distributions of Seps during Gles Using NM Data
Authors: Mishev, Alexander; Usoskin, Ilya
2014cosp...40E2124M    Altcode:
  It is important for space weather studies to be estimate radiation
  environment during major SEP (solar energetic particle) events. For this
  purpose, the main characteristics, viz. spectra and anisotropy of SEPs,
  should be derived in near real time. Here we present a method for a
  quasi-real time analysis of ground level enhancements using neutron
  monitor (NM) data. The method is based on a precise computations of
  SEP propagation in the Earth's magnetosphere, namely the assymptotic
  cones of acceptance of NM, application of the new computed neutron
  monitor yield function and non-linear optimization. Several examples
  and a comparison with previously obtained results as well with full
  scale modeling are demonstrated.

---------------------------------------------------------
Title: Temporal Evolution of Spectral and Angular Characteristics
    of SEP Particles during Several GLEs of Solar Cycle 23 Derived from
    NM Data
Authors: Mishev, Alexander; Usoskin, Ilya; Kocharov, Leon
2014cosp...40E2126M    Altcode:
  High-energy charged particles of solar origin could represent a severe
  radiation risk for astronauts and air crew. In addition, they could
  disrupt technological systems. When a ground-based neutron monitor
  register abrupt increases in solar energetic particles (SEPs),
  we observe a special case of solar energetic particle event, a
  ground-level enhancement (GLE). In order to derive the spectral and
  angular characteristics of GLE particles a precise computation of
  solar energetic particle propagation in the Earth's magnetosphere
  and atmosphere is necessary. It consists of detailed computation
  of assymptotic cones for neutron monitors (NMs) and application
  of inverse method using the newly computed neutron monitor yield
  function. Assymptotic directions are computed using the Planetocosmics
  code and realistic magnetospheric models, namely IGRF as the internal
  model and Tsyganenko 89 with the corresponding Kp index as the
  external one. The inverse problem solution is performed on the basis
  of non-linear least squares method, namely Levenberg-Marqurdt. In the
  study presented here, we analyse several major GLEs of the solar cycle
  23 as well as the first GLE event of the solar cycle 24, namely GLE69,
  GLE70 and GLE 71. The SEP spectra and pitch angle distribution are
  obtained at different momenta since the event's onset. The obtained
  characteristics are compared with previously reported results. The
  obtained results are briefly discussed.

---------------------------------------------------------
Title: The Disagreement Between Models and Observations of the Cosmic
    Ray Latitude Surveys is Solved with New NM Yield Function
Authors: Mishev, Alexander; Usoskin, Ilya; Kovaltsov, Gennady
2014cosp...40E2125M    Altcode:
  A convenient tool to measure cosmic ray (CR) variations in the
  vicinity of Earth is the world network of neutron monitors NMs. In
  order to derive angular and spectral characteristics of primary
  cosmic ray particles, specifically during ground level enhancements
  (GLE), a precise information for NM yield function is necessary. A
  long-standing problem, over last decades, is the disagreement between
  theoretically predicted spatial variability of CR and the directly
  measured latitude survey of NM count rate. Here we present a newly
  computed yield function of the standard sea-level 6NM64 neutron
  monitor for primary proton and alpha nuclei. The computations have
  been performed with Planetocosmics and CORSIKA codes using also an
  updated information concerning NM registration efficiency. A previously
  neglected effect of the geometrical correction of the NM effective
  area is considered. This correction enhances the relative impact of
  higher-energy cosmic rays, namely with energy above 5-10 GeV/nucleon,
  in neutron monitor count rate. This correction allows us to resolve
  the long-standing problem of disagreement between the theoretically
  calculated spatial variability of cosmic rays over the globe and the
  experimentally measured latitude surveys. The newly calculated yield
  function, corrected for this geometrical factor is fully consistent with
  the experimental latitude surveys performed during three consecutive
  solar minima in 1976-77, 1986-87 and 1996-97.

---------------------------------------------------------
Title: Parameterization of ionization induced in the atmosphere by
    precipitating particles
Authors: Artamonov, Anton; Usoskin, Ilya; Kovaltsov, Gennady
2014cosp...40E.123A    Altcode:
  We present a physical model to calculate ionization induced in
  the atmosphere by precipitating particles. This model is based on
  the Bethe-Bloch equation applied for precipitating particles such
  as: electrons, alpha-particles and protons. The energy range of
  precipitating particles is up to 5MeV and 80MeV/nuc respectively. This
  model provides an easy implementation with a robust realization of model
  calculations for a wide range of incident energies of precipitating
  particles. This method is limited to the upper-middle atmosphere. An
  ionization yield function [see, Usoskin and Kovaltsov, 2006; Usoskin,
  Kovaltsov, Mironova, 2010] can be also used in this model, making it
  possible to calculate the atmospheric ionization effect of precipitating
  particles for the entire atmosphere, dawn to the ground.

---------------------------------------------------------
Title: Inconsistency of the Wolf sunspot number series around 1848
Authors: Leussu, Raisa; Usoskin, Ilya G.; Arlt, Rainer; Mursula, Kalevi
2013A&A...559A..28L    Altcode: 2013arXiv1310.8443L
  <BR /> Aims: Sunspot numbers form a benchmark series in many studies,
  but may still contain inhomogeneities and inconsistencies. In
  particular, an essential discrepancy exists between the two main
  sunspot number series, Wolf and group sunspot numbers (WSN and GSN,
  respectively), before 1848. The source of this discrepancy has
  remained unresolved so far. However, the recently digitized series
  of solar observations in 1825-1867 by Samuel Heinrich Schwabe,
  who was the primary observer of the WSN before 1848, makes such an
  assessment possible. <BR /> Methods: We construct sunspot series,
  similar to WSN and GSN but using only Schwabe's data. These series,
  called here WSN-S and GSN-S, respectively, were compared with the
  original WSN and GSN series for the period 1835-1867 for possible
  inhomogeneities. <BR /> Results: This study supports the earlier
  conclusions that the GSN series is more consistent and homogeneous in
  the earlier part than the WSN series. We show that: the GSN series is
  homogeneous and consistent with the Schwabe data throughout the entire
  studied period; the WSN series decreases by roughly 20% around 1848,
  which is caused by the change of the primary observer from Schwabe
  to Wolf and an inappropriate individual correction factor used for
  Schwabe in the WSN; this implies a major inhomogeneity in the WSN,
  which needs to be corrected by reducing its values by 20% before 1848;
  the corrected WSN series is in good agreement with the GSN series.

---------------------------------------------------------
Title: Sunspot positions and sizes for 1825-1867 from the observations
    by Samuel Heinrich Schwabe
Authors: Arlt, R.; Leussu, R.; Giese, N.; Mursula, K.; Usoskin, I. G.
2013MNRAS.433.3165A    Altcode: 2013arXiv1305.7400A; 2013MNRAS.tmp.1611A
  Samuel Heinrich Schwabe made 8486 drawings of the solar disc with
  sunspots in the period from 1825 November 5 to 1867 December 29. We
  have measured sunspot sizes and heliographic positions on digitized
  images of these drawings. A total of about 135 000 measurements
  of individual sunspots are available in a data base. Positions are
  accurate to about 5 per cent of the solar radius or to about 3° in
  heliographic coordinates in the solar-disc centre. Sizes were given
  in 12 classes as estimated visually with circular cursor shapes on
  the screen. Most of the drawings show a coordinate grid aligned with
  the celestial coordinate system. A subset of 1168 drawings have no
  indication of their orientation. We have used a Bayesian estimator
  to infer the orientations of the drawings as well as the average
  heliographic spot positions from a chain of drawings of several days,
  using the rotation profile of the present Sun. The data base also
  includes all information available from Schwabe on spotless days.

---------------------------------------------------------
Title: Eccentric dipole approximation of the geomagnetic field:
    Application to cosmic ray computations
Authors: Nevalainen, J.; Usoskin, I. G.; Mishev, A.
2013AdSpR..52...22N    Altcode:
  A comparison of the full IGRF model of the geomagnetic field with two
  simplified models, the truncated IGRF and the eccentric dipole model,
  is performed. The simplified models were found to provide a reasonable
  approximation for the large scale geomagnetic field distribution. In
  the application of the simplified geomagnetic models to the shielding
  of cosmic rays in the magnetosphere as quantified via the geomagnetic
  cut-off rigidity, the eccentric dipole and the truncated IGRF provide
  a good large scale view. The use of the simplified model does not
  introduce any additional systematic errors at the global scale but
  may be a source of moderate uncertainty at the regional scale in the
  tropical Atlantic region. This study quantitatively validates the use
  of such simplified geomagnetic models when describing the shielding
  of cosmic rays in the magnetosphere.

---------------------------------------------------------
Title: Waldmeier relations and the solar cycle dynamics by the
    mean-field dynamos
Authors: Pipin, V. V.; Sokoloff, D. D.; Usoskin, I. G.
2013IAUS..294..595P    Altcode: 2012arXiv1211.2423P
  The long-term variability of the sunspot cycle, as recorded by the Wolf
  numbers, are imprinted in different kinds of statistical relations
  which relate the cycle amplitudes, duration and shapes. This subject
  always gets a special attention because it is important for the solar
  activity forecast. We discuss statistical properties of the mean-field
  dynamo model with the fluctuating α-effect. Also, we estimate dynamical
  properties of the model for the long and short time-scale and compare
  it with the dynamics of the sunspot numbers data sets.

---------------------------------------------------------
Title: Neutron monitor yield function: New improved computations
Authors: Mishev, A. L.; Usoskin, I. G.; Kovaltsov, G. A.
2013JGRA..118.2783M    Altcode: 2016arXiv161201498M
  A ground-based neutron monitor (NM) is a standard tool to measure
  cosmic ray (CR) variability near Earth, and it is crucially important
  to know its yield function for primary CRs. Although there are several
  earlier theoretically calculated yield functions, none of them agrees
  with experimental data of latitude surveys of sea-level NMs, thus
  suggesting for an inconsistency. A newly computed yield function of the
  standard sea-level 6NM64 NM is presented here separately for primary
  CR protons and α-particles, the latter representing also heavier
  species of CRs. The computations have been done using the GEANT-4
  PLANETOCOSMICS Monte-Carlo tool and a realistic curved atmospheric
  model. For the first time, an effect of the geometrical correction of
  the NM effective area, related to the finite lateral expansion of the
  CR induced atmospheric cascade, is considered, which was neglected in
  the previous studies. This correction slightly enhances the relative
  impact of higher-energy CRs (energy above 5-10 GeV/nucleon) in NM count
  rate. The new computation finally resolves the long-standing problem of
  disagreement between the theoretically calculated spatial variability
  of CRs over the globe and experimental latitude surveys. The newly
  calculated yield function, corrected for this geometrical factor,
  appears fully consistent with the experimental latitude surveys of
  NMs performed during three consecutive solar minima in 1976-1977,
  1986-1987, and 1996-1997. Thus, we provide a new yield function of the
  standard sea-level NM 6NM64 that is validated against experimental data.

---------------------------------------------------------
Title: The AD775 cosmic event revisited: the Sun is to blame
Authors: Usoskin, I. G.; Kromer, B.; Ludlow, F.; Beer, J.; Friedrich,
   M.; Kovaltsov, G. A.; Solanki, S. K.; Wacker, L.
2013A&A...552L...3U    Altcode: 2013arXiv1302.6897U
  <BR /> Aims: Miyake et al. (2012, Nature, 486, 240, henceforth M12)
  recently reported, based on <SUP>14</SUP>C data, an extreme cosmic
  event in about AD775. Using a simple model, M12 claimed that the event
  was too strong to be caused by a solar flare within the standard
  theory. This implied a new paradigm of either an impossibly strong
  solar flare or a very strong cosmic ray event of unknown origin that
  occurred around AD775. However, as we show, the strength of the event
  was significantly overestimated by M12. Several subsequent works have
  attempted to find a possible exotic source for such an event, including
  a giant cometary impact upon the Sun or a gamma-ray burst, but they are
  all based on incorrect estimates by M12. We revisit this event with
  analysis of new datasets and consistent theoretical modelling. <BR
  /> Methods: We verified the experimental result for the AD775 cosmic
  ray event using independent datasets including <SUP>10</SUP>Be series
  and newly measured <SUP>14</SUP>C annual data. We surveyed available
  historical chronicles for astronomical observations for the period
  around the AD770s to identify potential sightings of aurorae borealis
  and supernovae. We interpreted the <SUP>14</SUP>C measurements using
  an appropriate carbon cycle model. <BR /> Results: We show that:
  (1) The reality of the AD775 event is confirmed by new measurements
  of <SUP>14</SUP>C in German oak; (2) by using an inappropriate
  carbon cycle model, M12 strongly overestimated the event's strength;
  (3) the revised magnitude of the event (the global <SUP>14</SUP>C
  production Q = (1.1 - 1.5) × 10<SUP>8</SUP> atoms/cm<SUP>2</SUP>)
  is consistent with different independent datasets (<SUP>14</SUP>C,
  <SUP>10</SUP>Be, <SUP>36</SUP>Cl) and can be associated with a
  strong, but not inexplicably strong, solar energetic particle event
  (or a sequence of events), and provides the first definite evidence
  for an event of this magnitude (the fluence &gt;30 MeV was about
  4.5 × 10<SUP>10</SUP> cm<SUP>-2</SUP>) in multiple datasets; (4)
  this interpretation is in agreement with increased auroral activity
  identified in historical chronicles. <BR /> Conclusions: The results
  point to the likely solar origin of the event, which is now identified
  as the greatest solar event on a multi-millennial time scale, placing
  a strong observational constraint on the theory of explosive energy
  releases on the Sun and cool stars.

---------------------------------------------------------
Title: Consistent long-term variation in the hemispheric asymmetry
    of solar rotation
Authors: Zhang, L.; Mursula, K.; Usoskin, I.
2013A&A...552A..84Z    Altcode:
  Context. Solar active longitudes and their rotation have been studied
  for a long time using various forms of solar activity. However, the
  results on the long-term evolution of rotation rates and the hemispheric
  asymmetry obtained by earlier authors differ significantly from each
  other. <BR /> Aims: We aim to find a consistent result on the long-term
  migration of active longitudes of sunspots in 1877-2008 separately for
  the two hemispheres. <BR /> Methods: We used a dynamic, differentially
  rotating reference system to determine the best-fit values of the
  differential rotation parameters of active longitudes for each year
  in 1877-2008. With these parameters we determined the momentary
  rotation rates at the reference latitude of 17° and calculated the
  non-axisymmetries of active longitudes. We repeated this with five
  different fit intervals and two weighting methods and compared the
  results. <BR /> Results: The evolution of solar surface rotation in
  each hemisphere suggests a quasi-periodicity of about 80-90 years. The
  long-term variations of solar rotation in the northern and southern
  hemisphere have a close anti-correlation, leading to a significant
  80-90-year quasi-periodicity in the north-south asymmetry of solar
  rotation. The north-south asymmetry of solar rotation is found to have
  an inverse relationship with the area of large sunspots. The latitudinal
  contrast of differential rotation is also found to be anti-correlated
  with the sunspot area. Different fit and weight methods yield similar
  results. <BR /> Conclusions: Our results give strong evidence for the
  anti-correlation of the rotation of the two solar hemispheres. The
  long-term oscillation of solar rotation suggests that a systematic
  interchange of angular momentum takes place between the two hemispheres
  at a period of about 80-90 years.

---------------------------------------------------------
Title: The first SEPServer event catalogue ~68-MeV solar proton
    events observed at 1 AU in 1996-2010
Authors: Vainio, Rami; Valtonen, Eino; Heber, Bernd; Malandraki, Olga
   E.; Papaioannou, Athanasios; Klein, Karl-Ludwig; Afanasiev, Alexander;
   Agueda, Neus; Aurass, Henry; Battarbee, Markus; Braune, Stephan;
   Dröge, Wolfgang; Ganse, Urs; Hamadache, Clarisse; Heynderickx, Daniel;
   Huttunen-Heikinmaa, Kalle; Kiener, Jürgen; Kilian, Patrick; Kopp,
   Andreas; Kouloumvakos, Athanasios; Maisala, Sami; Mishev, Alexander;
   Miteva, Rositsa; Nindos, Alexander; Oittinen, Tero; Raukunen, Osku;
   Riihonen, Esa; Rodríguez-Gasén, Rosa; Saloniemi, Oskari; Sanahuja,
   Blai; Scherer, Renate; Spanier, Felix; Tatischeff, Vincent; Tziotziou,
   Kostas; Usoskin, Ilya G.; Vilmer, Nicole
2013JSWSC...3A..12V    Altcode:
  SEPServer is a three-year collaborative project funded by the seventh
  framework programme (FP7-SPACE) of the European Union. The objective
  of the project is to provide access to state-of-the-art observations
  and analysis tools for the scientific community on solar energetic
  particle (SEP) events and related electromagnetic (EM) emissions. The
  project will eventually lead to better understanding of the particle
  acceleration and transport processes at the Sun and in the inner
  heliosphere. These processes lead to SEP events that form one of the key
  elements of space weather. In this paper we present the first results
  from the systematic analysis work performed on the following datasets:
  SOHO/ERNE, SOHO/EPHIN, ACE/EPAM, Wind/WAVES and GOES X-rays. A catalogue
  of SEP events at 1 AU, with complete coverage over solar cycle 23,
  based on high-energy (~68-MeV) protons from SOHO/ERNE and electron
  recordings of the events by SOHO/EPHIN and ACE/EPAM are presented. A
  total of 115 energetic particle events have been identified and analysed
  using velocity dispersion analysis (VDA) for protons and time-shifting
  analysis (TSA) for electrons and protons in order to infer the SEP
  release times at the Sun. EM observations during the times of the
  SEP event onset have been gathered and compared to the release time
  estimates of particles. Data from those events that occurred during
  the European day-time, i.e., those that also have observations from
  ground-based observatories included in SEPServer, are listed and a
  preliminary analysis of their associations is presented. We find that
  VDA results for protons can be a useful tool for the analysis of proton
  release times, but if the derived proton path length is out of a range
  of 1 AU &lt; s ≲ 3 AU, the result of the analysis may be compromised,
  as indicated by the anti-correlation of the derived path length and
  release time delay from the associated X-ray flare. The average path
  length derived from VDA is about 1.9 times the nominal length of
  the spiral magnetic field line. This implies that the path length of
  first-arriving MeV to deka-MeV protons is affected by interplanetary
  scattering. TSA of near-relativistic electrons results in a release
  time that shows significant scatter with respect to the EM emissions
  but with a trend of being delayed more with increasing distance between
  the flare and the nominal footpoint of the Earth-connected field line.

---------------------------------------------------------
Title: The First Ground Level Enhancement Event of Solar Cycle 24:
    Direct Observation of Shock Formation and Particle Release Heights
Authors: Gopalswamy, N.; Xie, H.; Akiyama, S.; Yashiro, S.; Usoskin,
   I. G.; Davila, J. M.
2013ApJ...765L..30G    Altcode: 2013arXiv1302.1474G
  We report on the 2012 May 17 ground level enhancement (GLE) event,
  which is the first of its kind in solar cycle 24. This is the first GLE
  event to be fully observed close to the surface by the Solar Terrestrial
  Relations Observatory (STEREO) mission. We determine the coronal mass
  ejection (CME) height at the start of the associated metric type
  II radio burst (i.e., shock formation height) as 1.38 Rs (from the
  Sun center). The CME height at the time of GLE particle release was
  directly measured from a STEREO image as 2.32 Rs, which agrees well
  with the estimation from CME kinematics. These heights are consistent
  with those obtained for cycle-23 GLEs using back-extrapolation. By
  contrasting the 2012 May 17 GLE with six other non-GLE eruptions from
  well-connected regions with similar or larger flare sizes and CME
  speeds, we find that the latitudinal distance from the ecliptic is
  rather large for the non-GLE events due to a combination of non-radial
  CME motion and unfavorable solar B0 angle, making the connectivity
  to Earth poorer. We also find that the coronal environment may play
  a role in deciding the shock strength.

---------------------------------------------------------
Title: A History of Solar Activity over Millennia
Authors: Usoskin, Ilya G.
2013LRSP...10....1U    Altcode:
  Presented here is a review of present knowledge of the long-term
  behavior of solar activity on a multi-millennial timescale, as
  reconstructed using the indirect proxy method. The concept of solar
  activity is discussed along with an overview of the special indices
  used to quantify different aspects of variable solar activity, with
  special emphasis upon sunspot number.

---------------------------------------------------------
Title: Calculation of the cosmic ray induced ionization for the
    region of Athens
Authors: Makrantoni, P.; Mavromichalaki, H.; Usoskin, I.; Papaioannou,
   A.
2013JPhCS.409a2232M    Altcode:
  A complete study of ionization induced by cosmic rays, both solar and
  galactic, in the atmosphere, is presented. For the computation of the
  cosmic ray induced ionization, the CRII model was used [1] as well
  its new version [2] which is extended to the upper atmosphere. In this
  work, this model has been applied to the entire atmosphere, i.e. from
  atmospheric depth 0 g/cm<SUP>2</SUP>, which corresponds to the upper
  limit of the atmosphere, to 1025 g/cm<SUP>2</SUP>, which corresponds
  to the surface. Moreover, an application has been made as a function
  of rigidity and latitude, from 0GV or 90° which corresponds to Polar
  regions, to 15GV or 0° which corresponds to Equator. Athens corresponds
  to 8.53GV rigidity and 38°N latitude. An application has, also, been
  made for the different phases of the solar cycle (maximum at the year
  2000 and minimum at the year 2010), which coincides with the operational
  period of the cosmic ray station of the University of Athens.

---------------------------------------------------------
Title: Computations of cosmic ray propagation in the Earth's
    atmosphere, towards a GLE analysis
Authors: Mishev, A.; Usoskin, I.
2013JPhCS.409a2152M    Altcode:
  Computation of solar energetic particles propagation in the
  magnetosphere and atmosphere of the Earth is very important for ground
  level enhancement analysis. Detailed simulations of solar energetic
  particles events starting from asymptotic direction computation
  and NM detector response make it possible to build a strategy for
  inverse problem solution i.e. obtaining the characteristics of
  solar energetic particles on the basis on ground measurements. In
  this study a simulation of cosmic ray atmospheric cascade is carried
  out with PLANETOCOSMICS code. Energy spectra of secondary particles,
  namely neutrons and protons are obtained at various altitudes in the
  rigidity range of 0.7 GV to 1 TV of primary particles. Considering
  updated results for NM-64 detection efficiency the specific yield
  function for the standard neutron monitor is obtained for vertically
  and obliquely incident primary particles. The obtained results and
  applications are discussed.

---------------------------------------------------------
Title: Forecast of the arrival of interplanetary shocks by measuring
    cosmic ray fluctuations in the interplanetary medium
Authors: Starodubtsev, S. A.; Grigoryev, V. G.; Usoskin, I. G.
2013JPhCS.409a2180S    Altcode:
  Here we present a method to forecast the arrival of an interplanetary
  shock to the Earth's orbit in advance of up to one day, using cosmic
  ray fluctuations and solar wind parameters measured onboard the ACE
  spacecraft. The method is based on our previous results [1]. By means
  of continuous monitoring of the interplanetary space state since April
  2010, we conclude that not all shocks can be reliably forecasted by
  the method. Only those interplanetary shocks, for which a large flux
  of low-energy particles (10 keV - 10 MeV) of solar or interplanetary
  origin exists in the upstream region, can be forecasted. This is
  typically related to quasi-parallel shocks. In the absence of such
  particles, a forecast cannot be made. This is a typical situation
  for quasi-perpendicular shocks. Our analysis shows that, on average,
  an interplanetary shock can be forecasted for several hours up to one
  day, with the probability about 70%.

---------------------------------------------------------
Title: Hot Precursor Ejecta and Other Peculiarities of the 2012 May
    17 Ground Level Enhancement Event
Authors: Gopalswamy, N.; Xie, H.; Nitta, N. V.; Usoskin, I.; Davila,
   J. M.
2012AGUFMSH21A2180G    Altcode:
  We report on the first Ground Level Enhancement (GLE) event of Solar
  Cycle 24, which occurred on May 17, 2012 from a well-connected region
  (NOAA AR 11476, N11W76) on the Sun. There has been a real dearth
  of GLE events during cycle 24: even though the Sun has reached its
  solar maximum phase, it has produced only this one GLE event. Over the
  first 4.5 years of solar cycle 23, there were 5 GLE events, which is
  roughly a third of all the events of that cycle. The recent GLE event
  was associated with a moderate flare with an X-ray size of only M5.1,
  well below the median flare size (X3.8) of cycle 23 GLE events. On
  the other hand, the associated CME was very fast (~2000 km/s),
  typical of GLE events. During cycle 23, the CME speeds in GLE events
  ranged from 1203 km/s to 3675 km/s with an average value of 2083 km/s
  (Gopalswamy et al., 2012). The speed of the cycle 24 GLE was measured
  accurately because it was a limb event in the SOHO coronagraphic field
  of view. The CME was also observed by the STEREO coronagraphs, which
  helped derive the initial acceleration as 1.5 km/s/s, which is also
  typical of GLE-producing CMEs. We were also able to directly determine
  the heliocentric distance of the CME (2.3 solar radii (Rs)) at the
  time of the release of GLE particles because there was a STEREO/COR1
  image precisely at the time of the particle release. This result
  is consistent with what was obtained for the cycle 23 GLE events,
  including the distance of the CME at the time of metric type II burst
  onset (1.3 Rs), indicating shock formation very close to the Sun
  ( ~0.3 Rs above the solar surface). We infer that the shock had to
  travel an additional 1 Rs before the GLE particles were released. The
  CME had a precursor in the form of a hot ejecta some tens of minutes
  before the main eruption. The preceding ejecta is termed hot because
  it was observed only in the 94 A images obtained by the Solar Dynamics
  Observatory (SDO). The 94 A images correspond to coronal a temperature
  of ~6MK. The lower temperature images such as at 193 A did not show
  the ejecta. The hot ejecta was accelerating and attained a speed
  of ~70 km/s before it was blasted by the big GLE-producing CMEs. We
  suggest that the hot material of the precursor ejecta might have been
  further accelerated by the CME-driven shock resulting in the GLE
  event. Reference Gopalswamy, N.,Xie, H., Yashiro, S., Akiyama, S.,
  Mäkelä, P., Usoskin, I. G., Properties of Ground Level Enhancement
  Events and the Associated Solar Eruptions During Solar Cycle 23,
  Space Science reviews, DOI: 10.1007/s11214-012-9890-4

---------------------------------------------------------
Title: Heliospheric modulation of galactic cosmic rays during grand
solar minima: Past and future variations
Authors: Owens, M. J.; Usoskin, I.; Lockwood, M.
2012GeoRL..3919102O    Altcode:
  Galactic cosmic ray flux at Earth is modulated by the heliospheric
  magnetic field. Heliospheric modulation potential, Φ, during grand
  solar minima is investigated using an open solar flux (OSF) model with
  OSF source based on sunspot number, R, and OSF loss on heliospheric
  current sheet inclination. Changing dominance between source and loss
  means Φ varies in- (anti-) phase with R during strong (weak) cycles,
  in agreement with Φ estimates from ice core records of <SUP>10</SUP>Be
  concentration, which are in-phase during most of the last 300 years,
  but anti-phase during the Maunder Minimum. Model results suggest
  “flat” OSF cycles, such as solar cycle 20 result from OSF source
  and loss terms temporarily balancing throughout the cycle. Thus even
  if solar activity continues to decline steadily, the long-term drop
  in OSF through SC21 to SC23 may plateau during SC24, though reemerge
  in SC25 with the inverted phase relation.

---------------------------------------------------------
Title: Climate and Weather of the Sun - Earth System
Authors: Usoskin, Ilya; Krivova, Natalie
2012aaa2.book..397U    Altcode:
  The Sun is a variable star whose output, including electromagnetic
  radiation, magnetic fields and energetic particles varies at different
  time scales, from seconds to millennia. Solar variability affects the
  interplanetary medium but also planetary environments, including that of
  Earth. The state of the near-Earth environment is collectively called
  the Space weather, while its long-term changes make the concept of
  Space Climate. This forms the field of an interdisciplinary research
  focused on a wide range of topics: from solar physics, solar wind,
  cosmic rays, to planetary atmospheres and climate. Special emphasis
  is paid upon the processes that inter-relate solar variability
  and terrestrial environment - the Sun-Earth system. In this work,
  we present an overview on the state of the art in the field of the
  weather and climate of the Sun-Earth system.

---------------------------------------------------------
Title: Properties of Ground Level Enhancement Events and the
    Associated Solar Eruptions During Solar Cycle 23
Authors: Gopalswamy, N.; Xie, H.; Yashiro, S.; Akiyama, S.; Mäkelä,
   P.; Usoskin, I. G.
2012SSRv..171...23G    Altcode: 2012SSRv..tmp...38G; 2012arXiv1205.0688G
  Solar cycle 23 witnessed the most complete set of observations
  of coronal mass ejections (CMEs) associated with the Ground Level
  Enhancement (GLE) events. We present an overview of the observed
  properties of the GLEs and those of the two associated phenomena,
  viz., flares and CMEs, both being potential sources of particle
  acceleration. Although we do not find a striking correlation between
  the GLE intensity and the parameters of flares and CMEs, the solar
  eruptions are very intense involving X-class flares and extreme CME
  speeds (average ∼2000 km/s). An M7.1 flare and a 1200 km/s CME are
  the weakest events in the list of 16 GLE events. Most (80 %) of the CMEs
  are full halos with the three non-halos having widths in the range 167
  to 212 degrees. The active regions in which the GLE events originate are
  generally large: 1290 msh (median 1010 msh) compared to 934 msh (median:
  790 msh) for SEP-producing active regions. For accurate estimation of
  the CME height at the time of metric type II onset and GLE particle
  release, we estimated the initial acceleration of the CMEs using flare
  and CME observations. The initial acceleration of GLE-associated CMEs
  is much larger (by a factor of 2) than that of ordinary CMEs (2.3
  km/s<SUP>2</SUP> vs. 1 km/s<SUP>2</SUP>). We confirmed the initial
  acceleration for two events for which CME measurements are available
  in the inner corona. The GLE particle release is delayed with respect
  to the onset of all electromagnetic signatures of the eruptions:
  type II bursts, low frequency type III bursts, soft X-ray flares
  and CMEs. The presence of metric type II radio bursts some 17 min
  (median: 16 min; range: 3 to 48 min) before the GLE onset indicates
  shock formation well before the particle release. The release of GLE
  particles occurs when the CMEs reach an average height of ∼3.09 R
  <SUB> s </SUB> (median: 3.18 R <SUB> s </SUB>; range: 1.71 to 4.01
  R <SUB> s </SUB>) for well-connected events (source longitude in the
  range W20-W90). For poorly connected events, the average CME height at
  GLE particle release is ∼66 % larger (mean: 5.18 R <SUB> s </SUB>;
  median: 4.61 R <SUB> s </SUB>; range: 2.75-8.49 R <SUB> s </SUB>). The
  longitudinal dependence is consistent with shock accelerations because
  the shocks from poorly connected events need to expand more to cross
  the field lines connecting to an Earth observer. On the other hand, the
  CME height at metric type II burst onset has no longitudinal dependence
  because electromagnetic signals do not require magnetic connectivity
  to the observer. For several events, the GLE particle release is very
  close to the time of first appearance of the CME in the coronagraphic
  field of view, so we independently confirmed the CME height at particle
  release. The CME height at metric type II burst onset is in the narrow
  range 1.29 to 1.8 R <SUB> s </SUB>, with mean and median values of
  1.53 and 1.47 R <SUB> s </SUB>. The CME heights at metric type II
  burst onset and GLE particle release correspond to the minimum and
  maximum in the Alfvén speed profile. The increase in CME speed between
  these two heights suggests an increase in Alfvénic Mach number from
  2 to 3. The CME heights at GLE particle release are in good agreement
  with those obtained from the velocity dispersion analysis (Reames in
  Astrophys. J. 693:812, 2009a; Astrophys. J. 706:844, 2009b) including
  the source longitude dependence. We also discuss the implications of
  the delay of GLE particle release with respect to complex type III
  bursts by ∼18 min (median: 16 in; range: 2 to 44 min) for the flare
  acceleration mechanism. A similar analysis is also performed on the
  delay of particle release relative to the hard X-ray emission.

---------------------------------------------------------
Title: Nitrate in Polar Ice: A New Tracer of Solar Variability
Authors: Traversi, R.; Usoskin, I. G.; Solanki, S. K.; Becagli, S.;
   Frezzotti, M.; Severi, M.; Stenni, B.; Udisti, R.
2012SoPh..280..237T    Altcode: 2012SoPh..tmp..169T
  Knowledge of the long-term variability of solar activity is of
  both astrophysical and geoscientific interest. Reconstructions of
  solar activity over multiple millennia are traditionally based on
  cosmogenic isotopes <SUP>14</SUP>C or <SUP>10</SUP>Be measured in
  natural terrestrial archives, but the two isotopes exhibit significant
  differences on millennial time scales, so that our knowledge of solar
  activity at this time scale remains somewhat uncertain. Here we present
  a new potential proxy of solar activity on the centennial-millennial
  time scale, based on a chemical tracer, viz. nitrate content in an ice
  core drilled at Talos Dome (Antarctica). We argue that this location
  is optimal for preserving the solar signal in the nitrate content
  during the Holocene. By using the firn core from the same location
  we show that the 11-year and Gleissberg cycles are present with the
  variability of 10 - 25 % in nitrate content in the pre-industrial
  epoch. This is consistent with the results of independent efforts of
  modeling HNO<SUB>3</SUB> and NO<SUB>y</SUB> in Antarctic near surface
  air. However, meteorological noise on the interannual scale makes
  it impossible to resolve individual solar cycles. Based on different
  processes of formation and transport compared to cosmogenic isotopes,
  it provides new, independent insight into long-term solar activity
  and helps resolve the uncertainties related to cosmogenic isotopes as
  diagnostics of solar activity.

---------------------------------------------------------
Title: Occurrence of Extreme Solar Particle Events: Assessment from
    Historical Proxy Data
Authors: Usoskin, Ilya G.; Kovaltsov, Gennady A.
2012ApJ...757...92U    Altcode: 2012arXiv1207.5932U
  The probability of occurrence of extreme solar particle events (SPEs)
  with proton fluence (&gt;30 MeV) F <SUB>30</SUB> &gt;= 10<SUP>10</SUP>
  cm<SUP>-2</SUP> is evaluated based on data on the cosmogenic isotopes
  <SUP>14</SUP>C and <SUP>10</SUP>Be in terrestrial archives covering
  centennial-millennial timescales. Four potential candidates with F
  <SUB>30</SUB> = (1-1.5) × 10<SUP>10</SUP> cm<SUP>-2</SUP> and no
  events with F <SUB>30</SUB> &gt; 2 × 10<SUP>10</SUP> cm<SUP>-2</SUP>
  are identified since 1400 AD in the annually resolved <SUP>10</SUP>Be
  data. A strong SPE related to the Carrington flare of 1859 AD is not
  supported by the data. For the last 11,400 years, 19 SPE candidates
  with F <SUB>30</SUB> = (1-3) × 10<SUP>10</SUP> cm<SUP>-2</SUP>
  are found and clearly no event with F <SUB>30</SUB> &gt; 5 ×
  10<SUP>10</SUP> cm<SUP>-2</SUP> (50 times the SPE of 1956 February
  23) has occurred. These values serve as observational upper limits
  on the strength of SPEs on the timescale of tens of millennia. Two
  events, ca. 780 and 1460 AD, appear in different data series making
  them strong candidates for extreme SPEs. We build a distribution of
  the occurrence probability of extreme SPEs, providing a new strict
  observational constraint. Practical limits can be set as F <SUB>30</SUB>
  ≈ 1, 2-3, and 5×10<SUP>10</SUP> cm<SUP>-2</SUP> for occurrence
  probabilities ≈10<SUP>-2</SUP>, 10<SUP>-3</SUP>, and 10<SUP>-4</SUP>
  yr<SUP>-1</SUP>, respectively. Because of the uncertainties, our
  results should be interpreted as a conservative upper limit on the SPE
  occurrence near Earth. The mean solar energetic particle (SEP) flux
  is evaluated as ≈40 (cm<SUP>2</SUP> s)<SUP>-1</SUP>, in agreement
  with estimates from lunar rocks. On average, extreme SPEs contribute
  about 10% to the total SEP fluence.

---------------------------------------------------------
Title: Preface: Solar Variability, Cosmic Rays and Climate: What's up?
Authors: Usoskin, Ilya G.
2012AdSpR..50..655U    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: Estimating the frequency of extremely energetic solar events,
    based on solar, stellar, lunar, and terrestrial records
Authors: Schrijver, C. J.; Beer, J.; Baltensperger, U.; Cliver,
   E. W.; Güdel, M.; Hudson, H. S.; McCracken, K. G.; Osten, R. A.;
   Peter, T.; Soderblom, D. R.; Usoskin, I. G.; Wolff, E. W.
2012JGRA..117.8103S    Altcode: 2012arXiv1206.4889S; 2012JGRA..11708103S
  The most powerful explosions on the Sun - in the form of bright
  flares, intense storms of solar energetic particles (SEPs), and fast
  coronal mass ejections (CMEs) - drive the most severe space-weather
  storms. Proxy records of flare energies based on SEPs in principle
  may offer the longest time base to study infrequent large events. We
  conclude that one suggested proxy, nitrate concentrations in polar
  ice cores, does not map reliably to SEP events. Concentrations of
  select radionuclides measured in natural archives may prove useful in
  extending the time interval of direct observations up to ten millennia,
  but as their calibration to solar flare fluences depends on multiple
  poorly known properties and processes, these proxies cannot presently be
  used to help determine the flare energy frequency distribution. Being
  thus limited to the use of direct flare observations, we evaluate the
  probabilities of large-energy solar events by combining solar flare
  observations with an ensemble of stellar flare observations. We conclude
  that solar flare energies form a relatively smooth distribution from
  small events to large flares, while flares on magnetically active,
  young Sun-like stars have energies and frequencies markedly in excess
  of strong solar flares, even after an empirical scaling with the mean
  coronal activity level of these stars. In order to empirically quantify
  the frequency of uncommonly large solar flares extensive surveys
  of stars of near-solar age need to be obtained, such as is feasible
  with the Kepler satellite. Because the likelihood of flares larger
  than approximately X30 remains empirically unconstrained, we present
  indirect arguments, based on records of sunspots and on statistical
  arguments, that solar flares in the past four centuries have likely
  not substantially exceeded the level of the largest flares observed
  in the space era, and that there is at most about a 10% chance of a
  flare larger than about X30 in the next 30 years.

---------------------------------------------------------
Title: Grand minima of solar activity during the last millennia
Authors: Usoskin, Ilya G.; Solanki, Sami K.; Kovaltsov, Gennady A.
2012IAUS..286..372U    Altcode:
  In this review we discuss the occurrence and statistical properties of
  Grand minima based on the available data covering the last millennia. In
  particular, we consider the historical record of sunspot numbers
  covering the last 400 years as well as records of cosmogenic isotopes
  in natural terrestrial archives, used to reconstruct solar activity
  for up to the last 11.5 millennia, i.e. throughout the Holocene. Using
  a reconstruction of solar activity from cosmogenic isotope data, we
  analyze statistics of the occurrence of Grand minima. We find that: the
  Sun spends about most of the time at moderate activity, 1/6 in a Grand
  minimum and some time also in a Grand maximum state; Occurrence of Grand
  minima is not a result of long-term cyclic variations but is defined
  by stochastic/chaotic processes; There is a tendency for Grand minima
  to cluster with the recurrence rate of roughly 2000-3000 years, with
  a weak ~210-yr periodicity existing within the clusters. Grand minima
  occur of two different types: shorter than 100 years (Maunder-type)
  and long ~150 years (Spörer-type). It is also discussed that solar
  cycles (most possibly not sunspots cycle) could exist during the
  Grand minima, perhaps with stretched length and asymmetric sunspot
  latitudinal distribution. <P />These results set new observational
  constraints on long-term solar and stellar dynamo models.

---------------------------------------------------------
Title: Reconstructing the history of past solar activity
Authors: Usoskin, Ilya
2012cosp...39.2038U    Altcode: 2012cosp.meet.2038U
  While data of directly observed sunspots is available for the
  past centuries, longer time series are required for many purposes,
  from purely astrophysical (constraints on solar/stellar dynamo) to
  geophysical (assessments on possible solar influence on climate). In
  order to reconstruct solar activity in the past, one has to use
  indirect proxy methods, the most useful being based on cosmogenic
  isotope records. Applying this method to data on cosmogenic 14C
  and 10Be measured in independently dated natural archives, one can
  evaluate long-term variability of solar activity on multi-centennial
  time scales. Here I present a brief review of the modern methods of
  long-term solar activity reconstruction, with special emphasis upon
  separation of Grand minima and maxima of solar activity.

---------------------------------------------------------
Title: A new model of cosmogenic production of radiocarbon
    <SUP>14</SUP>C in the atmosphere
Authors: Kovaltsov, Gennady A.; Mishev, Alexander; Usoskin, Ilya G.
2012E&PSL.337..114K    Altcode: 2012arXiv1206.6974K
  We present the results of full new calculation of radiocarbon
  <SUP>14</SUP>C production in the Earth atmosphere, using a numerical
  Monte-Carlo model. We provide, for the first time, a tabulated
  <SUP>14</SUP>C yield function for the energy of primary cosmic ray
  particles ranging from 0.1 to 1000 GeV/nucleon. We have calculated
  the global production rate of <SUP>14</SUP>C, which is 1.64 and 1.88
  atoms/cm<SUP>2</SUP>/s for the modern time and for the pre-industrial
  epoch, respectively. This is close to the values obtained from
  the carbon cycle reservoir inventory. We argue that earlier models
  overestimated the global <SUP>14</SUP>C production rate because of
  outdated spectra of cosmic ray heavier nuclei. The mean contribution of
  solar energetic particles to the global <SUP>14</SUP>C is calculated
  as about 0.25% for the modern epoch. Our model provides a new tool to
  calculate the <SUP>14</SUP>C production in the Earth's atmosphere, which
  can be applied, e.g., to reconstructions of solar activity in the past.

---------------------------------------------------------
Title: Middle atmosphere response to the solar cycle in irradiance
    and ionizing particle precipitation.
Authors: Semeniuk, Kirill; Usoskin, Ilya; Fomichev, Victor; Melo,
   Stella M. L.; McConnell, John; Fu, Chao
2012cosp...39.1751S    Altcode: 2012cosp.meet.1751S
  The impact of NOx and HOx production by three types of energetic
  particle precipitation (EPP), high energy electrons, solar proton
  events and galactic cosmic rays is examined using a chemistry climate
  model. This process study uses ensemble simulations forced by transient
  EPP derived from observations, fixed chemical boundary conditions
  and fixed seasonally varying sea surface temperatures. We consider
  cases with and without solar cycle in irradiance. Our model results
  show a wintertime polar stratosphere ozone reduction of between 3%
  and 10% in agreement with previous studies. EPP is found to modulate
  the radiative solar cycle effect in the middle atmosphere in a
  significant way, bringing temperature and ozone variations closer
  to observed patterns. The Southern Hemisphere polar vortex undergoes
  an intensification from solar minimum to solar maximum instead of a
  weakening. This changes the solar cycle variation of the Brewer-Dobson
  circulation, with a weakening during solar maxima compared to solar
  minima. In response, the tropical tropopause temperature manifests a
  statistically significant solar cycle variation resulting in about 4%
  more water vapour transported into the lower tropical stratosphere
  during solar maxima compared to solar minima. This has implications
  for surface temperature variation due to the associated change in
  radiative forcing.

---------------------------------------------------------
Title: Reconstruction of solar modulation parameter for galactic
    cosmic rays for the last 70 years
Authors: Usoskin, Ilya; Kovaltsov, Gennady; Bazilevskaya, Galina
2012cosp...39.2039U    Altcode: 2012cosp.meet.2039U
  No abstract at ADS

---------------------------------------------------------
Title: Nitrate in polar ice as a new index of solar variability
Authors: Traversi, Rita; Usoskin, Ilya; Solanki, Sami K.; Becagli,
   Silvia; Frezzotti, Massimo; Severi, Mirko; Stenni, Barbara; Udisti,
   Roberto
2012cosp...39.2001T    Altcode: 2012cosp.meet.2001T
  The Sun affects Earth's climate and environment in multiple ways and
  on different time scales but understanding if and how the variations
  in solar radiative output might drive global climatic change has
  revealed to be a complex and controversial issue. In order to address
  the question about the Sun's role on the climate in the past, present
  and, eventually, in the future, a reliable reconstruction of solar
  activity is mandatory. Over millennia time scales, a quantitative
  information about past solar activity can only be obtained through
  proxies recorded in natural stratified archives (e.g., tree rings or
  ice cores), such as the cosmogenic isotopes 14C and 10Be. Nonetheless,
  the two isotopes exhibit significant differences on millennial time
  scales, making our knowledge of solar activity at this time scale less
  certain. Here we present a new potential proxy of solar activity on the
  centennial-millennial time scale, namely nitrate content in the TALDICE
  ice core (Talos Dome, placeEast Antarctica). Talos Dome site was shown
  to be favourably located to minimize possible local climate effects,
  which may be dominant in other coastal sites and, due to a sufficiently
  high snow accumulation rate throughout the Holocene, such a reversibly
  deposited species as nitrate is preserved here (in contrast to inland
  Antarctic sites) making it a potential paleomarker. Comparing the
  TALDICE nitrate record with the two traditionally used cosmogenic
  proxies of solar activity, we observed that a highly significant
  agreement on the millennial and multi-millennial time scales over the
  Holocene. The relation at centennial time scales is less significant,
  likely due to ice core dating uncertainties. No statistical relationship
  was found between the nitrate data series and other chemical markers
  of local climate/transport. Consequently, the coherence between
  nitrate and cosmogenic isotopes univocally suggests a common origin
  of their long-term variability. As concerning the more recent times,
  we show that the 11-year and Gleissberg cycles are present at a level
  of 10-25% in nitrate content in the pre-industrial epoch after the
  Maunder minimum, which is in agreement with model results. However, the
  “meteorological noise” on the interannual scale makes it impossible
  to resolve individual solar cycles. Since nitrate is characterised by
  different processes of formation and transport, compared to cosmogenic
  isotopes, we conclude that nitrate in this Antarctic ice core forms
  a novel proxy of solar activity on the centennial and longer time
  scales and could help in reconciling the discrepancies between the
  two cosmogenic isotopes as diagnostics of solar activity.

---------------------------------------------------------
Title: Variations of the solar cycle profile in a solar dynamo with
    fluctuating dynamo governing parameters
Authors: Pipin, V. V.; Sokoloff, D. D.; Usoskin, I. G.
2012A&A...542A..26P    Altcode: 2011arXiv1112.6218P
  Context. Solar cycles vary in their amplitude and shape. There are
  several empirical relations between various parameters that link
  the cycle's shape and amplitude, foremost these of the Waldmeier
  relations. <BR /> Aims: The solar cycle is believed to be a result
  of the solar dynamo action, therefore these relations require an
  explanation in the framework of this theory, which we aim to present
  here. <BR /> Methods: We related the cycle-to-cycle variability of
  solar activity to fluctuations of solar dynamo drivers and primarily
  to fluctuations in the parameter responsible for the recovery of
  the poloidal magnetic field from the toroidal one. To be specific,
  we developed a model in the framework of the mean-field dynamo
  based on the differential rotation and α-effect. <BR /> Results:
  We demonstrate that the mean-field dynamo model, which is based on
  a realistic rotation profile and on nonlinearity that is associated
  with the magnetic helicity balance, reproduces both qualitatively
  and quantitatively the Waldmeier relations observed in sunspot data
  since 1750. The model also reproduces more or less successfully other
  relations between the parameters under discussion, in particular,
  the link between odd and even cycles (Gnevyshev-Ohl rule). <BR />
  Conclusions: We conclude that the contemporary solar dynamo theory
  provides a way to explain the cycle-to-cycle variability of solar
  activity as recorded in sunspots.We discuss the importance of the
  model for stellar activity cycles which, as known from the data of
  the Mount Wilson HK project, which measures the Ca H and K line index
  for other stars, demonstrate the cycle-to-cycle variability similar
  to solar cycles. <P />Appendix A is available in electronic form at
  <A href="http://www.aanda.org">http://www.aanda.org</A>

---------------------------------------------------------
Title: Cosmogenic <SUP>7</SUP>Be and <SUP>22</SUP>Na in Finland:
    Production, observed periodicities and the connection to climatic
    phenomena
Authors: Leppänen, A. -P.; Usoskin, I. G.; Kovaltsov, G. A.;
   Paatero, J.
2012JASTP..74..164L    Altcode:
  This study presents theoretical production calculations and time
  series analyses of two cosmogenic isotopes, <SUP>7</SUP>Be and
  <SUP>22</SUP>Na, from the four high-latitude stations of Kotka,
  Kajaani, Rovaniemi and Ivalo located in Finland. We used published
  results for <SUP>7</SUP>Be but performed full simulations of the
  <SUP>22</SUP>Na production in atmosphere. For the first time, lookup
  tables of <SUP>22</SUP>Na production by cosmic rays in the atmosphere
  are presented. In conjunction with calculations using the new model
  of <SUP>22</SUP>Na production, the <SUP>7</SUP>Be/<SUP>22</SUP>Na
  ratios in the atmosphere were also calculated. The wavelet transform
  of the <SUP>7</SUP>Be and <SUP>22</SUP>Na time series revealed sets of
  periodicities in the 2.5-8 year range. The wavelet coherence method was
  used to study coherences between <SUP>7</SUP>Be and <SUP>22</SUP>Na
  and <SUP>7</SUP>Be/<SUP>22</SUP>Na data and AO, NAO, AMO, QBO and SO
  teleconnection indices representing different climatic variations in
  Northern Europe. In the wavelet coherence analyses, the <SUP>7</SUP>Be
  activities were found to be mainly modulated by NAO and AMO at an
  interannual scale, while <SUP>22</SUP>Na activity was found to be
  less effected by climatic phenomena. The <SUP>7</SUP>Be coherence
  with other indices was intermittent where the coherence with SO was
  limited to Ivalo data and in the case of QBO, to Kotka data. The
  <SUP>22</SUP>Na data was not found to be in coherence with any of the
  studied indices. In the <SUP>7</SUP>Be/<SUP>22</SUP>Na ratio a clear
  seasonal pattern was observed where low <SUP>7</SUP>Be/<SUP>22</SUP>Na
  ratios were observed during summer and high ratios during winter. This
  was speculated to be caused by the height of atmospheric vertical
  mixing. During 2006-2011, the <SUP>7</SUP>Be/<SUP>22</SUP>Na
  ratios from Kotka, Kajaani and Rovaniemi showed variance at
  synoptic time scales but were nearly identical at the seasonal
  scale. The <SUP>7</SUP>Be/<SUP>22</SUP>Na ratio was proposed to be
  a radiochronometer to estimate residence times of aerosols carrying
  <SUP>7</SUP>Be and <SUP>22</SUP>Na.

---------------------------------------------------------
Title: Cosmogenic isotope <SUP>7</SUP>Be: A case study of depositional
    processes in Rio de Janeiro in 2008-2009
Authors: Pacini, A. A.; Usoskin, I. G.; Evangelista, H.; Echer, E.;
   de Paula, R.
2011AdSpR..48..811P    Altcode:
  We present here an investigation of the depositional processes
  of <SUP>7</SUP>Be-carrying aerosols in the troposphere through an
  analysis of the isotope concentration variability measured at Rio
  de Janeiro (Brazil) during 2008 and 2009, with weekly resolution. By
  adopting a simplified description of the equilibrium scenario in the
  troposphere and combining our isotopic data with regional meteorological
  parameters and numerical CRAC:Be7 model of cosmogenic production,
  it was possible to quantitatively reproduce the observed seasonal
  variability and estimate the typical <SUP>7</SUP>Be-aerosols residence
  time in the lower troposphere ( t<SUB>r</SUB> ∼ 1 day) as well as
  the washout coefficient for each season (wet: Λ = 0.029; and dry:
  Λ = 0.023 h <SUP>-1</SUP>). These results allowed us to discuss the
  origin of the seasonal patterns of <SUP>7</SUP>Be concentrations,
  indicating that the wet deposition modulation, caused by changes in
  the regional weather condition, is the most important forcing in both
  seasons. Even an anomaly in isotopic short-term measured variability
  can be explained when a detailed air-mass dynamic is considered. Our
  results indicate that anomalous events of tropospheric dynamic, such
  as occurrence of strong downward air flux, imprint information about
  air masses 3-D movement in the near-ground air <SUP>7</SUP>Be data,
  making <SUP>7</SUP>Be a useful tracer of its peculiar dynamics at local
  and synoptic scales in the troposphere. This study, limited to a single
  location and one year time interval, illustrates the potential of the
  method. A more detailed general study is planned for the future.

---------------------------------------------------------
Title: Evolution of the solar irradiance during the Holocene
Authors: Vieira, L. E. A.; Solanki, S. K.; Krivova, N. A.; Usoskin, I.
2011A&A...531A...6V    Altcode: 2011arXiv1103.4958V
  Context. Long-term records of solar radiative output are vital for
  understanding solar variability and past climate change. Measurements
  of solar irradiance are available for only the last three decades,
  which calls for reconstructions of this quantity over longer time
  scales using suitable models. <BR /> Aims: We present a physically
  consistent reconstruction of the total solar irradiance for the
  Holocene. <BR /> Methods: We extend the SATIRE (Spectral And Total
  Irradiance REconstruction) models to estimate the evolution of the
  total (and partly spectral) solar irradiance over the Holocene. The
  basic assumption is that the variations of the solar irradiance are
  due to the evolution of the dark and bright magnetic features on the
  solar surface. The evolution of the decadally averaged magnetic flux
  is computed from decadal values of cosmogenic isotope concentrations
  recorded in natural archives employing a series of physics-based
  models connecting the processes from the modulation of the cosmic
  ray flux in the heliosphere to their record in natural archives. We
  then compute the total solar irradiance (TSI) as a linear combination
  of the jth and jth + 1 decadal values of the open magnetic flux. In
  order to evaluate the uncertainties due to the evolution of the Earth's
  magnetic dipole moment, we employ four reconstructions of the open flux
  which are based on conceptually different paleomagnetic models. <BR />
  Results: Reconstructions of the TSI over the Holocene, each valid for
  a different paleomagnetic time series, are presented. Our analysis
  suggests that major sources of uncertainty in the TSI in this model
  are the heritage of the uncertainty of the TSI since 1610 reconstructed
  from sunspot data and the uncertainty of the evolution of the Earth's
  magnetic dipole moment. The analysis of the distribution functions
  of the reconstructed irradiance for the last 3000 years, which is the
  period that the reconstructions overlap, indicates that the estimates
  based on the virtual axial dipole moment are significantly lower at
  earlier times than the reconstructions based on the virtual dipole
  moment. We also present a combined reconstruction, which represents
  our best estimate of total solar irradiance for any given time during
  the Holocene. <BR /> Conclusions: We present the first physics-based
  reconstruction of the total solar irradiance over the Holocene, which
  will be of interest for studies of climate change over the last 11 500
  years. The reconstruction indicates that the decadally averaged total
  solar irradiance ranges over approximately 1.5 W/m<SUP>2</SUP> from
  grand maxima to grand minima. <P />Appendix A is available in electronic
  form at <A href="http://www.aanda.org">http://www.aanda.org</A>The
  TSI data is only available at the CDS via anonymous
  ftp to cdsarc.u-strasbg.fr (130.79.128.5) or via <A
  href="http://cdsarc.u-strasbg.fr/viz-bin/qcat?J/A+A/531/A6">http://cdsarc.u-strasbg.fr/viz-bin/qcat?J/A+A/531/A6</A>

---------------------------------------------------------
Title: Applications and usage of the real-time Neutron Monitor
    Database
Authors: Mavromichalaki, H.; Papaioannou, A.; Plainaki, C.; Sarlanis,
   C.; Souvatzoglou, G.; Gerontidou, M.; Papailiou, M.; Eroshenko, E.;
   Belov, A.; Yanke, V.; Flückiger, E. O.; Bütikofer, R.; Parisi,
   M.; Storini, M.; Klein, K. -L.; Fuller, N.; Steigies, C. T.;
   Rother, O. M.; Heber, B.; Wimmer-Schweingruber, R. F.; Kudela, K.;
   Strharsky, I.; Langer, R.; Usoskin, I.; Ibragimov, A.; Chilingaryan,
   A.; Hovsepyan, G.; Reymers, A.; Yeghikyan, A.; Kryakunova, O.; Dryn,
   E.; Nikolayevskiy, N.; Dorman, L.; Pustil'Nik, L.
2011AdSpR..47.2210M    Altcode:
  A high-time resolution Neutron Monitor Database (NMDB) has started
  to be realized in the frame of the Seventh Framework Programme of the
  European Commission. This database will include cosmic ray data from at
  least 18 neutron monitors distributed around the world and operated in
  real-time. The implementation of the NMDB will provide the opportunity
  for several research applications most of which will be realized in
  real-time mode. An important one will be the establishment of an Alert
  signal when dangerous solar cosmic ray particles are heading to the
  Earth, resulting into ground level enhancements effects registered by
  neutron monitors. Furthermore, on the basis of these events analysis,
  the mapping of all ground level enhancement features in near real-time
  mode will provide an overall picture of these phenomena and will be used
  as an input for the calculation of the ionization of the atmosphere. The
  latter will be useful together with other contributions to radiation
  dose calculations within the atmosphere at several altitudes and will
  reveal the absorbed doses during flights. Moreover, special algorithms
  for anisotropy and pitch angle distribution of solar cosmic rays,
  which have been developed over the years, will also be set online
  offering the advantage to give information about the conditions of
  the interplanetary space. All of the applications will serve the
  needs of the modern world which relies at space environment and will
  use the extensive network of neutron monitors as a multi-directional
  spectrographic detector. On top of which, the decreases of the cosmic
  ray intensity - known as Forbush decreases - will also be analyzed and
  a number of important parameters such as galactic cosmic ray anisotropy
  will be made available to the users of NMDB. A part of the NMDB project
  is also dedicated to the creation of a public outreach website with the
  scope to inform about cosmic rays and their possible effects on humans,
  technological systems and space-terrestrial environment. Therefore,
  NMDB will also stand as an informative gate on space research through
  neutron monitor’s data usage.

---------------------------------------------------------
Title: VizieR Online Data Catalog: Evolution of solar irradiance
    during Holocene (Vieira+, 2011)
Authors: Vieira, L. E. A.; Solanki, S. K.; Krivova, N. A.; Usoskin, I.
2011yCat..35310006V    Altcode: 2011yCat..35319006V
  This is a composite total solar irradiance (TSI) time series for 9495BC
  to 2007AD constructed as described in Sect. 3.3 of the paper. Since
  the TSI is the main external heat input into the Earth's climate
  system, a consistent record covering as long period as possible
  is needed for climate models. This was our main motivation for
  constructing this composite TSI time series. <P />In order to
  produce a representative time series, we divided the Holocene into
  four periods according to the available data for each period. Table
  4 (see below) summarizes the periods considered and the models
  available for each period. After the end of the Maunder Minimum we
  compute daily values, while prior to the end of the Maunder Minimum
  we compute 10-year averages. For the period for which both solar disk
  magnetograms and continuum images are available (period 1) we employ
  the SATIRE-S reconstruction (Krivova et al. 2003A&amp;A...399L...1K;
  Wenzler et al. 2006A&amp;A...460..583W). SATIRE-T (Krivova et
  al. 2010JGRA..11512112K) reconstruction is used from the beginning of
  the Maunder Minimum (approximately 1640AD) to 1977AD. Prior to 1640AD
  reconstructions are based on cosmogenic isotopes (this paper). Different
  models of the Earth's geomagnetic field are available before and after
  approximately 5000BC. Therefore we treat periods 3 and 4 (before and
  after 5000BC) separately. Further details can be found in the paper. We
  emphasize that the reconstructions based on different proxies have
  different time resolutions. <P />(1 data file).

---------------------------------------------------------
Title: Global analysis of active longitudes of sunspots
Authors: Zhang, L.; Mursula, K.; Usoskin, I.; Wang, H.
2011A&A...529A..23Z    Altcode:
  Context. Active longitudes have been found in various manifestations
  of solar activity. The longitudinal distribution of, e.g., sunspots
  and solar X-ray flares shows two persistent preferred longitudes
  separated by roughly 180 degrees. We previously studied solar X-ray
  flares using an improved version of a dynamic, differentially rotating
  coordinate system and found enhanced rotational asymmetry and rotation
  parameter values that are consistent for the three classes of X-ray
  flares. <BR /> Aims: We aim to find the optimal values of rotation
  parameters of active longitudes of sunspots for several different
  time intervals and separately for the two solar hemispheres. <BR />
  Methods: We perform a global study of the longitudinal location of
  sunspots (all sunspots and first appearance sunspots) using a refined
  version of a dynamic, differentially rotating coordinate system. <BR
  /> Results: We find that the rotation parameters for sunspots are in
  good agreement with those obtained for X-ray flares using the same
  method. The improved method typically finds somewhat faster equatorial
  rotation with better accuracy. The improved treatment also leads to
  a larger non-axisymmetry. Rotation parameters for all sunspots and
  first appearances closely agree with each other, but non-axisymmetry
  is systematically larger for all sunspots than for first appearances,
  suggesting that strong fields follow more closely the pattern of active
  longitudes. The refined method emphasizes hemispheric differences in
  rotation. Over the whole interval, the mean rotation in the southern
  hemisphere is slower than in the north. We also find significant
  temporal variability in the two rotation parameters over the 136-year
  interval. Interestingly, the long-term variations (trends and residual
  oscillations) in solar rotation are roughly the opposite in the northern
  and southern hemispheres. <BR /> Conclusions: Rotation parameters vary
  differently with time in the northern and southern hemispheres. Both
  sunspots and flares strongly suggest that the northern hemisphere
  rotated considerably faster but the southern hemisphere slightly slower
  than the Carrington rotation rate during the last three solar cycles.

---------------------------------------------------------
Title: Revisited Sunspot Data: A New Scenario for the Onset of the
    Maunder Minimum
Authors: Vaquero, José M.; Gallego, M. C.; Usoskin, Ilya G.;
   Kovaltsov, Gennady A.
2011ApJ...731L..24V    Altcode: 2011arXiv1103.1520V
  The Maunder minimum forms an archetype for the Grand minima,
  and detailed knowledge of its temporal development has important
  consequences for the solar dynamo theory dealing with long-term
  solar activity evolution. Here, we reconsider the current paradigm of
  the Grand minimum general scenario by using newly recovered sunspot
  observations by G. Marcgraf and revising some earlier uncertain data
  for the period 1636-1642, i.e., one solar cycle before the beginning
  of the Maunder minimum. The new and revised data dramatically change
  the magnitude of the sunspot cycle just before the Maunder minimum,
  from 60-70 down to about 20, implying a possibly gradual onset of
  the minimum with reduced activity started two cycles before it. This
  revised scenario of the Maunder minimum changes, through the paradigm
  for Grand solar/stellar activity minima, the observational constraint
  on the solar/stellar dynamo theories focused on long-term studies and
  occurrence of Grand minima.

---------------------------------------------------------
Title: A review of Space Climate and an introduction to the papers
    of the JASTP special issue on Space Climate
Authors: Mursula, Kalevi; Marsh, Dan; Nandy, Dibyendu; Usoskin, Ilya
2011JASTP..73..179M    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: Global analysis of active longitudes of solar X-ray flares
Authors: Zhang, L.; Mursula, K.; Usoskin, I.; Wang, H.
2011JASTP..73..258Z    Altcode:
  There is increasing evidence that various manifestations of solar
  activity are non-axisymmetric and mainly occur in two preferred
  longitude ranges, so called active longitudes. We have earlier
  analyzed the longitudinal occurrence of solar X-ray flares observed
  by GOES satellites using a specially developed dynamic, differentially
  rotating coordinate system. In this frame, the longitude distribution
  shows two persistent preferred longitudes separated by about 180
  degrees whose strength alternates in time according to the so called
  flip-flop phenomenon. Here we make the first global statistical
  analysis to find the best fitting values for parameters describing
  the differential rotation of active longitudes of X-ray flares. We
  find that the new analysis greatly improves the earlier values for
  the rotation parameters, making them consistent between the three
  different classes of X-ray flares. The improved parameters also yield
  a systematically higher level of non-axisymmetry for the longitudinal
  distribution, thus increasing the statistical significance of the
  existence of active longitudes. Accordingly, a significant amount of
  X-ray flares of different classes are produced by the same two active
  longitudes. We also find a significant difference between the rotation
  rates in the two solar hemispheres, with active longitudes rotating
  faster than the Carrington rate in the northern hemisphere and slower
  than the Carrington rate in the southern hemisphere.

---------------------------------------------------------
Title: Solar modulation parameter for cosmic rays since 1936
    reconstructed from ground-based neutron monitors and ionization
    chambers
Authors: Usoskin, Ilya G.; Bazilevskaya, Galina A.; Kovaltsov,
   Gennady A.
2011JGRA..116.2104U    Altcode:
  The differential energy spectrum of galactic cosmic rays near
  Earth is often parameterized by the force field model with the only
  time-dependent parameter, the modulation potential $\phi$. Here we
  present a series of reconstructed monthly values of the modulation
  potential for the period from July 1936 through December 2009. This
  works extends our earlier study by employing new data and improving
  the reconstruction method. The presented series is a composite of three
  parts. The most reliable part is based on data from the world network of
  sea level neutron monitors and covers the period since April 1964. The
  part between February 1951 and March 1964 is based on data from one
  to two mountain neutron monitors of IGY type and is characterized by
  larger uncertainties and possible systematic error. The part related
  to the period before 1951 is based on data from Forbush ground-based
  ionization chambers and is characterized by large uncertainties and
  should be taken with caveats. The reconstructed series has been tested
  against long-term data of balloon-borne measurements of flux of cosmic
  ray ionizing radiation in the stratosphere performed by the Lebedev
  Institute since 1957. The comparison shows good agreement since 1964
  but suggests that the result before 1964 may contain larger errors
  in that the NM-based reconstruction method may underestimate the low
  energy part of GCR spectrum.

---------------------------------------------------------
Title: Solar modulation of cosmic rays since 1936: Neutron monitors
    and balloon-borne data
Authors: Usoskin, Ilya
2011ICRC...11...39U    Altcode: 2011ICRC...32k..39U
  No abstract at ADS

---------------------------------------------------------
Title: Numerical model of cosmic ray induced ionization in the
atmosphere CRAC:CRII
Authors: Usoskin, Ilya
2011ICRC...11..343U    Altcode: 2011ICRC...32k.343U
  No abstract at ADS

---------------------------------------------------------
Title: Long term Solar/heliospheric variability
Authors: Usoskin, Ilya
2011ICRC...12..131U    Altcode: 2011ICRC...32l.131U
  No abstract at ADS

---------------------------------------------------------
Title: Long-term variation of solar surface differential rotation
Authors: Zhang, L.; Mursula, K.; Usoskin, I.; Wang, H.; Du, Z.
2011ASInC...2..175Z    Altcode:
  Recently, the surface differential rotation parameters were found to
  vary differently with time for the northern and southern hemispheres of
  the Sun. Both sunspots and flares strongly suggest that the northern
  hemisphere rotated considerably faster than the southern during the
  last three solar cycles, showing a strong north-south asymmetry in
  solar surface rotation. In order to study the long-term variation of
  solar surface differential rotation, the location of sunspots during
  1877-2009 is analyzed <P />separately in the two hemispheres. The
  variation of the rotation of the northern hemisphere is found to have an
  anti-correlation with that of the southern hemisphere and the variation
  suggests a period of 10-12 cycles.

---------------------------------------------------------
Title: Cosmic rays and climate forcing .
Authors: Usoskin, I. G.
2011MmSAI..82..937U    Altcode:
  An important factor affecting the terrestrial environment is the
  flux of cosmic rays permanently impinging on Earth. Energetic cosmic
  rays initiate a nucleonic-electromagnetic cascade in the atmosphere,
  affecting its physical-chemical properties. In particular, cosmic
  rays form the dominant source of ionization in the lower and middle
  atmosphere. Therefore, a detailed knowledge of processes leading to the
  cosmic ray induced ionization makes a solid basis for a quantitative
  study of the outer space influence upon Earth. Via the variable
  heliospheric modulation of cosmic rays, this provides an indirect
  solar-terrestrial link. <P />We present here a review of atmospheric
  effects of cosmic rays, including ionization and aerosol particle
  formation. Both physical modeling and phenomenological relations are
  considered on different time scales.

---------------------------------------------------------
Title: Cosmogenic <SUP>7</SUP>Be in air: A complex mixture of
    production and transport
Authors: Leppänen, A. -P.; Pacini, A. A.; Usoskin, I. G.; Aldahan,
   A.; Echer, E.; Evangelista, H.; Klemola, S.; Kovaltsov, G. A.; Mursula,
   K.; Possnert, G.
2010JASTP..72.1036L    Altcode:
  The long-time series of <SUP>7</SUP>Be activity in surface air have
  been studied with the wavelet analysis technique in order to find
  coherence between <SUP>7</SUP>Be activity, theoretical production
  in the troposphere and climatic indices. The <SUP>7</SUP>Be activity
  were obtained from five different locations, Angra in the tropics in
  Brazil, Skåne in mid-latitudes in Southern Sweden, Kiruna in Polar
  region in Northern Sweden, Loviisa in Southern Finland and Rovaniemi
  in polar region in Northern Finland. The <SUP>7</SUP>Be data from the
  Northern hemisphere sites where tested for coherence with theoretical
  production of the isotope in troposphere and with the North Atlantic
  Oscillation index. In the Southern hemisphere separate theoretical
  production was calculated in order to describe local production and
  Southern Annular Mode was used as the climatic index. Consistent and
  significant coherence were found with theoretical production at Skåne,
  Kiruna and Loviisa at time-scales of four years or longer. At Angra
  and Rovaniemi sites, no coherence was detected between <SUP>7</SUP>Be
  theoretical tropospheric production and measured activity at ground
  level. The coherence between <SUP>7</SUP>Be data from Skåne and
  Angra and climatic indices is insignificant while data from Northern
  and Eastern Scandinavia show clear coherence with climatic indices
  at time-scales of four years or longer. Additionally, significant
  coherence was found between the cosmic ray induced production and NAO
  at the time band of 8-12 years whereas the coherence between cosmic
  ray induced production and SAM was insignificant. This feature implies
  that the ground level <SUP>7</SUP>Be activity contain mixed information
  on both production and transport. This conclusion means that further
  evaluation through models which enable accurate realistic models that
  will be investigated in future studies.

---------------------------------------------------------
Title: Fluctuations of energetic particle flux during solar cycle
    based on measurements in the solar wind, in the magnetosphere,
    and at Earth
Authors: Starodubtsev, S. A.; Usoskin, I. G.
2010AstL...36..438S    Altcode: 2010PAZh...36..462S
  We present the results of our studies of the cosmic-ray fluctuations
  in the frequency range 10<SUP>-4</SUP>-1.67 × 10<SUP>-3</SUP> Hz
  based on energetic particle flux measurements on spacecraft in the
  solar wind, in the magnetosphere, and at Earth in the 11-year solar
  cycle. The cosmic-ray fluctuation spectrum is shown to have an 11-year
  modulation related to the solar cycle. A different behavior of the
  level of energetic particle fluctuations measured in different regions
  of space is observed for cosmic rays of different origins. We conclude
  that the new, previously unknown phenomenon of 11-year modulation of
  the cosmic-ray fluctuation spectrum has been established. A possible
  explanation of this phenomenon is given.

---------------------------------------------------------
Title: Cosmic ray induced ionization model CRAC:CRII: An extension
    to the upper atmosphere
Authors: Usoskin, Ilya G.; Kovaltsov, Gennady A.; Mironova, Irina A.
2010JGRD..11510302U    Altcode:
  A new version of the CRAC:CRII model computing ionization induced by
  cosmic rays in the atmosphere is presented, which is extended to the
  upper atmosphere and can be now applied to the entire atmosphere. The
  model is able to compute the ionization rate in the atmosphere at
  any given location and time provided the energy spectrum of incoming
  cosmic rays is known. It is discussed that the use of earlier models,
  either analytical or Monte Carlo, with the limited upper energy of
  500 MeV, is well validated for the upper atmosphere (above a few
  g/cm<SUP>2</SUP> atmospheric depth, which corresponds to the altitude
  about 40 km) to study the effect of solar energetic particles but may
  lead to a significant underestimate of the background ionization due
  to galactic cosmic rays. The use of a full model accounting for the
  atmospheric cascade and full energy range of incoming cosmic rays,
  rather than earlier simplified models, is recommended to study the
  ionization effects of galactic cosmic rays in the upper atmosphere. On
  the other hand, transient strong effects of solar energetic particle
  events can be studied using truncated models.

---------------------------------------------------------
Title: A new 3D numerical model of cosmogenic nuclide <SUP>10</SUP>Be
    production in the atmosphere
Authors: Kovaltsov, Gennady A.; Usoskin, Ilya G.
2010E&PSL.291..182K    Altcode:
  A new quantitative model of production of the cosmogenic isotope
  <SUP>10</SUP>Be by cosmic rays in the Earth's atmosphere is
  presented. The CRAC:10Be (Cosmic Ray induced Atmospheric Cascade
  for <SUP>10</SUP>Be) model is based on a full numerical Monte-Carlo
  simulation of the nucleonic-electromagnetic-muon cascade induced by
  cosmic rays in the atmosphere and is able to compute the isotope's
  production rate at any given 3D location (geographical and altitude)
  and time, for all possible parameters including solar energetic particle
  events. The model was tested against the results of direct measurements
  of the <SUP>10</SUP>Be production in a number of dedicated experiments
  to confirm its quantitative correctness. A set of tabulated values
  for the yield function is provided along with a detailed numerical
  recipe forming a "do-it-yourself" kit, which allows anyone interested
  to apply the model for any given conditions. This provides a useful
  tool for applying the cosmogenic isotope method in direct integration
  with other models, e.g., dynamical atmospheric transport.

---------------------------------------------------------
Title: Solar modulation in surface atmospheric electricity
Authors: Giles Harrison, R.; Usoskin, Ilya
2010JASTP..72..176G    Altcode:
  The solar wind modulates the flux of galactic cosmic rays impinging
  on Earth inversely with solar activity. Cosmic ray ionisation is the
  major source of air's electrical conductivity over the oceans and well
  above the continents. Differential solar modulation of the cosmic
  ray energy spectrum modifies the cosmic ray ionisation at different
  latitudes, varying the total atmospheric columnar conductance. This
  redistributes current flow in the global atmospheric electrical circuit,
  including the local vertical current density and the related surface
  potential gradient. Surface vertical current density and potential
  gradient measurements made independently at Lerwick Observatory,
  Shetland, from 1978 to 1985 are compared with modelled changes in
  cosmic ray ionisation arising from solar activity changes. Both the
  lower troposphere atmospheric electricity quantities are significantly
  increased at cosmic ray maximum (solar minimum), with a proportional
  change greater than that of the cosmic ray change.

---------------------------------------------------------
Title: Sunspot cycles and Grand Minima
Authors: Sokoloff, Dmitry; Arlt, Rainer; Moss, David; Saar, Steven H.;
   Usoskin, Ilya
2010IAUS..264..111S    Altcode:
  Observational data concerning the long-term history of cyclic solar
  activity as recorded in sunspot and isotopic data are discussed in the
  context of solar dynamo theory. In particular, a simple dynamo model
  based on differential rotation and the mirror asymmetry of convection
  with random fluctuations of dynamo governing parameters is shown to
  reproduce some basic features of the solar magnetic activity evolution.

---------------------------------------------------------
Title: Atmospheric data over a solar cycle: no connection between
    galactic cosmic rays and new particle formation
Authors: Kulmala, M.; Riipinen, I.; Nieminen, T.; Hulkkonen, M.;
   Sogacheva, L.; Manninen, H. E.; Paasonen, P.; Petäjä, T.; Dal Maso,
   M.; Aalto, P. P.; Viljanen, A.; Usoskin, I.; Vainio, R.; Mirme, S.;
   Mirme, A.; Minikin, A.; Petzold, A.; Hõrrak, U.; Plaß-Dülmer, C.;
   Birmili, W.; Kerminen, V. -M.
2010ACP....10.1885K    Altcode: 2009ACPD....921525K
  Aerosol particles affect the Earth's radiative balance by directly
  scattering and absorbing solar radiation and, indirectly, through
  their activation into cloud droplets. Both effects are known
  with considerable uncertainty only, and translate into even bigger
  uncertainties in future climate predictions. More than a decade ago,
  variations in galactic cosmic rays were suggested to closely correlate
  with variations in atmospheric cloud cover and therefore constitute
  a driving force behind aerosol-cloud-climate interactions. Later,
  the enhancement of atmospheric aerosol particle formation by ions
  generated from cosmic rays was proposed as a physical mechanism
  explaining this correlation. Here, we report unique observations on
  atmospheric aerosol formation based on measurements at the SMEAR II
  station, Finland, over a solar cycle (years 1996-2008) that shed new
  light on these presumed relationships. Our analysis shows that none
  of the quantities related to aerosol formation correlates with the
  cosmic ray-induced ionisation intensity (CRII). We also examined the
  contribution of ions to new particle formation on the basis of novel
  ground-based and airborne observations. A consistent result is that
  ion-induced formation contributes typically significantly less than
  10% to the number of new particles, which would explain the missing
  correlation between CRII and aerosol formation. Our main conclusion is
  that galactic cosmic rays appear to play a minor role for atmospheric
  aerosol formation events, and so for the connected aerosol-climate
  effects as well.

---------------------------------------------------------
Title: Critical Comment on the Article by R. Rek “The Maunder
    Minimum and the Sun as the Possible Source of Particles Creating
    Increased Abundance of the <SUP>14</SUP>C Carbon Isotope”
Authors: Usoskin, I. G.; Kovaltsov, G. A.
2010SoPh..261..353U    Altcode: 2010SoPh..tmp...10U
  Several strong but erroneous statements were made by R. Rek in an
  article published in this volume of Solar Physics. Here we show that
  these misleading statements are caused by neglecting the known effects
  of the carbon cycle and misinterpretation of the data. In particular we
  show that the claim of the Maunder minimum being "the period without a
  significant cessation of activity" contradicts the bulk of observational
  evidence and is caused by the misinterpretation of proxy data.

---------------------------------------------------------
Title: Study of air mass dynamics using beryllium-7 data from Rio
    de Janeiro State
Authors: Pacini, Alessandra; Usoskin, Ilya; Evangelista, Heitor;
   de Paula, Raquel; Echer, Ezequiel
2010cosp...38..166P    Altcode: 2010cosp.meet..166P
  We present here a study of the atmospheric 7 Be inter-annual
  variability measured at Rio de Janeiro (Brazil) and its relation to
  local air mass dynamics. 7 Be is a cosmogenic isotope (produced by
  the spallation of atmospheric oxygen and nitrogen by cosmic rays)
  with the half-life of 53.2 days. Atmospheric concentration of this
  cosmogenic radionuclide is highest around 20 km above the surface and
  decreases with the altitude. After its production in the atmosphere,
  the 7 Be gets attached predominantly to small aerosols and follows
  their transport and deposition process. Therefore, temporal variations
  of the near-surface atmospheric 7 Be can provide information on the
  air mass dynamics, stratosphere-troposphere coupling and cosmic ray
  variations. Considering that the production variability is expected
  to be small at this location and timescale, we concentrate on the
  influence of the atmospheric dynamics and the local climatic upon our
  isotopic data. The 7 Be concentration time series was obtained by our
  team through nearly continuous weekly air sampling made since August
  2008 in Rio de Janeiro (22° 33'S 43° 18'W; Pc=10,89 GV). We have
  compared our measured isotopic data with the local climatic indices
  (temperature, barometric pressure and precipitation) to understand
  the seasonal behavior. In addition, we have applied two theoretical
  models to identify the origin of some 7 Be anomalies in our data. Using
  these models together we could calculate the 7 Be production (using
  the CRAC:Be7 model) in each point of the air sample path (the air mass
  back trajectories was calculated using the HYSPLIT model) before the
  measurement. Our results show that, during its movement (vertical or
  horizontal) into the low atmosphere, the traced air sample experiences
  consequent enrichments and losses of the isotopic concentration,
  imprinting this information over the surface 7 Be data, and making it
  an useful tracer of the atmospheric dynamics.

---------------------------------------------------------
Title: WWW.NMDB.EU: The real-time Neutron Monitor databas
Authors: Klein, Karl-Ludwig; Steigies, Christian; Steigies, Christian
   T.; Wimmer-Schweingruber, Robert F.; Kudela, Karel; Strharsky, Igor;
   Langer, Ronald; Usoskin, Ilya; Ibragimov, Askar; Flückiger, Erwin
   O.; Bütikofer, Rolf; Eroshenko, Eugenia; Belov, Anatoly; Yanke,
   Victor; Klein, Karl-Ludwig; Fuller, Nicolas; Mavromichalaki, Helen;
   Papaioannou, Athana-Sios; Sarlanis, Christos; Souvatzoglou, George;
   Plainaki, Christina; Geron-Tidou, Maria; Papailiou, Maria-Christina;
   Mariatos, George; Chilingaryan, Ashot; Hovsepyan, G.; Reymers, Artur;
   Parisi, Mario; Kryakunova, Olga; Tsepakina, Irina; Nikolayevskiy,
   Nikolay; Dor-Man, Lev; Pustil'Nik, Lev; García-Población, Oscar
2010cosp...38.1685K    Altcode: 2010cosp.meet.1685K
  The Real time database for high-resolution neutron monitor
  measurements(NMDB), which was supported by the 7th Framework
  Programme of the European Commission, hosts data on cosmic rays in
  the GeV range from European and some non-European neutron monitor
  stations. Besides real-time data and historical data over several
  decades in a unified format, it offers data products such as galactic
  cosmic ray spectra and applications including solar energetic particle
  alerts and the calculation of ionisation rates in the atmosphere and
  effective radiation dose rates at aircraft altitudes. Furthermore
  the web site comprises public outreach pages in several languages
  and offers training material on cosmic rays for university students
  and researchers and engineers who want to become familiar with cosmic
  rays and neutron monitor measurements. This contribution presents an
  overview of the provided services and indications on how to access the
  database. Operators of other neutron monitor stations are welcome to
  submit their data to NMDB.

---------------------------------------------------------
Title: Modelling of Cosmic Ray Induced Ionization of Low and Middle
Atmosphere: A Review
Authors: Usoskin, Ilya; Kovaltsov, Gennady
2010cosp...38.1330U    Altcode: 2010cosp.meet.1330U
  Cosmic rays form the main source of the atmospheric ionization in low
  and middle atmosphere. A major progress has been recently achieved
  in numerical modelling of this process, basing on a full Monte-Carlo
  simulation of the complicated cascade initiated by cosmic rays in the
  atmosphere. Here we present an overview of the current state of the art
  in modelling of cosmic ray induced ionization. We discuss the existing
  models and approaches, their inter-comparison, range of validity,
  advantages and missing points. We also perform an extensive comparison
  between model simulations and direct measurements and provide practical
  recommendation for a correct choice of the model parameters.

---------------------------------------------------------
Title: Regional millennial trend in the cosmic ray induced ionization
    of the troposphere
Authors: Usoskin, I. G.; Mironova, I. A.; Korte, M.; Kovaltsov, G. A.
2010JASTP..72...19U    Altcode:
  Long-term trends in the tropospheric cosmic ray induced ionization on
  the multi-millennial time scale are studied using the newly released
  paleomagnetic reconstruction models. Spatial and temporal variations of
  the tropospheric ionization has been computed using the CRAC:CRII model
  and applying the paleomagnetic CALS7k.2 reconstruction. It has been
  shown that long-term variations of the tropospheric ionization are not
  spatially homogeneous, and they are defined not only by solar (i.e.,
  covariant with solar irradiance) changes but also by the geomagnetic
  field. The dominance of the two effects is geographically separated,
  which makes it possible to distinguish between direct and indirect
  solar-terrestrial climate effects. Possible climate applications
  are considered.

---------------------------------------------------------
Title: A new 3D numerical model for production of cosmogenic
    spallation products (7) Be, (10) Be, (22) Na in the atmosphere
Authors: Usoskin, Ilya; Kovaltsov, Gennady
2010cosp...38.1754U    Altcode: 2010cosp.meet.1754U
  A new quantitative model of production of the cosmogenic isotopes,
  produced by spallation of atmospheric constitutes by the nucleonic
  component of cosmic rays induced cascade in the Earth's atmosphere
  is presented. We presents the results for three cosmogenic isotopes:
  7 Be, 10 Be and 22 Na, using the CRAC (Cosmic Ray induced Atmospheric
  Cascade) model is based on a full numerical Monte-Carlo simulation of
  the nucleonic-electromagnetic-muon cascade induced by cosmic rays in
  the atmosphere and is able to compute the isotope's production rate
  at any given 3D location (geographical and altitude) and time, for all
  possible parameters including solar energetic particle events. The model
  was tested against the results of direct measurements of production
  of 10 Be and 7 Be in a number of dedicated experiments to confirm
  its quantitative correctness. A set of tabulated values for the yield
  function is provided along with a detailed numerical recipe forming a
  `do-it-yourself' kit, which allows anyone interested to apply the model
  for any given conditions. This provides a useful tool for applying
  the cosmogenic isotope method in direct integration with other models,
  e.g., dynamical atmospheric transport.

---------------------------------------------------------
Title: Can the solar proxies -cloud cover relationship be mediated
    by internal climatic oscillations?
Authors: Voiculescu, Mirela; Usoskin, Ilya
2010cosp...38.1720V    Altcode: 2010cosp.meet.1720V
  Significant correlations have been found at global level between
  different types of cloud cover and ultraviolet irradiance (UVI),
  and respectively cosmic ray induced ionization (CRII). Clouds play
  an important role in climate changes as a major contributor to the
  Earth's radiation budget. Accordingly, the background conditions when
  the cloud-solar relation can contribute to climate change need to
  be studied as thoroughly as possible. In our previous work we have
  shown that different solar drivers seem to play different roles
  in the occurrence of clouds at different altitudes. We found that
  the response of clouds to solar drivers is complex, as expected,
  but different mechanisms might be at work at different timescales,
  depending on cloud characteristics (height and formation) as well as
  on general climatic background, geographical position, latitude and
  season. On the other hand, it has been shown that solar signal can be
  noticed in different teleconnection indices, as for instance NAO. We aim
  here at investigating the complicated spatial and temporal relationship
  between teleconnection indices (NAO), cloud cover and solar variability
  (CR or UVI based).

---------------------------------------------------------
Title: Variability of Cosmic Ray Induced Ionization Relevant to
Climate: A Review
Authors: Usoskin, Ilya
2010cosp...38.1718U    Altcode: 2010cosp.meet.1718U
  Despite numerous correlative studies relating climatic changes on Earth
  to solar variability on different time scales, a physical mechanism
  responsible for this is still poorly known. A possible link connecting
  solar activity and climate variations is related to cosmic rays and
  the physical-chemical changes they produce in the atmosphere. We
  review experimental evidence and theoretical grounds for this
  relation. We concentrate on two time scales where the effect of cosmic
  rays can be disentangled from direct solar effects: long-term scale
  (centennial-millennia) and very short time scale (days). We also try to
  estimate the expected effect. The cosmic ray-climate link seems to be
  a plausible climate driver which operates on different time scales, but
  its exact mechanism and relative importance still remain open questions.

---------------------------------------------------------
Title: Unusual features of solar cycle 23: cosmic rays and solar
    wind turbulence.
Authors: Starodubtsev, Sergey; Grigoryev, Vladislav; Usoskin, Ilya;
   Mursula, Kalevi; Kovaltsov, Gennady
2010cosp...38.1679S    Altcode: 2010cosp.meet.1679S
  We have analyzed the energetic part of the spectrum of solar wind
  turbulence in the frequency range between 2.2 · 10-6 and 1.39 ·
  10-4 Hz for the last four solar cycles (1964-2009). We have shown
  that the turbulence spectrum of the last cycle No.23 is essentially
  different from the three preceding ones Ns.20-22. While the mean power
  of fluctuations was roughly constant for the interplanetary magnetic
  field strength as well as for the velocity and density of solar wind
  plasma, the level of small-scale irregularities of the solar wind was,
  and still remains, greatly reduced. We discuss implications of these
  peculiar features for the observed variations of cosmic ray intensities
  during the solar cycle No.23.

---------------------------------------------------------
Title: Cosmogenic isotope beryllium-7 in the atmosphere: Production
    versus transport
Authors: Pacini, Alessandra; Usoskin, Ilya; Evangelista, Heitor;
   Echer, Ezequiel; Mursula, Kalevi; Leppanen, Ari-Pekka
2010cosp...38..165P    Altcode: 2010cosp.meet..165P
  Cosmogenic isotope 7 Be measured near the ground can provide
  information about its produc-tion (that occurs in the atmosphere
  due to the interaction of cosmic rays and atmospheric constituents)
  and its deposition processes (that involves air mass dynamics,
  stratosphere-troposphere coupling and local climatic conditions). We
  present the results of an investigation of the atmospheric 7 Be
  temporal variations at different geographic locations (Finland and
  Brazil). This study was based on an analysis of three time series
  of 7 Be concentration measured in near-surface air samples from
  Rovaniemi and Loviisa (Finland) and Rio de Janeiro (Brazil) for the
  last decades. We made use of the wavelet spectral method to identify the
  frequency-temporal features of the 7 Be temporal variations that allowed
  us to determine the relative importance of production and deposition
  process for the observed data. By comparing these time series with
  climatic indices and the values of 7 Be concentration expected from
  the model for the same period, we found that the climate system is the
  main driver of the surface isotopic modulation, while the imprints of
  the production variations are geographically dependent. Thus,7 Be can
  be considered a good tool to monitor the large-scale air mass dynamics.

---------------------------------------------------------
Title: Effect of an extreme solar energetic particle event of January
    20, 2005 on polar stratospheric aerosols
Authors: Mironova, Irina; Usoskin, Ilya; Kovaltsov, Gennady; Randall,
   Cora
2010cosp...38.1350M    Altcode: 2010cosp.meet.1350M
  This work is an extension of a phenomenological study of the middle
  polar atmosphere response to a severe solar energetic particle (SEP)
  event of January 20, 2005. The present work is focused on evaluation
  of the potential influence of atmospheric ionization caused by solar
  cosmic rays upon formation of aerosol particles in the low stratosphere
  over the polar regions. We have performed a thorough analysis of
  variations of the daily profiles of aerosol extinction as measured
  by the POAM III instrument in different wavelengths for both North
  and South polar regions during January 2005. We found statistically
  significant changes in the aerosol parameters associated with the
  SEP event that are stronger in the South hemisphere (local austral
  summer). The changes are mostly related to ultra-fine and fine aerosols
  and show no effect for larger particles.

---------------------------------------------------------
Title: Ionization of low and middle atmosphere caused by strong
    solar particle events
Authors: Usoskin, Ilya; Mironova, Irina; Tylka, Allan J.; Kovaltsov,
   Gennady; Dietrich, William F.
2010cosp...38.1343U    Altcode: 2010cosp.meet.1343U
  We quantitatively evaluate the possible ionization effect in the low and
  middle atmosphere for the major GLEs (Ground Level Enhancements) of the
  last five solar cycles. Reconstruction of the energy spectrum of solar
  protons was done based on fits to measurements from ground-based and
  satellite-borne instruments covering a wide energy range. Computations
  of the atmospheric ionization are based on the numerical 3D CRAC:CRII
  model. We show that the direct ionization effect of GLE is negligible or
  even negative, due to the accompanying Forbush decreases, in all low-and
  mid-latitude regions. The ionization effect is positive only in polar
  atmosphere, where it can be dramatic in the upper atmosphere during
  major GLE events but quickly fades downwards. We present a Table of
  the net ionization effect for all major GLEs of the last solar cycles.

---------------------------------------------------------
Title: Atmospheric Data over a Solar Cycle: No Connection between
    Galactic Cosmic Rays and Particle Formation in Boreal Forest
Authors: Riipinen, I.; Kulmala, M. T.; Nieminen, T.; Hulkkonen, M.;
   Sogacheva, L.; Manninen, H.; Paasonen, P.; Petdjd, T. T.; Dal Maso,
   M.; Aalto, P.; Viljanen, A.; Usoskin, I.; Vainio, R. O.; Mirme, S.;
   Mirme, A.; Minikin, A.; Petzold, A.; Horrak, U.; Plass-Duelmer, C.;
   Birmili, W.; Kerminen, V.
2009AGUFM.A13B0207R    Altcode:
  Aerosol particles affect the Earth’s radiative balance by
  directly scattering and absorbing solar radiation and, indirectly,
  through their activation into cloud droplets. Both effects are known
  with considerable uncertainty only, and translate into even bigger
  uncertainties in future climate predictions. More than a decade ago,
  variations in galactic cosmic rays were suggested to closely correlate
  with variations in atmospheric cloud cover and therefore constitute
  a driving force behind aerosol-cloud-climate interactions. Later,
  the enhancement of atmospheric aerosol particle formation by ions
  generated from cosmic rays was proposed as a physical mechanism
  explaining this correlation. Here, we report unique observations on
  atmospheric aerosol formation based on measurements at the SMEAR II
  station, Finland, over a solar cycle (years 1996-2008) that shed new
  light on these presumed relationships. Our analysis shows that none
  of the quantities related to aerosol formation correlates with the
  cosmic ray-induced ionisation intensity (CRII, see Fig. 1). We also
  examined the contribution of ions to new particle formation on the
  basis of novel ground-based and airborne observations. A consistent
  result is that ion-induced formation contributes typically less than
  10% to the number of new particles, which would explain the missing
  correlation between CRII and aerosol formation. Our main conclusion is
  that galactic cosmic rays appear to play a minor role for atmospheric
  aerosol formation, and so for the connected aerosol-climate effects
  as well. Figure 1. Particle formation events and CRII at the SMEAR II
  station in Hyytiälä, Finland during 1996-2008.

---------------------------------------------------------
Title: Does sunspot number calibration by the “magnetic needle”
    make sense?
Authors: Mursula, K.; Usoskin, I.; Yakovchouk, O.
2009JASTP..71.1717M    Altcode:
  It has been suggested recently that early sunspot numbers should be
  re-calibrated and significantly corrected using the observed daily
  range of the geomagnetic declination (so-called rY values). The
  suggested "correction" method makes an a priori detrending of
  the rY series and then extends the linear regression between rY
  and sunspot numbers established for the last 25 years to earlier
  times. The suggested "correction" of sunspot numbers by roughly
  30% goes far beyond the traditional estimates of observational
  uncertainties of sunspots. Concentrating here on Zürich sunspot
  numbers (Rz), we demonstrate that the rY values do not actually imply
  that the observed Rz values in the 19th century are systematically
  underestimated. Rather, we find that the Rz numbers are fairly uniform
  after mid-19th century. The suggested "correction" is largely induced
  by the detrending of the rY series, which enhances the rY-based sunspot
  activity in the 19th century relative to later times. We also show
  that while the annually averaged declinations have a rough relation
  between sunspots and other related solar parameters, this relation
  is strongly seasonally dependent and, therefore, not sufficiently
  accurate or uniform to allow annually averaged rY values to be used
  as a very reliable proxy of solar activity in early times.

---------------------------------------------------------
Title: Dynamics of the Earth's Particle Radiation Environment
Authors: Vainio, Rami; Desorgher, Laurent; Heynderickx, Daniel;
   Storini, Marisa; Flückiger, Erwin; Horne, Richard B.; Kovaltsov,
   Gennady A.; Kudela, Karel; Laurenza, Monica; McKenna-Lawlor, Susan;
   Rothkaehl, Hanna; Usoskin, Ilya G.
2009SSRv..147..187V    Altcode:
  The physical processes affecting the dynamics of the Earth’s particle
  radiation environment are reviewed along with scientific and engineering
  models developed for its description. The emphasis is on models that
  are either operational engineering models or models presently under
  development for this purpose. Three components of the radiation
  environment, i.e., galactic cosmic rays (GCRs), solar energetic
  particles (SEPs) and trapped radiation, are considered separately. In
  the case of SEP models, we make a distinction between statistical
  flux/fluence models and those aimed at forecasting events. Models
  of the effects of particle radiation on the atmosphere are also
  reviewed. Further, we summarize the main features of the models and
  discuss the main outstanding issues concerning the models and their
  possible use in operational space weather forecasting. We emphasize
  the need for continuing the development of physics-based models of
  the Earth’s particle radiation environment, and their validation
  with observational data, until the models are ready to be used for
  nowcasting and/or forecasting the dynamics of the environment.

---------------------------------------------------------
Title: History of cosmic ray research in Finland
Authors: Usoskin, I. G.; Valtonen, E.; Vainio, R.; Tanskanen, P. J.;
   Aurela, A. M.
2009AdSpR..44.1232U    Altcode:
  The history of cosmic ray research in Finland can be traced back to
  the end of 1950s, when first ground-based cosmic ray measurements
  started in Turku. The first cosmic ray station was founded in
  Oulu in 1964 performing measurements of cosmic rays by a muon
  telescope, which was later complemented by a neutron monitor. Since
  the 1990s, several research centers and universities, such as The
  Finnish Meteorological Institute, Helsinki University of Technology,
  University of Oulu, University of Turku and University of Helsinki have
  been involved in space science projects, such as SOHO, AMS, Cluster,
  Cassini, BepiColombo, etc. At the same time, ground-based cosmic ray
  measurements have reached a new level, including a fully automatic
  on-line database in Oulu and a new muon measuring underground site
  in Pyhäsalmi. Research groups in Helsinki, Oulu and Turku have also
  extensive experience in theoretical investigations of different aspects
  of cosmic ray physics. Cosmic ray research has a 50-year long history
  in Finland, covering a wide range from basic long-running ground-based
  observations to high-technology space-borne instrumentation and
  sophisticated theoretical studies. Several generations of researchers
  have been involved in the study ensuring transfer of experience and
  building the recognized Finnish research school of cosmic ray studies.

---------------------------------------------------------
Title: A Solar Cycle Lost in 1793-1800: Early Sunspot Observations
    Resolve the Old Mystery
Authors: Usoskin, Ilya G.; Mursula, Kalevi; Arlt, Rainer; Kovaltsov,
   Gennady A.
2009ApJ...700L.154U    Altcode: 2009arXiv0907.0063U
  Because of the lack of reliable sunspot observations, the quality of
  the sunspot number series is poor in the late 18th century, leading
  to the abnormally long solar cycle (1784-1799) before the Dalton
  minimum. Using the newly recovered solar drawings by the 18-19th
  century observers Staudacher and Hamilton, we construct the solar
  butterfly diagram, i.e., the latitudinal distribution of sunspots
  in the 1790s. The sudden, systematic occurrence of sunspots at high
  solar latitudes in 1793-1796 unambiguously shows that a new cycle
  started in 1793, which was lost in the traditional Wolf sunspot
  series. This finally confirms the existence of the lost cycle that
  has been proposed earlier, thus resolving an old mystery. This Letter
  brings the attention of the scientific community to the need of revising
  the sunspot series in the 18th century. The presence of a new short,
  asymmetric cycle implies changes and constraints to sunspot cycle
  statistics, solar activity predictions, and solar dynamo theories,
  as well as for solar-terrestrial relations.

---------------------------------------------------------
Title: Correction to “Stochastic simulation of cosmic ray modulation
    including a wavy heliospheric current sheet”
Authors: Alanko-Huotari, K.; Usoskin, I. G.; Mursula, K.; Kovaltsov,
   G. A.
2009JGRA..114.3101A    Altcode: 2009JGRA..11403101A
  <A href="/journals/ja/ja0903/2008JA013919/">Abstract Available</A>
  from <A href="http://www.agu.org">http://www.agu.org</A>

---------------------------------------------------------
Title: On the common solar signal in different cosmogenic isotope
    data sets
Authors: Usoskin, Ilya G.; Horiuchi, Kazuho; Solanki, Sami; Kovaltsov,
   Gennady A.; Bard, Edouard
2009JGRA..114.3112U    Altcode: 2009JGRA..11403112U
  In this article, we aim to determine frequency ranges and intervals
  of time in which the solar signal dominates in different cosmogenic
  isotope data. From a <SUP>14</SUP>C-based reconstruction of cosmic ray
  intensity over the last millennia, we computed expected <SUP>10</SUP>Be
  variations in two Antarctic sites (Dom Fuji and South Pole) and two
  Greenland sites (Dye-3 and GISP-2) and compared them with the actually
  measured <SUP>10</SUP>Be abundance at the sites. By applying different
  methods of analysis, such as bivariate correlation, conventional
  FFT coherence, and wavelet coherence, we found the following: (1)
  The modeled series, on the basis of <SUP>14</SUP>C data, are in good
  agreement with the measured <SUP>10</SUP>Be data sets, on different
  timescales and at different locations, confirming the existence of a
  common solar signal in both isotope data. (2) The <SUP>10</SUP>Be data
  are driven by the solar signal on timescales from about 100 years up
  to 1000 years or even to multimillennial scales (at the longer scales,
  paleomagnetism plays an increasingly important role). (3) The local
  climate dominates the <SUP>10</SUP>Be data mostly on short (&lt;100
  years) timescales, but the solar signal becomes important even at short
  scales during periods of Grand minima of solar activity. (4) There is an
  indication of a possible systematic uncertainty in the early Holocene,
  likely due to a not-perfectly-stable thermohaline circulation, which
  requires additional studies. We have shown that both <SUP>14</SUP>C- and
  <SUP>10</SUP>Be-based records are consistent with each other over a wide
  range of timescales and time intervals. They form a robust basis for
  quantitative reconstructions of solar activity variations in the past.

---------------------------------------------------------
Title: Ionization of the earth's atmosphere by solar and galactic
    cosmic rays
Authors: Usoskin, Ilya G.; Desorgher, Laurent; Velinov, Peter; Storini,
   Marisa; Flückiger, Erwin O.; Bütikofer, Rolf; Kovaltsov, Gennady A.
2009AcGeo..57...88U    Altcode: 2008AcGeo..57...88U; 2008AcGeo.tmp...40U
  A brief review of the research of atmospheric effects of cosmic
  rays is presented. Numerical models are discussed, that are capable
  to compute the cosmic ray induced ionization at a given location
  and time. Intercomparison of the models, as well as comparison with
  fragmentary direct measurements of the atmospheric ionization, validates
  their applicability for the entire atmosphere and the whole range of the
  solar activity level variations. The effect of sporadic solar energetic
  particle events is shown to be limited on the global scale, even for
  the most severe event, but can be very strong locally in polar regions,
  affecting the physical-chemical properties of the upper atmosphere,
  especially at high altitudes. Thus, a new methodology is presented to
  study cosmic ray induced ionization of the atmosphere in full detail
  using realistic numerical models calibrated to direct observations.

---------------------------------------------------------
Title: Grand Minima of Solar Activity and the Mean-Field Dynamo
Authors: Usoskin, I. G.; Sokoloff, D.; Moss, D.
2009SoPh..254..345U    Altcode:
  We demonstrate that a simple solar dynamo model, in the form of
  a Parker migratory dynamo with random fluctuations of the dynamo
  governing parameters and algebraic saturation of dynamo action, can
  at least qualitatively reproduce all the basic features of solar
  Grand Minima as they are known from direct and indirect data. In
  particular, the model successfully reproduces such features as an
  abrupt transition into a Grand Minimum and the subsequent gradual
  recovery of solar activity, as well as mixed-parity butterfly
  diagrams during the epoch of the Grand Minimum. The model predicts
  that the cycle survives in some form during a Grand Minimum, as well
  as the relative stability of the cycle inside and outside of a Grand
  Minimum. The long-term statistics of simulated Grand Minima appears
  compatible with the phenomenology of the Grand Minima inferred from
  the cosmogenic isotope data. We demonstrate that such ability to
  reproduce the Grand Minima phenomenology is not a general feature of
  the dynamo models but requires some specific assumption, such as random
  fluctuations in dynamo governing parameters. In general, we conclude
  that a relatively simple and straightforward model is able to reproduce
  the Grand Minima phenomenology remarkably well, in principle providing
  us with a possibility of studying the physical nature of Grand Minima.

---------------------------------------------------------
Title: A History of Solar Activity over Millennia
Authors: Usoskin, Ilya G.
2008LRSP....5....3U    Altcode: 2008arXiv0810.3972U
  Presented here is a review of present knowledge of the long-term
  behavior of solar activity on a multi-millennial timescale, as
  reconstructed using the indirect proxy method.

---------------------------------------------------------
Title: Variations of aerosol optical properties during the extreme
    solar event in January 2005
Authors: Mironova, I. A.; Desorgher, L.; Usoskin, I. G.; Flückiger,
   E. O.; Bütikofer, R.
2008GeoRL..3518610M    Altcode:
  We present the results of analysis of the aerosol optical depth
  variations for January 2005 when an extreme solar energetic particle
  event occurred leading to a greatly enhanced flux of energetic particles
  penetrating into the atmosphere. An increase of the concentration
  of sulfate or nitrate aerosol was found on the second day after the
  solar energetic particle event in the south magnetic pole region
  with the maximum penetration of anisotropic solar cosmic rays. This
  suggests that an enhanced flux of solar energetic particles can lead
  to notable changes in the chemical and physical properties of the polar
  troposphere. A statistical test confirms that the observed change of the
  aerosol index is significant and is unlikely to be related to a spatial
  or temporal independent fluctuation of the aerosol content. Thus, the
  results of the present work provide evidence of a direct influence of
  cosmic rays on physical-chemical properties of the atmosphere.

---------------------------------------------------------
Title: Solar Grand Minima and Random Fluctuations in Dynamo Parameters
Authors: Moss, D.; Sokoloff, D.; Usoskin, I.; Tutubalin, V.
2008SoPh..250..221M    Altcode: 2008arXiv0806.3331M; 2008SoPh..tmp..101M
  We consider to what extent the long-term dynamics of cyclic solar
  activity in the form of Grand Minima can be associated with random
  fluctuations of the parameters governing the solar dynamo. We consider
  fluctuations of the alpha coefficient in the conventional Parker
  migratory dynamo, and also in slightly more sophisticated dynamo
  models, and demonstrate that they can mimic the gross features of the
  phenomenon of the occurrence of Grand Minima over suitable parameter
  ranges. The temporal distribution of these Grand Minima appears chaotic,
  with a more or less exponential waiting time distribution, typical of
  Poisson processes. In contrast, however, the available reconstruction of
  Grand Minima statistics based on cosmogenic isotope data demonstrates
  substantial deviations from this exponential law. We were unable to
  reproduce the non-Poissonic tail of the waiting time distribution
  either in the framework of a simple alpha-quenched Parker model or in
  its straightforward generalization, nor in simple models with feedback
  on the differential rotation. We suggest that the disagreement may
  only be apparent and is plausibly related to the limited observational
  data, and that the observations and results of numerical modeling can
  be consistent and represent physically similar dynamo regimes.

---------------------------------------------------------
Title: Forbush decreases of cosmic rays: Energy dependence of the
    recovery phase
Authors: Usoskin, I. G.; Braun, I.; Gladysheva, O. G.; HöRandel,
   J. R.; JäMséN, T.; Kovaltsov, G. A.; Starodubtsev, S. A.
2008JGRA..113.7102U    Altcode: 2008JGRA..11307102U
  Cause and general shape of Forbush decreases of cosmic rays
  are relatively well understood, however, the knowledge of their
  recovery times remains rather poor. Earlier results of theoretical
  and fragmentary statistical studies are in disagreement whether
  the recovery time does or does not depend on the energy of cosmic
  rays. A thorough empirical study of the recovery phase of strong
  isolated Forbush decreases is presented here, based on the ground
  based data from the World Neutron Monitor Network since 1964 and three
  ground based muon telescopes since 1973. In total 39 strong Forbush
  decreases, suitable for the analysis, have been identified for the
  period 1964-2006, 24 of them depicting a clear energy dependence of
  the recovery time and 15 consistent with no energy dependence. All
  analyzed Forbush decreases with magnitudes exceeding 10% demonstrate
  an energy dependence of the recovery time, while smaller events can
  be of either type. No apparent relation between the occurrence of
  energy dependent/independent recovery and the IMF polarity has been
  found. This result provides an observational constraint for more
  detailed modeling of the propagation of interplanetary transients and
  their dynamic effects on cosmic ray transport.

---------------------------------------------------------
Title: Cosmic Ray Induced Ion Production in the Atmosphere
Authors: Bazilevskaya, G. A.; Usoskin, I. G.; Flückiger, E. O.;
   Harrison, R. G.; Desorgher, L.; Bütikofer, R.; Krainev, M. B.;
   Makhmutov, V. S.; Stozhkov, Y. I.; Svirzhevskaya, A. K.; Svirzhevsky,
   N. S.; Kovaltsov, G. A.
2008SSRv..137..149B    Altcode: 2008SSRv..tmp...44B
  An overview is presented of basic results and recent developments
  in the field of cosmic ray induced ionisation in the atmosphere,
  including a general introduction to the mechanism of cosmic ray
  induced ion production. We summarize the results of direct and indirect
  measurements of the atmospheric ionisation with special emphasis to
  long-term variations. Models describing the ion production in the
  atmosphere are also overviewed together with detailed results of
  the full Monte-Carlo simulation of a cosmic ray induced atmospheric
  cascade. Finally, conclusions are drawn on the present state and further
  perspectives of measuring and modeling cosmic ray induced ionisation
  in the terrestrial atmosphere.

---------------------------------------------------------
Title: Reconstruction Of Grand Minima Of Solar Activity On
    Multi-Millennial Time Scale
Authors: Usoskin, I.
2008AGUSMGP31C..05U    Altcode:
  Using a reconstruction of sunspot numbers stretching over multiple
  millennia, we analyze the statistics of the occurrence of grand minima
  and maxima and set new observational constraints on long-term solar
  and stellar dynamo models. We present an updated reconstruction of
  sunspot number over multiple millennia, from 14C data by means of
  a physics-based model, using an updated model of the evolution of
  the solar open magnetic flux. A list of grand minima and maxima of
  solar activity is presented for the Holocene (since 9500 BC) and
  the statistics of both the length of individual events as well as
  the waiting time between them are analyzed. The occurrence of grand
  minima/maxima appears to be driven not by long-term cyclic variability,
  but by a stochastic/chaotic process. The waiting time distribution
  of the occurrence of grand minima/maxima deviates from an exponential
  distribution, implying that these events tend to cluster together with
  long event-free periods between the clusters. Two different types
  of grand minima are observed: short (30-90 years) minima of Maunder
  type and long (&gt;110 years) minima of Spörer type, implying that a
  deterministic behaviour of the dynamo during a grand minimum defines
  its length. The duration of grand maxima follows an exponential
  distribution, suggesting that the duration of a grand maximum is
  determined by a random process.

---------------------------------------------------------
Title: Does sunspot number calibration by the "magnetic needle"
    make sense?
Authors: Mursula, K.; Usoskin, I.; Yakovchouk, O.
2008AGUSMSP23A..06M    Altcode:
  It has been suggested recently that early sunspot numbers should be
  re-calibrated and significantly corrected using the observed daily
  range of the geomagnetic inclination (so called rY values). The
  suggested "correction" method makes an a priori detrending of the rY
  series and then extends the linear regression between rY and sunspot
  numbers established for the last 25 years to earlier times. The
  suggested "correction" of sunspot numbers by roughly 30% goes far
  beyond the traditional estimates of observational uncertainties
  of sunspots. Concentrating here on international sunspot numbers
  (Rz), we demonstrate that the rY values do not actually imply
  that the observed Rz values in the 19th century are systematically
  underestimated. Rather, we find that the Rz numbers are fairly uniform
  after mid-19th century. The suggested "correction" is largely induced
  by the detrending of the rY series, which enhances the rY-based sunspot
  activity in the 19th century relative to later times. We also show
  that while the annually averaged declinations have a rough relation
  between sunspots and other related solar parameters, this relation
  is strongly seasonally dependent and nonlinear and, therefore, not
  sufficiently accurate or uniform for rY to be used as a very reliable
  proxy of solar activity in early times.

---------------------------------------------------------
Title: Role of centennial geomagnetic changes in local atmospheric
    ionization
Authors: Usoskin, I. G.; Korte, M.; Kovaltsov, G. A.
2008GeoRL..35.5811U    Altcode:
  Many studies of solar-terrestrial relation are based on globally (or
  hemispherically) averaged quantities, including the average cosmic ray
  flux. However, regional effects of cosmic ray induced ionization due to
  geomagnetic changes may be comparable to or even dominate over the solar
  signal at mid-latitudes on centennial-to-millennial time scales. We show
  that local changes of the tropospheric ionization due to fast migration
  of the geomagnetic axis are crucial on centennial time scale, and the
  use of global averages may smear an important effect. We conclude that
  changes of the regional tropospheric ionization at mid-latitudes are
  defined by both geomagnetic changes and solar activity, and none of the
  two processes can be neglected. This substantiates a necessity for a
  careful analysis of the regional, not global, indices at mid-latitudes
  and offers a new possibility to disentangle direct (solar radiation) and
  indirect (via cosmic rays) effects in the solar-terrestrial relations.

---------------------------------------------------------
Title: Cosmic Ray Induced Ion Production in the Atmosphere
Authors: Bazilevskaya, G. A.; Usoskin, I. G.; Flückiger, E. O.;
   Harrison, R. G.; Desorgher, L.; Bütikofer, R.; Krainev, M. B.;
   Makhmutov, V. S.; Stozhkov, Y. I.; Svirzhevskaya, A. K.; Svirzhevsky,
   N. S.; Kovaltsov, G. A.
2008pae..book..149B    Altcode:
  An overview is presented of basic results and recent developments
  in the field of cosmic ray induced ionisation in the atmosphere,
  including a general introduction to the mechanism of cosmic ray
  induced ion production. We summarize the results of direct and indirect
  measurements of the atmospheric ionisation with special emphasis to
  long-term variations. Models describing the ion production in the
  atmosphere are also overviewed together with detailed results of
  the full Monte-Carlo simulation of a cosmic ray induced atmospheric
  cascade. Finally, conclusions are drawn on the present state and further
  perspectives of measuring and modeling cosmic ray induced ionisation
  in the terrestrial atmosphere.

---------------------------------------------------------
Title: Forbush decreases: Energy dependence of the recovery
Authors: Usoskin, Ilya G.; Kovaltsov, Gennady A.; Gladysheva, Olga G.;
   Jämsén, Teppo
2008ICRC....1..327U    Altcode: 2008ICRC...30a.327U
  We presented a statistical study of major Forbush decreases during
  the last decades, using cosmic ray data from ground based detectors
  -- neutron monitors and a muon detector. We show that, in addition to
  typical event (e.g., September 2005), there are several unusual Forbush
  decreases (e.g., November 2004), which depict unexpected features:
  (1) the recovery time of a Forbush decrease strongly depends on the
  mean response energy of the detector; (2) an over-recovery is observed
  in the most energetic cosmic ray data (muon detector). Such a behavior
  is not expected from the standard theory of a Forbush decrease. Here
  we suggest a simple qualitative scenario for the observed phenomenon.

---------------------------------------------------------
Title: Numerical Model of Cosmic Ray Induced Ionization in the
    Atmosphere
Authors: Usoskin, Ilya G.; Kovaltsov, Gennady A.
2008ICRC....1..705U    Altcode: 2008ICRC...30a.705U
  We present a physical model to calculate cosmic ray induced ionization
  in the atmosphere. The model is based on the Monte-Carlo CORSIKA tool,
  which simulates full development of an electromagnetic-muon-nucleonic
  cascade in the atmosphere, with the FLUKA package used for low energy
  interactions. The model is applicable to the entire atmosphere,
  from the ground up to the stratosphere. A comparison to fragmentary
  direct measurements of the ionization in the atmosphere confirms the
  validity of the model in the whole range of geographical latitudes and
  altitudes. We provide a detailed recipe to compute easily the cosmic
  ray induced ionization for given location, altitude and the spectrum of
  cosmic rays. This provides a new tool for a quantitative study of the
  space weather influence upon the Earth's environment. Some practical
  applications are discussed.

---------------------------------------------------------
Title: Rapid cosmic ray fluctuations in real-time during the SEP
    events in December 2006
Authors: Starodubtsev, S. A.; Grigoryev, A. V.; Usoskin, I. G.;
   Mursula, K.
2008ICRC....1..135S    Altcode: 2008ICRC...30a.135S
  Cosmic ray fluctuations with the periods less than 3 h by data
  of the EPAM/LEMS120 aboard ACE spacecraft are studied. It is shown
  that the frequency spectra of cosmic rays undergo significant dynamic
  changes caused by the presence of fast magnetosonic waves in the solar
  wind. Evidences of generation of fast magnetosonic waves by the SEP
  fluxes have been found.

---------------------------------------------------------
Title: Grand minima and maxima of solar activity on multi-millennial
    scale
Authors: Usoskin, Ilya; Solanki, Sami; Kovaltsov, Gennady
2008cosp...37.3264U    Altcode: 2008cosp.meet.3264U
  Using a reconstruction of sunspot numbers stretching over multiple
  millennia, we analyze the statistics of the occurrence of grand minima
  and maxima and set new observational constraints on long-term solar
  and stellar dynamo models. We present an updated reconstruction of
  sunspot number over multiple millennia, from 14C data by means of
  a physics-based model, using an updated model of the evolution of
  the solar open magnetic flux. A list of grand minima and maxima of
  solar activity is presented for the Holocene (since 9500 BC) and
  the statistics of both the length of individual events as well as
  the waiting time between them are analyzed. It is discussed that the
  occurrence of grand minima/maxima is driven not by long-term cyclic
  variability, but by a stochastic/chaotic process. The waiting time
  distribution of the occurrence of grand minima/maxima deviates from an
  exponential distribution, implying that these events tend to cluster
  together with long event-free periods between the clusters. Two
  different types of grand minima are observed: short (30-90 years)
  minima of Maunder type and long (&gt;110 years) minima of Sp¨rer type,
  implying that a deterministic behaviour of the dynamo during o a grand
  minimum defines its length. The duration of grand maxima follows an
  exponential distribution, suggesting that the duration of a grand
  maximum is determined by a random process.

---------------------------------------------------------
Title: Fluctuations of cosmic rays and IMF in the vicinity of
    interplanetary shocks
Authors: Grigoryev, A. V.; Starodubtsev, S. A.; Grigoryev, V. G.;
   Usoskin, I. G.; Mursula, K.
2008AdSpR..41..955G    Altcode:
  Fluctuations of cosmic rays and interplanetary magnetic field upstream
  of interplanetary shocks are studied using data of ground-based polar
  neutron monitors as well as measurements of energetic particles and
  solar wind plasma parameters aboard the ACE spacecraft. It is shown
  that coherent cosmic ray fluctuations in the energy range from 10 keV
  to 1 GeV are often observed at the Earth’s orbit before the arrival
  of interplanetary shocks. This corresponds to an increase of solar
  wind turbulence level by more than the order of magnitude upstream
  of the shock. We suggest a scenario where the cosmic ray fluctuation
  spectrum is modulated by fast magnetosonic waves generated by flux of
  low-energy cosmic rays which are reflected and/or accelerated by an
  interplanetary shock.

---------------------------------------------------------
Title: Stochastic simulation of cosmic ray modulation: Effect of a
    wavy HCS
Authors: Usoskin, Ilya G.; Alanko-Huotari, Katja; Mursula, Kalevi;
   Kovaltsov, Gennady A.
2008ICRC....1..459U    Altcode: 2008ICRC...30a.459U
  We present a new method to include a wavy heliospheric current sheet
  into a 2D numerical model of the heliospheric transport of galactic
  cosmic rays. Since the wavy current sheet has essentially 3D structure,
  we have developed an approach of averaging the corresponding drift
  effect over all longitudes for an axisymmetric model. First, an
  analytical solution is found for the flat sheet, this model then is
  applied to a wavy sheet assuming its local quasi-flatness. We study
  cosmic ray modulation in different solar modulation conditions and
  waviness of the current sheet. We discuss changes in the cosmic ray
  spectrum and the dominant streaming patterns of cosmic rays in the
  heliosphere for different solar polarities and HCS tilt angles.

---------------------------------------------------------
Title: Role of centennial geomagnetic changes in local atmospheric
    ionization
Authors: Usoskin, Ilya; Korte, Monika; Kovaltsov, Gennady
2008cosp...37.3266U    Altcode: 2008cosp.meet.3266U
  Many studies of solar-terrestrial relation are based on globally (or
  hemispherically) averaged quantities, including the average cosmic ray
  flux. However, regional effects of cosmic ray induced ionization due to
  geomagnetic changes may be comparable to or even dominate over the solar
  signal at mid-latitudes on centennial-to-millennial time scales. We show
  that local changes of the tropospheric ionization due to fast migration
  of the geomagnetic axis are crucial on centennial time scale, and the
  use of global averages may smear an important effect. We conclude that
  changes of the regional tropospheric ionization at midlatitudes are
  defined by both geomagnetic changes and solar activity, and none of the
  two processes can be neglected. This substantiates a necessity for a
  careful analysis of the regional, not global, indices at mid-latitudes
  and offers a new possibility to disentangle direct (solar radiation) and
  indirect (via cosmic rays) effects in the solar-terrestrial relations.

---------------------------------------------------------
Title: Forbush decreases of cosmic rays: Does the recovery phase
    depend on energy?
Authors: Usoskin, Ilya; Braun, Isabel; Gladysheva, Olga; Hoerandel,
   J. R.; Kovaltsov, Gennady; Jamsen, Teppo; Starodubtsev, Sergei
2008cosp...37.3265U    Altcode: 2008cosp.meet.3265U
  While the cause and general shape of Forbush decreases of cosmic ray
  intesnity are relatively well understood, physical modelling of their
  recovery still remains rather poor. Earlier results of theoretical
  and fragmentary statistical studies are inconsistent in the sense
  whether the recovery time depends on the energy of cosmic rays. A
  thorough empirical study of the recovery phase of strong isolated
  Forbush decreases is presented here, based on the ground based data
  from the World Neutron Monitor Network since 1964 and three ground
  based muon telescopes since 1973. We have analyzed a total of 39 strong
  Forbush decreases. About 60% of them (24) of them depict a clear energy
  dependence of the recovery time and 15 are consistent with no energy
  dependence. The recovery rate depicts a strong energy dependence for all
  analyzed strong Forbush decreases, with a magnitude exceeding 10%, while
  smaller events can be of either type. We found no apparent relation
  between the occurrence of energy dependent/independent recovery and
  the IMF polarity. This result provides an observational constraint for
  more detailed modeling of the propagation of interplanetary transients
  and their dynamic effects on cosmic ray transport.

---------------------------------------------------------
Title: Grand Minima of solar activity : Random fluctuations in
    dynamo parameters
Authors: Usoskin, Ilya; Moss, David; Sokoloff, Dmitry
2008cosp...37.3267U    Altcode: 2008cosp.meet.3267U
  A recent statistical study of the rate and regularity of Grand Minima
  occurrence on a multimillennial time scale poses new observational
  constraints on solar dynamo theory. We consider to what extent the
  long-term dynamics of cyclic solar activity in the form of Grand Minima
  can be associated with random fluctuations of the parameters governing
  the solar dynamo. We consider fluctuations of the alpha-coefficient in
  the conventional Parker migratory dynamo, and also in slightly more
  sophisticated dynamo models, and demonstrate that they can mimic the
  principal features of the phenomenon of the occurrence of Grand Minima
  over a suitable parameter range. The temporal distribution of these
  Grand Minima appears chaotic, with a more or less exponential waiting
  time distribution, typical of Poisson processes. In contrast however,
  the available reconstruction of Grand Minima statistics based on
  cosmogenic isotope data demonstrates substantial deviations from this
  exponential law. We were unable to reproduce the non-Poissonic tail
  of the waiting time distribution either in the framework of a simple
  alpha-quenched Parker model, or in its straightforward generalization,
  nor in simple models with feedback on the differential rotation. We
  suggest that the disagreement may only be apparent and is plausibly
  related to the limited observational data, and that the observations
  and results of numerical modeling can be consistent and represent
  physically similar dynamo regimes.

---------------------------------------------------------
Title: Stochastic simulation of cosmic ray modulation including a
    wavy heliospheric current sheet
Authors: Alanko-Huotari, K.; Usoskin, I. G.; Mursula, K.; Kovaltsov,
   G. A.
2007JGRA..112.8101A    Altcode: 2007JGRA..11208101A
  We present a quasi-steady two-dimensional (axisymmetric) model of the
  heliospheric transport of galactic cosmic rays. The model is based
  on stochastic simulation techniques and includes all the modulation
  mechanisms that cosmic rays experience in the heliosphere: convection,
  adiabatic cooling, diffusion, and drifts. A special emphasis is
  given to the cosmic ray transport in the vicinity of the heliospheric
  current sheet (HCS), and a new method to calculate the wavy current
  sheet drift is presented. We study cosmic ray modulation in different
  solar modulation conditions and levels of waviness of the current
  sheet. We discuss changes in the cosmic ray spectrum and the dominant
  streaming patterns of cosmic rays in the heliosphere for different
  solar polarities and HCS tilt angles.

---------------------------------------------------------
Title: Grand minima and maxima of solar activity: new observational
    constraints
Authors: Usoskin, I. G.; Solanki, S. K.; Kovaltsov, G. A.
2007A&A...471..301U    Altcode: 2007arXiv0706.0385U
  Aims:Using a reconstruction of sunspot numbers stretching over
  multiple millennia, we analyze the statistics of the occurrence of
  grand minima and maxima and set new observational constraints on
  long-term solar and stellar dynamo models. <BR />Methods: We present
  an updated reconstruction of sunspot number over multiple millennia,
  from <SUP>14</SUP>C data by means of a physics-based model, using an
  updated model of the evolution of the solar open magnetic flux. A
  list of grand minima and maxima of solar activity is presented for
  the Holocene (since 9500 BC) and the statistics of both the length
  of individual events as well as the waiting time between them are
  analyzed. <BR />Results: The occurrence of grand minima/maxima is
  driven not by long-term cyclic variability, but by a stochastic/chaotic
  process. The waiting time distribution of the occurrence of grand
  minima/maxima deviates from an exponential distribution, implying that
  these events tend to cluster together with long event-free periods
  between the clusters. Two different types of grand minima are observed:
  short (30-90 years) minima of Maunder type and long (&gt;110 years)
  minima of Spörer type, implying that a deterministic behaviour of
  the dynamo during a grand minimum defines its length. The duration of
  grand maxima follows an exponential distribution, suggesting that the
  duration of a grand maximum is determined by a random process. <BR
  />Conclusions: These results set new observational constraints upon
  the long-term behaviour of the solar dynamo.

---------------------------------------------------------
Title: (1) Preferred longitudes in sunspot activity (2) Preferred
sunspot longitudes: non-axisymmetry and differential rotation
Authors: Usoskin, I. G.; Berdyugina, S. V.; Poutanen, J.
2007A&A...464..761U    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: Cyclic variations of the heliospheric tilt angle and cosmic
    ray modulation
Authors: Alanko-Huotari, K.; Usoskin, I. G.; Mursula, K.; Kovaltsov,
   G. A.
2007AdSpR..40.1064A    Altcode:
  Using data on cosmic ray modulation parameter since 1951, we have
  estimated the evolution of the heliospheric current sheet tilt angle
  for the period 1951-1975, i.e., 25 years before regular observations of
  the tilt angle. This estimate is based on our recent empirical model
  relating cosmic ray intensity with global heliospheric parameters. We
  propose a simple model to describe the cyclic evolution of the
  tilt angle with the solar cycle. This model agrees with available
  observational data. Using this model, we have estimated the cosmic
  ray intensity since 1710. This estimate is consistent with the results
  based on cosmogenic isotopes ( <SUP>14</SUP>C and <SUP>10</SUP>Be).

---------------------------------------------------------
Title: Long-term persistence of solar active longitudes and its
    implications for the solar dynamo theory
Authors: Usoskin, I. G.; Berdyugina, S. V.; Moss, D.; Sokoloff, D. D.
2007AdSpR..40..951U    Altcode:
  We present an overview of the observational results related to the
  existence of long-lived sunspot active longitudes. These are affected
  by the solar differential rotation. The existence of such migrating
  active longitudes imposes an important constraint on the dynamo
  theory. We review different approaches to model non-axisymmetry in
  solar dynamo models and find that, in principle, plausible mechanisms
  exist to reproduce the observed non-axisymmetry. The most favorable
  interpretation is suggested by the 'stroboscopic effect', where
  a quasi-rigidly rotating non-axisymmetric mean field can produce
  seemingly migrating active longitudes in sunspots. Other scenarios
  are less favorable but cannot yet be excluded.

---------------------------------------------------------
Title: Effect of ENSO and volcanic events on the Sun cloud link
Authors: Voiculescu, Mirela; Usoskin, Ilya; Mursula, Kalevi
2007AdSpR..40.1140V    Altcode:
  Results of correlation studies between solar proxies and clouds suggest
  that there is a solar effect on the occurrence of clouds. However, there
  is a possibility that terrestrial quasi-periodic and sporadic phenomena,
  such as ENSO and/or major volcanic eruptions, which have an effect on
  the cloud formation, may influence the results of statistical studies of
  the Sun-cloud relation. We show that removing ENSO and volcanic years
  from the full-set analysis does not alter the results. Moreover, the
  correlation between clouds of different type and two solar proxies, UV
  irradiance and cosmic ray induced ionisation, is partly improved. This
  supports the idea that the solar signal affects clouds directly. An
  interesting result relates to an area in the eastern Pacific where
  the full-set analysis showed that the relationship between clouds
  and cosmic ray induced ionization is opposite to the global one. When
  ENSO and volcanic years are removed this odd correlation disappears,
  suggesting that in this particular area, the ENSO effect prevails over
  solar effects.

---------------------------------------------------------
Title: Case study of Forbush decreases: Energy dependence of the
    recovery
Authors: Jämsén, T.; Usoskin, I. G.; Räihä, T.; Sarkamo, J.;
   Kovaltsov, G. A.
2007AdSpR..40..342J    Altcode:
  Case study is presented for three Forbush decreases in 2004-2005,
  using cosmic ray data from ground-based detectors - neutron monitors
  and a muon detector. One of them was a typical event (September 2005),
  while two other were quite unusual (November 2004 and January 2005). Two
  unusual features, not expected from the standard theory, are revealed:
  (1) the recovery time of a Forbush decrease can strongly depend on
  the energy; (2) an over-recovery is observed in the most energetic
  cosmic ray data (muon detector). A simple scenario is suggested for
  the observed phenomenon.

---------------------------------------------------------
Title: Introduction to Space Climate
Authors: Mursula, K.; Usoskin, I. G.; Maris, G.
2007AdSpR..40..885M    Altcode:
  "Space Climate" is a relatively new scientific concept, which combines
  a number of disciplines in space and atmospheric sciences under the
  common aim to better understand the long-term changes in the Sun,
  heliosphere and in the near-Earth environment. In this brief summary
  we define the contents and aims of Space Climate. We also review some
  recent findings that are discussed in the papers included in this issue
  of Advances in Space Research, noting on some problems that should
  be solved, as well as some new lines of research that could lead to
  a better understanding of some of the main questions of Space Climate.

---------------------------------------------------------
Title: Correlation between clouds at different altitudes and solar
activity: Fact or Artifact?
Authors: Usoskin, I. G.; Voiculescu, M.; Kovaltsov, G. A.; Mursula, K.
2006JASTP..68.2164U    Altcode: 2006JATP...68.2164U
  Studies of the relation between cosmic rays (CR) (solar activity) and
  atmospheric cloudiness are mostly based on the satellite ISCCP cloud
  data. However, doubts have been cast that these relations can be an
  artifact of instrumental effects, i.e., of the masking/obscuring low
  clouds by higher clouds in the satellite view. If this is the case, most
  of the earlier results based on ISCCP data would be devaluated. Here,
  we reanalyze the ISCCP cloud coverage data and its relation with the
  cosmic ray-induced ionization, and show that the correlation between
  low clouds and CR is affected by higher clouds in some geographical
  regions, but not everywhere. In turn, our results show that low
  clouds also may affect the relation of higher clouds with CR in some
  regions. Accordingly, correlation analysis can be performed only
  when the strong relation between clouds of different types is taken
  into account. In particular, studies based on global or latitudinal
  (zonally averaged) cloud data should be revised.

---------------------------------------------------------
Title: On possible drivers of Sun-induced climate changes
Authors: de Jager, Cornelis; Usoskin, Ilya
2006JASTP..68.2053D    Altcode: 2006JATP...68.2053D
  We tested the validity of two current hypotheses on the dependence of
  climate change on solar activity. One of them states that variations in
  the tropospheric temperature are caused directly by changes of the solar
  radiance (total or spectral). The other suggests that cosmic ray (CR)
  fluctuations, caused by the solar/heliospheric modulation, affect the
  climate via cloud formation. Confronting these hypotheses with seven
  different sets of the global/hemispheric temperature reconstructions
  for the last 400 years, we found that the former mechanism is in
  general more prominent than the latter. Therefore, we can conclude
  that in so far as the Sun climate connection is concerned tropospheric
  temperatures are more likely affected by variations in the UV radiation
  flux rather than by those in the CR flux.

---------------------------------------------------------
Title: Global Heliospheric Parameters and Cosmic-Ray Modulation:
    An Empirical Relation for the Last Decades
Authors: Alanko-Huotari, K.; Mursula, K.; Usoskin, I. G.; Kovaltsov,
   G. A.
2006SoPh..238..391A    Altcode: 2006SoPh..tmp...83A
  We study empirical relations between the modulation of galactic
  cosmic rays quantified in terms of the modulation potential and the
  following global heliospheric parameters: the open solar magnetic flux,
  the tilt angle of the heliospheric current sheet, and the polarity of
  the heliospheric magnetic field. We show that a combination of these
  parameters explains the majority of the modulation potential variations
  during the neutron monitor era 1951 - 2005. Two empirical models
  are discussed: a quasi-linear model and a model assuming a power-law
  relation between the modulation potential and the magnetic flux. Both
  models describe the data fairly well. These empirical models provide
  a simple tool for evaluating various cosmic-ray related effects on
  different time scales. The models can be extended backwards in time
  or used for predictions, if the corresponding global heliospheric
  variables can be independently estimated.

---------------------------------------------------------
Title: Different response of clouds to solar input
Authors: Voiculescu, Mirela; Usoskin, Ilya G.; Mursula, Kalevi
2006GeoRL..3321802V    Altcode:
  There is evidence that solar activity variations can affect the cloud
  cover at Earth. However, it is still unclear which solar driver plays
  the most important role in the cloud formation. Here we use partial
  correlations to distinguish between the effects of two solar drivers
  (cosmic rays and the UV irradiance) and the mutual relations between
  clouds at different altitudes. We find that the solar influence on
  cloud cover is not uniquely defined by one solar driver, but both seem
  to play a role depending on the climatic conditions and altitude. In
  particular, low clouds are mostly affected by UV irradiance over oceans
  and dry continental areas and by cosmic rays over some mid-high latitude
  oceanic areas and moist lands with high aerosol concentration. High
  clouds respond more strongly to cosmic ray variations, especially over
  oceans and moist continental areas. These results provide observational
  constraints on related climate models.

---------------------------------------------------------
Title: Long-term solar activity reconstructions: direct test by
    cosmogenic <SUP>44</SUP>Ti in meteorites
Authors: Usoskin, I. G.; Solanki, S. K.; Taricco, C.; Bhandari, N.;
   Kovaltsov, G. A.
2006A&A...457L..25U    Altcode:
  Aims.Long-term solar activity in the past is usually estimated from
  cosmogenic isotopes, <SUP>10</SUP>Be or <SUP>14</SUP>C, deposited in
  terrestrial archives such as ice cores and tree rings. A number of such
  reconstruction models have been proposed which differ from each other
  significantly. This approach suffers, however, from uncertainties due
  to the sensitivity of the data to several terrestrial processes. Here
  we propose a method to constrain these solar activity reconstructions
  using cosmogenic <SUP>44</SUP>Ti activity in meteorites which is
  not affected by terrestrial processes. <BR /> Methods: .We test the
  veracity of recent solar activity reconstructions using the data on
  the activity of cosmogenic isotope <SUP>44</SUP>Ti in meteorites which
  fell during the past 235 years, and provide an independent and direct
  measure of the cosmic ray flux near the Earth and allow decoupling of
  solar activity variations from terrestrial influences.<BR /> Results:
  .We demonstrate that the <SUP>44</SUP>Ti data can distinguish between
  various reconstructions of past solar activity based on cosmogenic
  isotope data in terrestrial archives, allowing unrealistic models to
  be ruled out. We also show that a model based on the sunspot number
  record is consistent with the data on <SUP>44</SUP>Ti activity in
  meteorites, thus confirming the validity of the method. In particular
  the <SUP>44</SUP>Ti data confirm significant secular variations of
  the solar magnetic flux during the last century.<BR />

---------------------------------------------------------
Title: An upper limit of sunspot activity during the Maunder minimum
Authors: Usoskin, I. G.; Kovaltsov, G. A.; Mursula, K.
2006IAUJD...8E..15U    Altcode:
  The Maunder minimum (1645-1715) is of great interest for solar activity
  studies. During that period, sunspot activity was at the very low level,
  indicating a specific state of the solar dynamo corresponding to a
  grand minimum. However, the exact level of sunspot activity during
  the Maunder minimum is still debated. The Maunder minimum period was
  amazingly well covered by sunspot data, but some of these data are
  based not on direct daily drawings/ counts of sunspots but on general
  statements on the absence of spots during long periods. Although such
  statements were done by highly qualified astronomers, this fact has led
  to speculations that the actual sunspot activity level in the earlier
  part of the Maunder minimum could have been higher than suggested in the
  group sunspot number series. Here we have estimated conservative upper
  and lower limits of sunspot activity as obtained from direct sunspot
  observation records. We use the concept of active day fraction during
  the Maunder minimum, applied to the raw information on individual daily
  observations. Establishing the relation between the sunspot activity
  and active day fraction after 1850, we have evaluated the upper limit of
  annual group sunspot number during the deep Maunder minimum (1645-1700)
  which does not exceed 4. The solar cycle in 1700-1710 has been shown to
  be tiny, below 8 in sunspot numbers. The earlier finding of a dominant
  22-year periodicity during the Maunder minimum is confirmed as well
  as the abrupt start of the minimum.

---------------------------------------------------------
Title: The modern high solar activity: How unusual is it?
Authors: Usoskin, I. G.
2006IAUJD...8E..14U    Altcode:
  The history of direct solar observations is 400-years long, but for
  many purposes longer series are needed. On the longer time scales,
  indirect proxy data like cosmogenic nuclides should be used to evaluate
  the past level of solar activity. Here I present a reconstruction
  of the solar activity on the multi-millennial time scale using
  physics-based models for the whole chain of processes between the Sun
  and Earth. The reconstructed activity depicts great variability, from
  grand minima with almost vanishing sunspot activity to grand maxima,
  when the activity was comparable to the contemporary high activity
  level. The fraction of time that the Sun spends in grand minima and
  hyper-active states is evaluated. In particular, these reconstructions
  imply that the contemporary high level of solar activity is quite
  exceptional on the multi-millennial time scale. Possible uncertainties
  of reconstructions are discussed in details, including random errors
  as well as systematic uncertainties, related, e.g., to the geomagnetic
  field model. The conclusion about the unusually high contemporary level
  of solar activity on the multi-millennial time scale is confirmed
  to be robust by using different methods. Implications for the solar
  dynamo and solar-terrestrial connections are discussed as well.

---------------------------------------------------------
Title: Solar proton events in cosmogenic isotope data
Authors: Usoskin, Ilya G.; Solanki, Sami K.; Kovaltsov, Gennady A.;
   Beer, Jürg; Kromer, Bernd
2006GeoRL..33.8107U    Altcode:
  A possible contribution of solar energetic particle events to the
  production of cosmogenic <SUP>10</SUP>Be and <SUP>14</SUP>C in the
  atmosphere is studied. The solar particle effect is negligible in
  the <SUP>14</SUP>C data, but extreme events may be detectable in
  high-resolution <SUP>14</SUP>C data. Although the overall effect
  is small in the <SUP>10</SUP>Be data, strong events may contribute
  notably on the inter-annual time scale. In combination with the
  11-year solar modulation of galactic cosmic rays, it may lead to an
  intermittent 5.5-year periodicity, which is seen in high resolution
  <SUP>10</SUP>Be data. We have identified ten episodes during 1750-1950
  when <SUP>10</SUP>Be may hold signatures of strong solar proton
  events. This opens a new possibility to study extreme solar particle
  events in the past using high resolution cosmogenic isotope data.

---------------------------------------------------------
Title: Solar activity reconstructed over the last 7000 years: The
    influence of geomagnetic field changes
Authors: Usoskin, I. G.; Solanki, S. K.; Korte, M.
2006GeoRL..33.8103U    Altcode:
  The long-term solar activity, as manifested by sunspot number,
  has been recently reconstructed on multi-millennium time scales
  by S. K. Solanki et al. (2004) from the measured concentration of
  <SUP>14</SUP>C in tree rings. The exact level of the reconstructed
  solar activity depends, however, on independently evaluated data of
  the geomagnetic dipole strength variations. Recently, a new series
  of the palaeomagnetic dipole moment reconstruction for the last 7000
  years has been presented by M. Korte and C. G. Constable (2005a) on the
  basis of a thorough analysis of global samples. The new palaeomagnetic
  series yields a systematically lower dipole moment in the past,
  compared to the earlier geomagnetic reconstructions. We have revised
  the earlier sunspot activity reconstruction since 5000 BC, using the
  new geomagnetic data series, and found that it is roughly consistent
  with the previous results during most of the period, although the
  revised sunspot number values are in general higher. Nonetheless, it
  is confirmed with the new palaeomagnetic series that the Sun spends
  only 2-3% of the time in a state of high activity, similar to the
  modern episode. This strengthens the conclusion that the modern high
  activity level is very unusual during the last 7000 years.

---------------------------------------------------------
Title: Long-term modulation of the cosmic ray fluctuation spectrum
Authors: Starodubtsev, S. A.; Usoskin, I. G.; Grigoryev, A. V.;
   Mursula, K.
2006AnGeo..24..779S    Altcode:
  Here we study the power level of rapid cosmic ray fluctuations
  in the frequency range of 10<SUP>-4</SUP>-1.67·10<SUP>-3</SUP> Hz
  (periods from 10 min to about 3 h), using measurements by space-borne
  instruments for the period since 1974. We find that the power level
  of these fluctuations varies over the solar cycle, but the phase of
  this variation depends on the energy of cosmic ray particles. While
  the power level of these fluctuations in the higher energy channels
  (corresponding to galactic cosmic rays) changes in phase with the solar
  cycle, the fluctuation level for lower energy channels (predominantly of
  solar/interplanetary origin) is roughly in an opposite phase with the
  solar cycle. The results prove conclusively that these fluctuations
  originate in the near-Earth space, excluding their atmospheric or
  magnetospheric origin. We present these new results and discuss a
  possible scenario explaining the observed energy-dependence.

---------------------------------------------------------
Title: The Solar Cycle at the Maunder Minimum Epoch
Authors: Miyahara, Hiroko; Sokoloff, Dmitry; Usoskin, Ilya G.
2006aogs....2....1M    Altcode:
  Here, we present a brief review of the current status of the Maunder
  minimum study. The Maunder minimum is considered as an example of
  occasionally occurring Grand minima, when the solar dynamo was in a
  special mode. We review available sets of direct and indirect data
  covering the period during and around the Maunder minimum. The start
  of the minimum was very abrupt and was followed by a gradual recovery
  of the activity. The data suggest that while the sunspot activity was
  greatly suppressed during the deep phase of the minimum, the cyclic
  dynamo kept working around the sunspot formation threshold level,
  leading to seemingly sporadic occurrence of sunspots. The majority of
  proxy data depict the dominant 22-year periodicity during the Maunder
  minimum with the sub-dominant 11-year cycle. The length of the cycles
  was probably slightly enhanced. We also discuss theoretical models and
  speculations concerning the solar dynamo as well as the heliosphere
  during the Maunder minimum. Comparison with other minima (Spörer and
  Dalton) suggests that these features are common.

---------------------------------------------------------
Title: Multi-millennium changes of the geomagnetic field and solar
    activity
Authors: Usoskin, I. G.; Solanki, S.; Korte, M.
2006cosp...36.2281U    Altcode: 2006cosp.meet.2281U
  The long-term solar activity has been recently reconstructed on
  the multi-millennium time scale Solanki et al Nature 431 384 2004
  from the measured concentration of radiocarbon 14 C in tree rings
  The exact level of the reconstructed solar activity depends however
  on independently evaluated data of the geomagnetic dipole strength
  variations Recently a new series of the palaeomagnetic dipole moment
  reconstruction for the last 7000 years has been presented by Korte and
  Constable Earth Plan Sci Lett 236 348 2005 on the basis of a thorough
  complex analysis of global samples The new palaeomagnetic series yields
  systematically lower dipole moment in the past compared to the earlier
  geomagnetic reconstructions We have revised the earlier sunspot activity
  reconstruction since 5000 BC using the new geomagnetic data and found
  that it is consistent with the previous results during most of the
  period although it yields a slightly higher level of the reconstructed
  sunspot activity The earlier finding on the very unusual level of the
  contemporary solar activity over the last millennia is confirmed with
  the new palaeomagnetic series The Sun spent only 2-3 of the time in
  a high activity state similar to the modern episode implying that the
  modern high activity level is very unusual during the last 7000 years On
  the other hand grand minima occupy about 12 of the time in the recent
  history of the Sun The new reconstruction allows for a comparative
  study of solar-terrestrial relations in the multi-millennium time scale

---------------------------------------------------------
Title: Cosmic ray induced ionization in the atmosphere: An improved
    model
Authors: Usoskin, I. G.; Kovaltsov, G. A.
2006cosp...36.2293U    Altcode: 2006cosp.meet.2293U
  We present a full quantitative physical model to calculate cosmic
  ray induced ionization in the atmosphere The model is based on the
  Monte-Carlo CORSIKA tool which simulates the full development of an
  electromagnetic-muon-nucleonic cascade in the atmosphere with the FLUKA
  package used for low energy interactions The model is applicable to the
  entire atmosphere from the ground up to the stratosphere A comparison
  to direct measurements of the ionization in the atmosphere confirms
  the validity of the model in the whole range of geographical latitudes
  and altitudes This provides a new tool for a quantitative study of the
  space weather influence upon the Earth s environment We apply the model
  to study the cosmic ray induced ionization on different time scales
  In particular variations of the induced ionization are calculated for
  the last centuries and show a great variability about 50 between the
  modern period and the Maunder minimum

---------------------------------------------------------
Title: Empirical relations between the cosmic ray flux and the
    heliospheric current sheet tilt angle
Authors: Alanko-Huotari, K.; Usoskin, I. G.; Mursula, K.
2006cosp...36.1972A    Altcode: 2006cosp.meet.1972A
  One of the main factors in the heliospheric modulation of galactic
  cosmic rays is the tilt angle of the heliospheric current sheet which
  is formed as an interface between the oppositely directed field lines
  of the HMF and corresponds to the heliomagnetic equator The structure
  of the current sheet is defined by the tilt angle between the magnetic
  and rotational axes of the Sun which depends on the phase of the
  solar cycle Due to the charge-dependent drift of cosmic rays along
  the current sheet variations of the tilt angle in the course of the
  solar cycle results in a notable variation of cosmic ray flux in the
  Earth s vicinity An empirical model relating the cosmic ray flux with
  such global heliospheric parameters as the tilt angle the open solar
  flux and the polarity of the heliospheric magnetic field was developed
  Inverting this model we study a possibility to evaluate the tilt angle
  in the past before its measurements Comparing the model results with
  the actual measurements of the tilt angle which have been carried out
  for the last 30 years we confirm the validity of the method Finally we
  extend our model to cover the last 55 years providing thus an estimate
  of the tilt angle for nearly 20 years before the actual measurements

---------------------------------------------------------
Title: Evidence for the generation of MHD- turbulence by energetic
    storm particles
Authors: Starodubtsev, S. A.; Grigoryev, A. V.; Usoskin, I. G.;
   Mursula, K.
2006cosp...36.1862S    Altcode: 2006cosp.meet.1862S
  Here we present a study of the MHD-turbulence generation in the IMF
  fluctuation spectrum observed in the pre-shock front region of an
  interplanetary shock We have studied 177 interplanetary shocks recorded
  aboard the ACE spacecraft between 1998 and 2003 As a result we have
  found 19 shock events when the energy density was essentially increased
  just before the front by orders of magnitude from 10 -12 to 10 -10 ergs
  cm 3 in the frequency range of 10 -4 - 3 125 10 -2 Hz i e sometimes it
  is comparable to that of the undisturbed large-scale IMF Thereby the
  field and plasma parameters remain undisturbed while considerable fluxes
  of energetic storm particles are observed We conclude that generation
  of MHD-waves and a subsequent increase of the level of small-scale
  turbulence in the pre-front range are caused by these storm particles

---------------------------------------------------------
Title: Link Between Cosmic Rays and Clouds on Different Time Scales
Authors: Usoskin, Ilya G.; Kovaltsov, Gennady A.
2006aogs....2..321U    Altcode:
  A possible mechanism of solar variability influence upon the
  Earth's climate is related to a link between the cosmic ray flux and
  cloudiness. Here we review evidences relating terrestrial climate
  variability to changes of cosmic ray flux in the Earth's vicinity on
  different time scales. On daily scales, major For-bush decreases and
  solar energetic particle events can affect the cyclogenesis in sub-polar
  regions. At inter-annual scales, a significant correlation between low
  clouds and cosmic ray induced ionization has been found. Different
  climate reconstructions depict a correlation with variations of the
  geomagnetic field intensity throughout the last millennia, providing
  additional support to a systematic effect of cosmic rays. On very
  long time scales, a close relation was reported between the global
  climate and variations of cosmic ray flux expected from local galactic
  environment changes. Although none of these facts alone is conclusive,
  in the aggregate they strongly support the link between cosmic rays and
  climate on Earth. These links are based on phenomenological relations,
  and theoretical development and experimental investigation of this
  hypothesis is ongoing.

---------------------------------------------------------
Title: Link between solar activity and cloud cover: Fact or artifact?
Authors: Voculescu, M.; Usoskin, I. G.; Kovaltsov, G. A.; Mursula, K.
2006cosp...36.2291V    Altcode: 2006cosp.meet.2291V
  While it is commonly accepted that the solar activity affects the
  Earth climate the exact driving process is still not identified An
  important potential driver is a link between cosmic rays and cloud
  cover suggested on the basis of extensive correlation studies of cosmic
  rays solar activity and atmospheric cloudiness Such studies are mostly
  based on the satellite ISCCP cloud data However doubts have been cast
  that these relations can be an artifact of instrumental effects i e of
  the masking obscuring the low clouds by higher clouds in the satellite
  view If this is the case most of the earlier results based on ISCCP data
  would be devaluated Here we re-analyze the ISCCP cloud coverage data and
  its relation with the cosmic ray induced ionization and show that the
  correlation between low clouds and cosmic rays is affected by higher
  clouds in some geographical regions but it is not a global feature In
  turn our results show that low clouds also may affect the relation of
  higher clouds with cosmic rays in some regions Accordingly correlation
  analysis can be performed only when the strong relation between clouds
  of different types is taken into account In particular studies based
  on global or latitudinal zonally averaged cloud data should be revised

---------------------------------------------------------
Title: What do we know about the link between cosmic rays and climate?
Authors: Usoskin, I. G.
2006cosp...36.2287U    Altcode: 2006cosp.meet.2287U
  Although there is a general agreement that the solar activity affects
  the Earth s climate details are still missing One of the potential
  mechanisms of the solar variability influence upon the Earth s climate
  is via the cosmic ray flux bombarding the Earth s atmosphere that can
  affect the cloud formation Here we review different pieces of evidence
  relating the terrestrial climate variability to changes of cosmic
  ray flux in the Earth s vicinity on different time scales On daily
  scales there are hints on the instantaneous relation between short term
  variations of cosmic rays and either the cloud amount vorticity indices
  At inter-annual scales impressing correlation between low clouds and
  cosmic ray induced ionization has been found but it appears significant
  only in some geographical areas Although a link between solar activity
  and climate seems plausible on millennial time scale only a marginal
  correlation between palaeoclimatic data and geomagnetic field variations
  supports the idea of cosmic ray influence On very long time scales a
  close relation was reported between the global climate and variations of
  cosmic ray flux expected from changes in the local galactic environment
  However large uncertainties make this result only indicative Although
  none of these facts alone is conclusive in the aggregate they support
  the link between cosmic rays and the Earth s climate These results
  are based on phenomenological relations and theoretical development
  and experimental investigation of this hypothesis is ongoing

---------------------------------------------------------
Title: Variations of cosmic ray flux: From decades to millennia
Authors: Usoskin, I. G.; Kovaltsov, G. A.
2006cosp...36.2282U    Altcode: 2006cosp.meet.2282U
  Galactic cosmic rays are subject to modulation in the heliosphere
  because of different processes e g diffusion convection and adiabatic
  deceleration in solar wind with frozen-in magnetic field as well as
  charge-dependent drift effects While sophisticated theoretical models
  have been developed corresponding to advanced understanding of the
  modulation process they can be hardly applied to the past when only very
  limited and mostly indirect information exists on the solar heliospheric
  parameters In this case special efforts should be taken to study the
  modulation We apply such methods based on reasonable simplification
  and coarsening of full models to the study of heliospheric modulation
  at different time scales and discuss the main heliospheric parameters
  of the cosmic ray modulation We present some results of the long-term
  modulation study covering the time scales from a solar cycle to the
  millennial scale

---------------------------------------------------------
Title: Fluctuations of cosmic rays and IMF in the vicinity of an
    interplanetary shock
Authors: Starodubtsev, S. A.; Grigoryev, A. V.; Usoskin, I. G.;
   Mursula, K.
2006cosp...36..902S    Altcode: 2006cosp.meet..902S
  Fluctuations of IMF and cosmic rays in the pre-front region of
  interplanetary shocks are studied using direct measurements of the solar
  wind parameters and cosmic ray intensity onboard the ACE spacecraft as
  well as cosmic rays at ground based polar stations It is shown that
  coherent fluctuations of cosmic ray flux in the energy range between
  100 keV and 1 GeV are observed during energetic storm particles ESP
  events This is typically accompanied by an increase of the level of
  the solar wind turbulence by an order of magnitude on the average We
  conclude that the cosmic ray fluctuation spectrum is modulated by fast
  magnetosonic waves generated by strong fluxes of ESP in the pre-front
  region of an interplanetary shock

---------------------------------------------------------
Title: Establishing a Cosmic Ray Station and Other Space Research
    Facilities in Ethiopia
Authors: Damtie, B.; Bosinger, T.; Usoskin, I.
2006AfrSk..10...29D    Altcode:
  This paper describes the potential of Ethiopia in establishing
  space research facilities and conducting collaborative research and
  training. It also describes the goals and objectives of a proposed
  cosmic ray station in Ethiopia which would greatly improve the
  abilities of the existing worldwide network for heliospheric and
  cosmic ray research. The station will be located at the geomagentic
  equator, which is a very unique place for geomagnetic and heliospheric
  studies. Moreover, the paper presents an overview of the research and
  training activities in space physics and the successful collaborative
  project between Ethiopia and Finland, which facilitated the installation
  of a pulsation magnetometer and a photometer at Entoto Mountain in a
  suburb of the Ethiopian capital, Addis Ababa.

---------------------------------------------------------
Title: Cosmic ray spectrum during Forbush decreases: Ground based
    observations
Authors: Jämsen, T.; Usoskin, I. G.; Sakramo, J.; Kovaltsov, G. A.
2006cosp...36.2298J    Altcode: 2006cosp.meet.2298J
  Strong shocks propagating in the interplanetary medium sweep out
  energetic cosmic rays leading to Forbush decreases of the cosmic ray
  intensity Studying the cosmic ray spectrum during the times of Forbush
  decreases would provide a tool for probing large scale interplanetary
  irregularities However since the Forbush decreases are short transient
  phenomena there is lack of information on detailed direct measurements
  of the cosmic ray spectrum especially in the high energy range Here we
  analyze the spectrum indirectly using simultaneous continuous cosmic ray
  measurements in 2003-2005 at the ground in two nearby sites in Finland
  by a neutron monitor in Oulu and by a muon scintillator detector in
  Pyhasalmi Data from other neutron monitors are also used We showed
  that the shock which sweeps out particles of all energies the fast
  active phase of the Forbush decrease soon becomes transparent for high
  energy particles leading to a faster recovery of more energetic cosmic
  rays In some cases we observed a post-increase of cosmic rays in the
  muon data the cosmic ray level at a late recovery phase exceeds the
  pre-increase level We discussed some implications of the present study
  in terms of the shocks development and interaction with cosmic rays

---------------------------------------------------------
Title: Active longitudes, nonaxisymmetric dynamos and phase mixing
Authors: Berdyugina, S. V.; Moss, D.; Sokoloff, D.; Usoskin, I. G.
2006A&A...445..703B    Altcode:
  We discuss the problem of solar active longitudes from the viewpoint
  of dynamo theory. We start from a recent observational analysis of the
  problem undertaken by Berdyugina &amp; Usoskin (2003, A&amp;A, 405,
  1121) and Usoskin et al. (2005, A&amp;A, 441, 347) who demonstrated
  from a study of sunspot data that solar active longitudes rotate
  differentially, with a small but significant asynchrony between
  northern and southern hemispheres. We suggest two concepts by which the
  underlying magnetic structure could lead to the observed phenomenology -
  the true differential rotation of a nonaxisymmetric magnetic structure
  and a stroboscopic effect. In the latter case, a solid body rotation of
  nonaxisymmetric magnetic structure is illuminated by an activity wave
  propagating from middle latitudes to the solar equator, and so mimics a
  differential rotation. We then discuss several mechanisms which could in
  principle lead to the excitation of active longitudes. In particular,
  we consider dynamo excitation of nonaxisymmetric magnetic modes,
  nonaxisymmetric structures as a manifestation of a relic magnetic
  field in the solar core, nonaxisymmetric solar hydrodynamics and
  nonlinear instabilities that lack axial symmetry. We conclude that
  these mechanisms all provide ways to explain the phenomenology,
  provided the stroboscopic interpretation is accepted. Of course, a
  quantitative explanation in the framework of any scenario requires
  ultimately a detailed numerical simulation. The interpretation of
  the available observations as a true differential rotation appears to
  provide a much more severe challenge for theorists. We are unable to
  suggest a plausible mechanism of this kind; however we can not exclude
  in principle such an explanation. We relate the phenomenon of solar
  active longitudes to the information available concerning stellar
  active longitudes, and also consider evidence from other tracers of
  solar activity.

---------------------------------------------------------
Title: Heliospheric modulation of cosmic rays: Monthly reconstruction
    for 1951-2004
Authors: Usoskin, Ilya G.; Alanko-Huotari, Katja; Kovaltsov, Gennady
   A.; Mursula, Kalevi
2005JGRA..11012108U    Altcode:
  The differential energy spectrum of galactic cosmic rays in the
  vicinity of the Earth can be parameterized by the so-called force
  field model which has only one parameter, the modulation potential ϕ,
  for a given local interstellar spectrum. Here we present the series
  of monthly values of the modulation potential ϕ since February 1951,
  reconstructed using the data from the worldwide neutron monitor network
  and calibrated with precise balloon and space-borne direct measurements
  of cosmic ray energy spectrum. This work provides a long series
  of a parameter allowing for a quantitative estimate of the average
  monthly differential energy spectrum of cosmic rays near the Earth. A
  comparison with other occasional direct measurements of cosmic ray
  spectra confirms the reliability of the present reconstruction. The
  results can be applied in studies of long-term solar-terrestrial
  relations and the global evolution of the heliosphere.

---------------------------------------------------------
Title: What is Unusual About the 2005 January 20 SEP Event?
Authors: Gopalswamy, N.; Xie, H.; Yashiro, S.; Usoskin, I.
2005AGUFMSH23A0318G    Altcode:
  We report on the solar energetic particle (SEP) event of 2005 January
  20 that had an associated ground level enhancement (GLE). The Solar
  and Heliospheric Observatory (SOHO) spacecraft observed a CME, which
  was among the fastest of cycle 23 CMEs. This event is consistent with
  the results that the GLE-associated CMEs represent the fastest known
  population of CMEs. A metric type II burst started before the proton
  injection time, suggesting that a coronal shock was formed before
  high-energy protons were released at the Sun. These 2005 January 20
  event is consistent with the current paradigm that large SEP events
  originate in CME-driven shocks. We also determined the height of
  the CME at two time marks: the metric type II onset (2.1 Rs) and
  the proton injection time (4.5 Rs). At a height of 4.5 Rs the CME
  should have attained the maximum speed, thus driving the strongest
  shocks. We discuss the estimation of the CME speed given that the
  coronagraph observations were hampered by the SEPs arriving at the SOHO
  spacecraft. We also discuss the arrival of the CME-associated plasma
  and shock at 1 AU. Work supported by NASA/LWS and NSF/SHINE programs.

---------------------------------------------------------
Title: Measurements of muon flux in the Pyhäsalmi underground
    laboratory
Authors: Enqvist, T.; Mattila, A.; Föhr, V.; Jämsén, T.; Lehtola,
   M.; Narkilahti, J.; Joutsenvaara, J.; Nurmenniemi, S.; Peltoniemi,
   J.; Remes, H.; Sarkamo, J.; Shen, C.; Usoskin, I.
2005NIMPA.554..286E    Altcode: 2005hep.ex....6032E
  The cosmic-ray induced muon flux was measured at several depths in
  the Pyhäsalmi mine (Finland) using a plastic scintillator telescope
  mounted on a trailer. The flux was determined at four different
  depths underground at 400 m (980 m.w.e), at 660 m (1900 m.w.e), at
  990 m (2810 m.w.e) and at 1390 m (3960 m.w.e) with the trailer, and
  also at the ground surface. In addition, previously measured fluxes
  from depths of 90 m (210 m.w.e) and 210 m (420 m.w.e) are shown. A
  relation was obtained for the underground muon flux as a function of
  the depth. The measured flux follows well the general behaviour and
  is consistent with results determined in other underground laboratories.

---------------------------------------------------------
Title: Preferred sunspot longitudes: non-axisymmetry and differential
    rotation
Authors: Usoskin, I. G.; Berdyugina, S. V.; Poutanen, J.
2005A&A...441..347U    Altcode: 2005astro.ph..8422U
  As recently found, the distribution of sunspots is non-axisymmetric
  and spot group formation implies the existence of two persistent
  active longitudes separated by 180°. Here we quantitatively study the
  non-axisymmetry of sunspot occurrence. In a dynamic reference frame
  inferred from the differential rotation law, the raw sunspot data
  show a clear clustering around the persistent active longitudes. The
  differential rotation describing the dynamic frame is quantified
  in terms of the equatorial angular velocity and the differential
  rotation rate, which appear to be significantly different from those
  for individual sunspots. This implies that the active longitudes are
  not linked to the depth of sunspot anchoring. In order to quantify
  the observed effect, we introduce a measure of the non-axisymmetry of
  the sunspot distribution. The non-axisymmetric component is found to
  be highly significant, and the ratio of its strength to that of the
  axisymmetric one is roughly 1:10. This provides additional constraints
  for solar dynamo models.

---------------------------------------------------------
Title: Solar activity, cosmic rays, and Earth's temperature: A
    millennium-scale comparison
Authors: Usoskin, I. G.; Schüssler, M.; Solanki, S. K.; Mursula, K.
2005JGRA..11010102U    Altcode:
  Previous studies of a solar influence on climate variations have often
  suffered from the relatively short length of continuous direct solar
  observations of less than 400 years. We use two recently reconstructed
  series of the sunspot number and the cosmic ray flux to study this
  question over time intervals of up to nearly 1800 years. Comparison of
  the Sun-related data sets with various reconstructions of terrestrial
  Northern Hemisphere mean surface temperatures reveals consistently
  positive correlation coefficients for the sunspot numbers and
  consistently negative correlation coefficients for the cosmic rays. The
  significance levels reach up to 99% but vary strongly for the different
  data sets. The major part of the correlation is due to the similarity
  of the long-term trends in the data sets. The trend of the cosmic ray
  flux correlates somewhat better with the terrestrial temperature than
  the sunspot numbers derived from the same cosmogenic isotope data.

---------------------------------------------------------
Title: Climate:  How unusual is today's solar activity? (reply)
Authors: Solanki, S. K.; Usoskin, I. G.; Kromer, B.; Schüssler, M.;
   Beer, J.
2005Natur.436E...4S    Altcode:
  Muscheler et al. claim that the solar activity affecting cosmic rays
  was much higher in the past than we deduced from <SUP>14</SUP>C
  measurements. However, this claim is based on a problematic
  normalization and is in conflict with independent results, such as
  the <SUP>44</SUP>Ti activity in meteorites and the <SUP>10</SUP>Be
  concentration in ice cores.

---------------------------------------------------------
Title: Solar activity over the last 1150 years: does it correlate
    with climate?
Authors: Usoskin, I. G.; Schüssler, M.; Solanki, S. K.; Mursula, K.
2005ESASP.560...19U    Altcode: 2005csss...13...19U
  No abstract at ADS

---------------------------------------------------------
Title: Real-Time Cosmic Ray Distributed (RECORD) database: A status
    report
Authors: Starodubtsev, S. A.; Turpanov, A. A.; Kudela, K.; Usoskin,
   I. G.; Yanke, V. G.; Grigoryev, V. G.; Neustroyev, N. I.; Egorov,
   A. G.; Prikhodko, A. N.
2005ICRC....2..465S    Altcode: 2005ICRC...29b.465S
  No abstract at ADS

---------------------------------------------------------
Title: Long-Term Modulation of the Cosmic Ray Fluctuation Spectrum:
    Spacecraft Measurements
Authors: Starodubtsev, S. A.; Usoskin, I. G.; Grigoryev, A. V.;
   Mursula, K.
2005ICRC....2..247S    Altcode: 2005ICRC...29b.247S
  No abstract at ADS

---------------------------------------------------------
Title: Coronal Mass Ejections and Ground Level Enhancements
Authors: Gopalswamy, N.; Xie, H.; Yashiro, S.; Usoskin, I.
2005ICRC....1..169G    Altcode: 2005ICRC...29a.169G
  No abstract at ADS

---------------------------------------------------------
Title: The role of drifts in the galactic cosmic ray transport
Authors: Alanko, K.; Usoskin, I. G.; Mursula, K.
2005ICRC....2...53A    Altcode: 2005ICRC...29b..53A
  No abstract at ADS

---------------------------------------------------------
Title: Cosmic ray-induced ionization in the atmosphere: spatial and
    temporal changes
Authors: Usoskin, I. G.; Gladysheva, O. G.; Kovaltsov, G. A.
2004JASTP..66.1791U    Altcode: 2004JATP...66.1791U
  Detailed calculations of the time-variable spatial distribution of
  cosmic ray-induced ionization of the lower atmosphere are presented
  using a physical model. Using the differential energy spectrum of cosmic
  rays obtained from the worldwide neutron monitor network since 1951 and
  taking into account also the slow changes in the geomagnetic dipole,
  we have calculated the corresponding 3D (geographical coordinates and
  altitude) equilibrium ion concentration in the lower atmosphere as a
  function of time for the period 1951-2000. A comparison to the results
  of measurements validates the calculation method, as the calculated
  cosmic ray-induced ionization reproduces in general the observed
  altitudinal and latitudinal profiles of the ion concentration. The
  results of the present work provide a basis for a quantitative study
  of the solar-terrestrial relationships on long time scales.

---------------------------------------------------------
Title: An Upper Limit on Sunspot Activity During the Maunder Minimum
Authors: Kovaltsov, G. A.; Usoskin, I. G.; Mursula, K.
2004SoPh..224...95K    Altcode: 2005SoPh..224...95K
  We have estimated the upper and lower limits of sunspot activity, in
  terms of active day fraction during the Maunder minimum (1645-1710),
  using raw information on individual daily observations (Hoyt and
  Schatten, 1998). Establishing the relation between the sunspot
  activity and active day fraction after 1850, we evaluate the upper
  limit of annual group sunspot number during the deep Maunder minimum
  (1645-1700) which does not exceed 4. The earlier finding of a dominant
  22-year periodicity during the Maunder minimum is verified and shown
  to be robust. Also we confirm that the start of the Maunder minimum
  was very abrupt.

---------------------------------------------------------
Title: Rapid Cosmic Ray Fluctuations: Evidence for Cyclic Behaviour
Authors: Starodubtsev, S. A.; Usoskin, I. G.; Mursula, K.
2004SoPh..224..335S    Altcode: 2005SoPh..224..335S
  We study rapid cosmic-ray fluctuations using 5-min resolution data
  from eight neutron monitors with different cutoff rigidities as well
  as from the ACE satellite. We define a proxy index of rapid cosmic-ray
  fluctuations as the mean power of the cosmic-ray power spectrum in the
  frequency range 10<SUP>−4</SUP> −1.67 × 10<SUP>−3</SUP> Hz (10
  min to about 3 h). A dominant 11-year periodicity in the index is found
  in all neutron monitors. We also report on intermittent, short-term
  periodicities in the power of rapid cosmic-ray fluctuations. A strong
  mid-term periodicity of about 1.6 - 1.8 years, possibly related to a
  recently found similar periodicity in IMF, appears in CR fluctuation
  power since the 1980s. Another strong periodicity is found at 1 year,
  which is likely related to the relative position of the Earth in the
  heliosphere. These results also provide new challenge to test the
  cosmic-ray modulation theory.

---------------------------------------------------------
Title: Preface
Authors: mursula, kalevi; usoskin, ilya; cliver, edward
2004SoPh..224....3M    Altcode: 2005SoPh..224....3M
  No abstract at ADS

---------------------------------------------------------
Title: Long-Term Solar Activity: Direct and Indirect Study
Authors: Usoskin, I. G.; Kovaltsov, G. A.
2004SoPh..224...37U    Altcode: 2005SoPh..224...37U
  The series of directly observed sunspot numbers is nearly 400 years
  long. We stress that the recently compiled group sunspot number series
  is an upgrade of the old Wolf series and should always be used before
  1850. The behavior of solar activity on longer time scales can be
  studied only using indirect proxies. Such proxies as aurorae occurrence
  or naked-eye sunspot observations are qualitative indicators of solar
  activity but can be hardly quantitatively interpreted. Cosmogenic
  isotope records provide a basis for quantitative estimate of the past
  solar activity. Here we overview the main methods of the long-term
  solar activity reconstruction on the centennial to multimillennia
  time scale. We discuss that regression-based reconstructions of solar
  activity lead to very uncertain results, while recently developed
  physics-based models raise solar activity reconstruction to a new level
  and allow studying its behavior on a multimillennia time scale. In
  particular, the reconstructions show that the recent episode of high
  solar activity is quite unusual in the multimillennia time scale.

---------------------------------------------------------
Title: Unusual activity of the Sun during recent decades compared
    to the previous 11,000 years
Authors: Solanki, S. K.; Usoskin, I. G.; Kromer, B.; Schüssler, M.;
   Beer, J.
2004Natur.431.1084S    Altcode:
  Direct observations of sunspot numbers are available for the past
  four centuries, but longer time series are required, for example,
  for the identification of a possible solar influence on climate
  and for testing models of the solar dynamo. Here we report a
  reconstruction of the sunspot number covering the past 11,400 years,
  based on dendrochronologically dated radiocarbon concentrations. We
  combine physics-based models for each of the processes connecting
  the radiocarbon concentration with sunspot number. According to our
  reconstruction, the level of solar activity during the past 70 years is
  exceptional, and the previous period of equally high activity occurred
  more than 8,000 years ago. We find that during the past 11,400 years
  the Sun spent only of the order of 10% of the time at a similarly high
  level of magnetic activity and almost all of the earlier high-activity
  periods were shorter than the present episode. Although the rarity
  of the current episode of high average sunspot numbers may indicate
  that the Sun has contributed to the unusual climate change during the
  twentieth century, we point out that solar variability is unlikely
  to have been the dominant cause of the strong warming during the past
  three decades.

---------------------------------------------------------
Title: Latitudinal dependence of low cloud amount on cosmic ray
    induced ionization
Authors: Usoskin, I. G.; Marsh, N.; Kovaltsov, G. A.; Mursula, K.;
   Gladysheva, O. G.
2004GeoRL..3116109U    Altcode: 2004physics...7066U
  A significant correlation between the annual cosmic ray flux and
  the amount of low clouds has recently been found for the past 20
  years. However, of the physical explanations suggested, none has
  been quantitatively verified in the atmosphere by a combination
  of modelling and experiment. Here we study the relation between
  the global distributions of the observed low cloud amount and the
  calculated tropospheric ionization induced by cosmic rays. We find
  that the time evolution of the low cloud amount can be decomposed into
  a long-term trend and inter-annual variations, the latter depicting
  a clear 11-year cycle. We also find that the relative inter-annual
  variability in low cloud amount increases polewards and exhibits a
  highly significant one-to-one relation with inter-annual variations
  in the ionization over the latitude range 20-55°S and 10-70°N. This
  latitudinal dependence gives strong support for the hypothesis that
  the cosmic ray induced ionization modulates cloud properties.

---------------------------------------------------------
Title: Solar Modulation Models:. a Comparison Through a 2d Stochastic
    Simulation
Authors: Bobik, P.; Gervasi, M.; Grandi, D.; Rancoita, P. G.; Usoskin,
   I. G.
2004apsp.conf...23B    Altcode:
  We developed a 2D stochastic simulation model of galactic cosmic rays
  propagation in the heliosphere. Drift effects are taken in account in
  the solar modulation model. The model has been optimized by comparison
  with measured data. We also analyze the dependence of the modulated
  flux of cosmic rays at 1 AU from the diffusion tensor, and its relation
  with the solar cavity and cosmic rays parameters. We compute spectra
  for different values of the tilt angle for both positive and negative
  solar cycles.

---------------------------------------------------------
Title: Usoskin et al. Reply:
Authors: Usoskin, Ilya G.; Solanki, Sami K.; Schüssler, Manfred;
   Mursula, Kalevi
2004PhRvL..92s9002U    Altcode:
  A Reply to the Comment by G. M. Raisbeck and F. Yiou.

---------------------------------------------------------
Title: Persistent active longitudes in the surface magnetic activity
    on the Sun
Authors: Berdyugina, S.; Usoskin, I. G.
2004cosp...35.1722B    Altcode: 2004cosp.meet.1722B
  A novel analysis of sunspot data for the past 120 years reveals
  that sunspots in both northern and southern hemispheres are formed
  preferably in two persistent active longitudes separated by 180°. In
  the Carrington reference frame, the active longitudes continuously
  migrate in phase with respect to the Carrington meridian. The
  migration of the active longitudes is determined by changes of the mean
  latitude of sunspots and the surface differential rotation. The two
  active longitudes periodically alternate being the dominant region,
  similar to the 'flip-flop' phenomenon known in starspot activity. The
  period of the oscillations is about 3.8 and 3.65 years in the northern
  and southern hemispheres, respectively. The difference between the
  periods is significant and can be related to the known north-south
  asymmetry in the solar magnetic activity. Similar results are obtained
  from the analysis of large-scale surface magnetic fields using solar
  magnetic synoptic maps, for the cycles 20 to 23. The persistent active
  longitudes 180° apart, which migrate with the surface differential
  rotation and alternate their activity level with the 3.7-yr cycle, are
  found separately in positive and negative polarity fields. Our results
  provide new observational constraints for current solar dynamo models
  and strengthen the solar paradigm for magnetic activity on cool stars.

---------------------------------------------------------
Title: Cosmic ray induced ionization in the troposphere: Numerical
    model
Authors: Usoskin, I. G.; Gladysheva, O. G.; Kovaltsov, G. A.
2004cosp...35.1671U    Altcode: 2004cosp.meet.1671U
  First detailed calculations of the time-variable spatial distribution
  of cosmic ray induced ionization of the lower atmosphere are
  presented using a physical model describing development of a
  nucleonic-electromagnetic cascade in the atmosphere. Using the
  differential energy spectrum of cosmic rays obtained from the worldwide
  neutron monitor network data since 1951 and taking into account also
  the slow changes in the geomagnetic field, we have calculated the
  corresponding 3D (geographical coordinates and altitude) equilibrium
  ion concentration in the lower atmosphere as a function of time for the
  period 1951-2000. A comparison with the results of actual balloon-borne
  measurements of the atmospheric ionization validates the calculation
  method, and the calculated cosmic ray induced ionization reproduces the
  observed altitudinal and latitudinal profiles of the ion concentration
  for the altitude range 0-12 km. The results of the present work provide
  a basis for quantitative study of the solar-terrestrial relationships
  on long time scales.

---------------------------------------------------------
Title: Cosmic ray modulation and global heliospheric parameters:
    Non-linear relations
Authors: Usoskin, I. G.; Kovaltsov, G. A.; Mursula, K.; Alanko, K.
2004cosp...35.1685U    Altcode: 2004cosp.meet.1685U
  Despite the great success of sophisticated cosmic ray modulation models,
  the heliospheric modulation strength is still a useful parameter
  for formal description of the long-term modulation of cosmic rays,
  which alone defines shape of the cosmic ray energy spectrum in the
  neutron monitor energy range. Annual averaged values of the modulation
  strength have recently been computed for the neutron monitor era
  since 1951-2002 (Usoskin et al., Sol. Phys., 207, 389, 2002). Here we
  study a physics-based semi-empirical, non-linear relation between the
  modulation strength and the following global heliospheric parameters:
  the heliospheric current sheet tilt angle, the open solar magnetic
  flux and the global magnetic field polarity. The suggested relation,
  which includes four fitting parameters, reproduces the measured
  annual NM count rates within the accuracy of 0.8%. Using the measured
  interplanetary magnetic field parameters and the modulation strength
  values computed since 1951, this relation allows us to reconstruct
  the annual tilt angle for about 20 years before the time of direct
  measurements of the tilt angle.

---------------------------------------------------------
Title: Persistent Active Longitudes in Sunspot Activity: Sun-as-a-Star
    Approach
Authors: Berdyugina, S. B.; Usoskin, I. G.
2004IAUS..219..128B    Altcode: 2003IAUS..219E.183B
  An analysis of sunspot group data for the past 120 years reveals
  that sunspots are formed preferably in two persistent migrating
  active longitudes 180 degrees apart. Their migration is determined by
  changes of the mean latitude of sunspots and the surface differential
  rotation. The two active regions periodically alternate being the
  dominant region with a period of about 3.5-3.7 years similar to the
  ""flip-flop"" phenomenon known in starspot activity. The fact that the
  Sun shows the same pattern of magnetic activity as highly active stars
  strengthens the solar paradigm for magnetic activity on cool stars
  allowing the physics of the activity on such stars to be understood
  within the context of the physical principles deduced from the study
  of the Sun.

---------------------------------------------------------
Title: Reconstruction of solar activity for the last millennium
    using <SUP>10</SUP>Be data
Authors: Usoskin, I. G.; Mursula, K.; Solanki, S.; Schüssler, M.;
   Alanko, K.
2004A&A...413..745U    Altcode: 2003astro.ph..9556U
  In a recent paper (Usoskin et al. 2002a), we have reconstructed
  the concentration of the cosmogenic <SUP>10</SUP>Be isotope in ice
  cores from the measured sunspot numbers by using physical models
  for <SUP>10</SUP>Be production in the Earth's atmosphere, cosmic ray
  transport in the heliosphere, and evolution of the Sun's open magnetic
  flux. Here we take the opposite route: starting from the <SUP>10</SUP>Be
  concentration measured in ice cores from Antarctica and Greenland, we
  invert the models in order to reconstruct the 11-year averaged sunspot
  numbers since 850 AD. The inversion method is validated by comparing
  the reconstructed sunspot numbers with the directly observed sunspot
  record since 1610. The reconstructed sunspot record exhibits a prominent
  period of about 600 years, in agreement with earlier observations
  based on cosmogenic isotopes. Also, there is evidence for the century
  scale Gleissberg cycle and a number of shorter quasi-periodicities
  whose periods seem to fluctuate in the millennium time scale. This
  invalidates the earlier extrapolation of multi-harmonic representation
  of sunspot activity over extended time intervals.

---------------------------------------------------------
Title: Establishing space research capability in Ethiopia
Authors: Bosinger, T.; Damtie, B.; Usoskin, I. G.
2004cosp...35.2504B    Altcode: 2004cosp.meet.2504B
  It is often considered by various sources and institutions around the
  world that promotion of space physics activities in a developing country
  like Ethiopia is a waste of time and resources. It has, of course, some
  sense: developing countries should put all their efforts in improving
  the standard of life, infrastructure and basic education. However,
  it is straightforward to realize that nowadays improvement in any of
  the basic needs of developing countries is related to high technology
  (e.g. mobile phones, GPS, remote sensing). This means that a developing
  country has to take care of recruiting specialists among their own
  people who can take part in the decision making processes which are
  increasingly of global nature. Moreover, many citizens of developing
  countries are studying and working abroad attaining high expertise. As
  a matter of fact, there are more Ethiopians with PhD in physics working
  abroad than in the country. These people are lost for the benefit of
  their own country if there is no need for their profession in their
  home country. There is no doubt that the main task of improving the
  standard of living cannot be achieved without development and social
  transformation of the society, which can take place efficiently in a
  self-adopting and dynamic process. In line with the above argument, we
  have initiated the establishment of the Washera Space Physics Laboratory
  (WASPL) at Addis Ababa University in Ethiopia. It is a collaboration
  project between Oulu University and Addis Ababa University. The
  laboratory is expected to start operation of a pulsation magnetometer
  and photometer in September 2004. Other types of standard geophysical
  instruments are to be installed in subsequent missions. The project is
  of mutual interest of both parties. The equatorial ionosphere is still a
  poorly investigated region of our near Earth's space. In a first pilot
  investigation the existence and properties of the ionospheric Alfvén
  resonator (IAR) in the equatorial ionosphere is addressed. WASPL is
  expected to join worldwide activities in monitoring local and global
  atmosphereic and ionospheric parameters. There is also a plan to install
  a neutron monitor to measure galactic and solar cosmic rays. WASPL will
  be situated at the magnetic equator and at 2500m above seal level, which
  make it a unique place to carry out space physics experiments. In this
  paper, we describe WASPL in some more details. Interested scientists
  may participate with us and/or start similar initiatives.

---------------------------------------------------------
Title: Long-term variations in cosmic ray fluctuations
Authors: Starodubtsev, S. A.; Usoskin, I. G.; Mursula, K.
2004cosp...35.1930S    Altcode: 2004cosp.meet.1930S
  It has been shown recently that the level of cosmic ray fluctuations
  varies over a solar cycle due to the corresponding changes of the in
  interplanetary turbulence spectrum. In earlier studies, fragmentary
  high-resolution data from polar neutron monitors (Tixie Bay and
  Oulu) were used. Here we present the results of an analysis of 5-min
  resolution cosmic ray data series from six neutron monitors with
  geomagnetic cutoff rigidities from polar to 6 GV (Calgary, Kiel,
  Lomnicky Stit, Oulu, Rome and Tixie) as well as from space-borne
  IMP-8. The longest time series of 5-min data is from Oulu NM
  since 1968. As the index of cosmic ray fluctuations we use the
  mean power of the cosmic ray power spectrum in the frequency range
  10<SUP>-4</SUP>-1.67\cdot 10<SUP>-3</SUP> Hz. The dominant 11-year
  periodicity is found in all series, confirming earlier results but
  in a wide range of cutoff rigidities. We report also new persistent
  periodicities in cosmic ray fluctuations. A strong 1.5-1.8-year
  periodicity related the corresponding cyclicities in IMF is apparent
  in all data series. Another strong peak is found at nearly 1 year
  period, which is related to the relative position of the Earth in the
  heliosphere. These results provide a new basis for testing the cosmic
  ray modulation theory.

---------------------------------------------------------
Title: Low cloud amount vs. Cosmic ray induced ionization: One-to-one
    relation
Authors: Usoskin, I. G.; Marsh, N.; Mursula, K.; Gladysheva, O. G.;
   Kovaltsov, G. A.
2004cosp...35.1683U    Altcode: 2004cosp.meet.1683U
  A highly significant correlation between the annual flux of cosmic
  rays at the Earth's orbit and the amount of low clouds has recently
  been found for the past 20 years. However, a comprehensive physical
  explanation still remains elusive. Elsewhere in this session we present
  a numerical model to calculate ionization of the troposphere caused by
  a cosmic ray induced nucleonic-electromagnetic cascade. Here we study
  the relation between this calculated cosmic ray induced ionization
  and the global distributions of the observed low cloud amount. We find
  that the time evolution of the low cloud amount can be decomposed into
  a long-term trend and inter-annual variations, the latter depicting a
  clear 11-year cycle with very strong correlation (r=0.84) with cosmic
  ray induced ionization. We also find that the relative inter-annual
  variability in low cloud amount increases polewards and exhibits a
  highly significant one-to-one relation with inter-annual variations in
  the ionization over the latitude range 20--55° S and 10--70° N. This
  latitudinal dependence gives strong support for the hypothesis that
  cosmic ray induced ionization modulates cloud properties.

---------------------------------------------------------
Title: Streaming of Galactic Cosmic Rays in the Heliosphere and the
    Role of Drifts
Authors: Alanko, K.; Usoskin, I. G.; Mursula, K.
2004cosp...35.2250A    Altcode: 2004cosp.meet.2250A
  During their transport through the heliosphere, galactic cosmic rays
  suffer from scattering on magnetic inhomogenities, from convection
  and adiabatic cooling by the solar wind. In addition to these basic
  mechanisms, also drifts (gradient, curvature and drift along the wavy
  heliospheric current sheet) affect the transport of cosmic rays. All
  these effects are known as the solar modulation of cosmic rays. We have
  recently presented a new model of the transport of galactic cosmic rays
  in a 2D axisymmetric heliosphere, which includes the above mentioned
  effects. Using this model, we can compare the effects of different
  modulation mechanisms in the model and, in particular, study the role
  of drifts. We also study the streaming of galactic cosmic rays inside
  the heliosphere, their modulated spectra, the time particles spend in
  the heliosphere and the modulation function.

---------------------------------------------------------
Title: Solar activity and climate during the last millennium
Authors: Solanki, S. K.; Usoskin, I.; Schüssler, M.
2004cosp...35.2535S    Altcode: 2004cosp.meet.2535S
  The sunspot number is the longest running direct index of solar
  activity, with direct measurements starting in 1610. For many purposes,
  e.g., for comparisons with climate indices, it is still too short. We
  present a reconstruction of the cycle-averaged sunspot number over the
  last millennium based on <SUP>10</SUP>Be concentrations in Greenland
  and Antarctic ice cores. As intermediate steps of the method, we also
  reconstruct the cosmic ray flux at Earth and the Sun's open magnetic
  flux. The reconstructions are validated by comparison with direct
  measurements or independent reconstructions. We also compare with
  records of global climate, in particular with the global temperature
  ("hockey stick") curve of Mann et al (1998). A reasonable agreement
  is found for the entire millennium, excluding only the last decades,
  when the two curves start diverging from each other.

---------------------------------------------------------
Title: Magnetic Activity Cycles on the Sun and Stars
Authors: Usoskin, I. G.; Berdyugina, S.
2004cosp...35.1721U    Altcode: 2004cosp.meet.1721U
  Cycles of magnetic activity on the Sun and stars are manifestations
  of a magnetic dynamo, which is one of the most interesting processes
  in solar/stellar astrophysics. Evolution of solar magnetic cycles is
  studied for several centuries including the nearly spotless Maunder
  minimum and recent super-active cycles, thanks to tremendous work
  of R. Wolf and his successors and later D. Hoyt and K. Schatten who
  complied sunspot record series. Magnetic cycles in stars are studied
  during few decades but they provide a large ensemble statistics
  due to a large number of studied stars. Here we review most recent
  achievements and findings in studies of solar/stellar magnetic cycles,
  such as determinism and chaos in the cyclicity, cycles during active
  phases and great minima, active longitudes and 'flip-flop' cycles,
  occurrence of great minima and super-active periods.

---------------------------------------------------------
Title: Reconstruction of Monthly and Yearly Group Sunspot Numbers
    From Sparse Daily Observations
Authors: Usoskin, I. G.; Mursula, K.; Kovaltsov, G. A.
2003SoPh..218..295U    Altcode:
  Some periods before 1820 are poorly covered by sunspot observations. In
  addition to apparent, long observational gaps, there are also
  periods when there are only few sparse daily sunspot observations
  during a long time. It is important to estimate the reliability of
  the monthly and yearly mean sunspot values obtained from such sparse
  daily data. Here we suggest a new method to estimate the reliability of
  individual monthly means. The method is based on comparing the actual
  sparse data (sample population) to the well-measured sunspot data in
  1850-1996 (reference population), and assumes that the statistical
  properties of sunspot activity remain similar throughout the entire
  period. For each sample population we first found those months in the
  reference population that contain the same data set, and constructed
  the statistical distribution of the corresponding monthly means. The
  mean and standard error of this distribution represent the mean and
  uncertainty of a monthly mean sunspot number reconstructed from sparse
  daily observations. The simple arithmetic mean of daily values can
  be adequately applied for months which contain more than 4-5 evenly
  distributed daily observations. However, the reliability of monthly
  means for less covered months has to be estimated more carefully. Using
  the estimated, new monthly values, we have also calculated the weighted
  annual sunspot numbers.

---------------------------------------------------------
Title: Long-Term Solar Cycle Evolution: Review of Recent Developments
Authors: Usoskin, I. G.; Mursula, K.
2003SoPh..218..319U    Altcode:
  The sunspot number series forms the longest directly observed index
  of solar activity and allows one to trace its variations on the time
  scale of about 400 years since 1610. This time interval covers a wide
  range from seemingly vanishing sunspots during the Maunder minimum in
  1645-1700 to the very high activity during the last 50 years. Although
  the sunspot number series has been studied for more than a century, new
  interesting features have been found even recently. This paper gives a
  review of the recent achievements and findings in long-term evolution
  of solar activity cycles such as determinism and chaos in sunspot
  cyclicity, cycles during the Maunder minimum, a general behaviour of
  sunspot activity during a great minimum, the phase catastrophe and
  the lost cycle in the beginning of the Dalton minimum in 1790s and
  persistent 22-year cyclicity in sunspot activity. These findings shed
  new light on the underlying physical processes responsible for sunspot
  activity and allow a better understanding of such empirical rules as
  the Gnevyshev-Ohl rule and the Waldmeier relations.

---------------------------------------------------------
Title: Millennium-Scale Sunspot Number Reconstruction: Evidence for
    an Unusually Active Sun since the 1940s
Authors: Usoskin, Ilya G.; Solanki, Sami K.; Schüssler, Manfred;
   Mursula, Kalevi; Alanko, Katja
2003PhRvL..91u1101U    Altcode: 2003astro.ph.10823U
  The extension of the sunspot number series backward in time is of
  considerable interest for dynamo theory, solar, stellar, and climate
  research. We have used records of the <SUP>10</SUP>Be concentration in
  polar ice to reconstruct the average sunspot activity level for the
  period between the year 850 to the present. Our method uses physical
  models for processes connecting the <SUP>10</SUP>Be concentration with
  the sunspot number. The reconstruction shows reliably that the period
  of high solar activity during the last 60years is unique throughout
  the past 1150years. This nearly triples the time interval for which
  such a statement could be made previously.

---------------------------------------------------------
Title: 2D stochastic simulation model of cosmic ray modulation:
    comparison with experimental data
Authors: Bobik, P.; Gervasi, M.; Grandi, D.; Rancoita, P. G.; Usoskin,
   I. G.
2003ESASP.535..637B    Altcode: 2003iscs.symp..637B
  We developed a 2D stochastic simulation model for heliospheric
  propagation of galactic cosmic rays. The model solves numerically the
  transport equation of particles in the heliosphere. In the calculation
  we use also drift effects which are included through analytical
  effective drift velocities. We estimated the cosmic rays spectrum at
  1 AU using this model formalism. The calculated spectra are compared
  with other models (CREME96) and with experimental data (IMP8 and AMS)
  for positive (A&gt;0) and negative (A&lt;0) solar periods.

---------------------------------------------------------
Title: Long-Term Modulation of the Galactic Cosmic-Ray Fluctuation
    Spectrum
Authors: Starodubtsev, S. A.; Usoskin, I. G.
2003AstL...29..594S    Altcode:
  We study the temporal behavior of the power spectra for Galactic
  cosmic-ray fluctuations during the last two solar cycles. We use the
  5-min data for 1980-2002 corrected for the barometric effect from two
  widely separated high-latitude cosmic-ray stations, Tixie Bay and
  Oulu. The cosmic-ray fluctuation spectrum is shown to be subjected
  to a regular long-term modulation with a period of about 11 years in
  phase with the solar cycle, in accordance with the variations in the
  inertial part of the turbulence spectrum for the interplanetary magnetic
  field. Based on independent measurements, we confirm the previously
  detected cosmic-ray fluctuation power enhancement at the maximum of
  the 11-year solar cycle and its subsequent decrease at minimum solar
  activity using new, more extensive data sets. We reach the conclusion
  about the establishment of a new cosmic-ray modulation phenomenon that
  has not been described previously in scientific literature.

---------------------------------------------------------
Title: On the reliability of monthly/yearly means calculated from
    sparse daily sunspot numbers
Authors: Usoskin, Ilya G.; Mursula, Kalevi; Kovaltsov, Gennady A.
2003ESASP.535..165U    Altcode: 2003iscs.symp..165U
  Some periods before 1850 are poorly covered by sunspot observations. In
  addition to apparent observational gaps, there are also periods when
  there are only few sparse daily sunspot observations during a long
  time. It is important to estimate the reliability of the monthly/yearly
  mean values obtained from sparse daily data. Here we suggest a new
  method to estimate the reliability of individual monthly means. The
  method is based on comparing the actual sparse data (sample population)
  to the well-measured sunspot data in 1850-1996 (reference population)
  and employs two assumptions: (I) statistical properties of sunspot
  activity are similar throughout the entire period and (II) individual
  sparse daily observations are distributed randomly in time. First,
  for each sample population we found months in the reference population
  containing the same data set and then constructed the statistical
  distribution of the corresponding monthly means. From this distribution
  we calculated the weighted mean and its standard error which gives
  the uncertainty of a monthly mean sunspot number reconstructed from
  sparse daily observation. The simple arithmetic mean can be adequately
  applied for months which contain more than 4-5 evenly distributed daily
  observations. However, the reliability of monthly means for less covered
  months should be estimated more carefully. Using the estimated monthly
  values, we can also calculate the weighted annual sunspot numbers.

---------------------------------------------------------
Title: The lost sunspot cycle: reanalysis of sunspot statistics
Authors: Usoskin, Ilya G.; Mursula, Kalevi; Kovaltsov, Gennady A.
2003ESASP.535..161U    Altcode: 2003iscs.symp..161U
  We have recently suggested (Usoskin et al., 2000) that one low sunspot
  cycle was possibly lost in 1790s, and argued (Usoskin et al., 2002) that
  the existence of such a cycle does not contradict with available solar
  proxies, like auroral observations and cosmogenic isotopes. However,
  some arguments based on a statistical analysis of sunspot activity have
  been presented against the lost cycle (Krivova et al., 2002). Since the
  consequences of a new cycle are significant for solar cycle studies,
  it is important to try to estimate the probability of such a cycle to
  exist. Here we present the results of a rigorous statistical analysis
  of all available sunspot observations around the suggested additional
  cycle minimum in 1792-1793. We show that the level of sunspot activity
  in 1792-1793 is statistically similar to that in the minimum phase,
  but significantly different from that in the mid-declining or maximum
  phases. Using the estimated uncertainties we also calculate new,
  weighted annual values of group sunspot numbers in 1790-1796 which show
  a clear minimum in 1792-1793 and a maximum in 1794-1795, supporting
  the idea of an additional weak cycle in 1790's.

---------------------------------------------------------
Title: Neutron monitor database in real time
Authors: Kozlov, Valery; Kudela, Karel; Starodubtsev, Sergei; Turpanov,
   Alexey; Usoskin, Ilya; Yanke, Victor
2003ESASP.535..675K    Altcode: 2003iscs.symp..675K
  A first distributed Real Time Cosmic Ray Database using measurements
  of several neutron monitors is presented. The aim of the project is to
  develop a unified database with data from different neutron monitors
  collected together, in unified format and to provide a user with several
  commonly used data access methods. The database contains original
  cosmic ray as well as all housekeeping and technical data necessary
  for scientific data analysis. Currently the database includes Lomnicky
  Stit, Moscow, Oulu, Tixie Bay, Yakutsk stations and it is opened for
  other neutron monitors. The main database server is located in IKFIA
  SB RAS (Yakutsk) but there will be several mirrors of the database. The
  datbase and all its mirrors are updated on the nearly real-time (1 hour)
  basis. The data access software includes WWW-interface, Perl scipts and
  C library, which may be linked to a user program. Most of frequently
  used functions are implemented to make it operable to users without
  SQL language knowledge. A draft of the data representation standard is
  suggested, based on common practice of neutron monitor community. The
  database engine is freely distributed open-sourced PostgreSQL server
  coupled with a set of replication tools developed at Bioengineering
  division of the IRCCS E. Medea, Italy.

---------------------------------------------------------
Title: New standpoints in long-term solar cycle evolution: a review
Authors: Usoskin, I. G.; Mursula, K.
2003ESASP.535...25U    Altcode: 2003iscs.symp...25U
  The sunspot number series forms the longest directly observed index of
  solar activity and allows to trace its variations on the time scale of
  about 400 years since 1610. This time interval covers a wide range from
  seemingly vanishing sunspots during the Maunder minimum in 1645-1700
  to the very high activity during the last 500 years. Although the
  sunspot number series has been studied for more than a century, new
  interesting features can still be found. This paper gives a review of
  the recent achievements and findings in long-term evolution of solar
  activity cycles such as determinism and chaos in sunspot cyclicity,
  cycles during the Maunder minimum, scenario of a great minimum, the
  phase catastrophe and the lost cycle in the beginning of the Dalton
  minimum in 1790s and persistent 22-year cyclicity. These findings shed
  new light on the underlying physical processes responsible for the
  sunspot activity and allow for better understanding of such empirical
  rules as Gnevyshev-Ohl rule and Waldmeier relations.

---------------------------------------------------------
Title: Heliospheric modulation strength: effective neutron monitor
    energy
Authors: Alanko, K.; Usoskin, I. G.; Mursula, K.; Kovaltsov, G. A.
2003AdSpR..32..615A    Altcode:
  The widely used concept of the neutron monitor energy range is not
  well defined. Also, the median energy of a neutron monitor varies in
  the course of the solar cycle. Here we present a new concept of the
  effective energy of cosmic rays as measured by neutron monitors. Using
  a spherically-symmetric model of the heliospheric transport of cosmic
  rays and the specific yield function of a neutron monitor, we show that
  there is such an effective energy that the count rate of a given neutron
  monitor is directly proportional to the flux of cosmic rays with energy
  above this effective energy, irrespectively of the phase of the solar
  cycle. The new concept of the effective energy allows to regard the
  neutron monitor count rate as a direct measurement of the galactic
  cosmic ray flux with energy above this value. The effective energy
  varies from about 6 GeV for polar up to about 50 GeV for equatorial
  stations (e.g., it is about 6.5 GeV for high-latitude Oulu, 8 GeV for
  mid-latitude Climax and 40 GeV for equatorial Huancayo NM).

---------------------------------------------------------
Title: Effective Energy of Neutron Monitors
Authors: Alanko, K. M.; Usoskin, I. G.; Mursula, K.; Kovaltsov, G. A.
2003ICRC....7.3901A    Altcode: 2003ICRC...28.3901A
  The widely used concept of the neutron monitor energy range is not
  well defined. Also, the median energy of a neutron monitor varies in
  the course of the solar cycle. Here we present a new concept of the
  effective energy of cosmic rays measured by neutron monitors. Using
  a 1D model of the heliospheric transport of cosmic rays and the
  specific yield function of a neutron monitor, we show that there is
  such an energy value, here called the effective energy, that the
  count rate of a given neutron monitor is directly proportional to
  the flux of cosmic rays with energy above this effective energy,
  irresp ective of the phase of the solar cycle. The new concept of
  the effective energy allows to regard the count rate of each neutron
  monitor as a direct measurement of the galactic cosmic ray flux with
  energy above the effective energy specified for tha station. The
  effective energy varies from about 5.5 GeV for polar up to about 20
  GeV for equatorial stations. The effective energy for the cosmogenic
  polar 10 Be and global 14 C production is about 1.3 GeV and 2.8 GeV,
  respectively. The data of the world-wide network of neutron monitors
  (NMs) provide a good, stable and consistent data set of galactic
  cosmic ray (GCR) intensities for more than 50 years. However, a NM is
  an integral device measuring all cosmic rays above a certain energy
  (local geomagnetic or atmospheric rigidity cutoff ) with the yield
  function increasing sharply with energy. Therefore, it is not clear
  what is the effective energy of cosmic rays as measured by NM. In
  this paper, we intro duce a concept of the effective energy of a NM,
  Eef f , so that the count rate of a given neutron monitor is directly
  proportional to the flux of cosmic rays with energy above this effective
  energy, irresp ectively of the phase of solar cycle. In other words,
  variations of NM count rate directly corresp ond to variations of the
  GCR flux above this effective energy. Neutron monitor count rates can
  be obtained as follows: ∞ G(T , t) · Y (T , x) · dT N (Pc , x, t) =
  (1) Pc

---------------------------------------------------------
Title: A 2D Stochastic Simulation of Galactic Cosmic Rays Transport
    in the Heliosphere
Authors: Alanko, K. M.; Usoskin, Ilya; Mursula, Kalevi; Kovaltsov,
   Gennady A.
2003ICRC....7.3851A    Altcode: 2003ICRC...28.3851A
  We present a new code to numerically simulate the transport of galactic
  cosmic rays in a 2D axisymmetric heliosphere. The model solves the
  transport equation by sto chastic simulation techniques, tracing
  trajectories of test particles in a guiding center approximation. It
  includes such basic modulation mechanisms as diffusion, convection and
  adiabatic cooling. We present the first results from this model and
  compare the effects of the different modulation mechanisms in the model.

---------------------------------------------------------
Title: Galactic Cosmic Ray Fluctuations: Long-Term Modulation of
    Power Spectrum
Authors: Usoskin, Ilya G.; Starodubtsev, S.
2003ICRC....7.3905S    Altcode: 2003ICRC....7.3905U; 2003ICRC...28.3905S
  In the present paper we study the time evolution of power spectra
  of galactic cosmic ray fluctuations during the last three solar
  cycles (1968-2002) using data of 5-min count rates from two far
  spaced high-latitude neutron monitors, Tixie Bay (Russia) and Oulu
  (Finland). We have shown that the power spectrum of cosmic ray
  fluctuations is a sub ject of a regular long-term periodic 11-year
  modulation in phase with solar activity, in accordance with variations
  of the inertial part of the interplanetary magnetic field turbulence
  power spectrum. These results present a new kind of modulation of
  cosmic ray intensities.

---------------------------------------------------------
Title: Active longitudes in sunspot activity: Century scale
    persistence
Authors: Berdyugina, S. V.; Usoskin, I. G.
2003A&A...405.1121B    Altcode:
  A novel analysis of sunspot group data for the past 120 years reveals
  that sunspots in both northern and southern hemispheres are formed
  preferably in two persistent active longitudes separated by 180°. In
  the Carrington reference frame, the active longitudes continuously
  migrate in phase with respect to the Carrington meridian with a variable
  rate. They remain however a quasi-rigid structure. We find that the
  migration of the active longitudes is determined by changes of the mean
  latitude of sunspots and the differential rotation. The differential
  rotation rate calculated from the migration is in agreement with
  SOHO/MDI measurements. The two active longitude periodically alternate
  being the dominant region, similar to the “flip-flop” phenomenon
  known in starspot activity. The period of the oscillations is 3.8
  and 3.65 years in the north and south, respectively. The difference
  between the periods is significant and can be related to the known
  north-south asymmetry in the solar magnetic activity. Our results
  provide new observational constraints for current solar dynamo models
  and strengthen the solar paradigm for magnetic activity on cool stars.

---------------------------------------------------------
Title: REal-time COsmic Ray Database (RECORD)
Authors: Usoskin, I.; Kozlov, Valery; Ksenofontov, Leonid, Kudela,
   Karel; Starodubtsev, Sergei; Turpanov, Alexey; Yanke, Victor
2003ICRC....6.3473K    Altcode: 2003ICRC...28.3473K; 2003ICRC....6.3473U
  In this paper we present a first distributed REal-time COsmic Ray
  Database (RECORD). The aim of the project is to develop a unified
  database with data from different neutron monitors collected together,
  in unified format and to provide a user with several commonly
  used data access methods. The database contains not only original
  cosmic ray data but also auxiliary data necessary for scientific data
  analysis. Currently the database includes Lomn.Stit, Moscow, Oulu; Tixie
  Bay, Yakutsk stations. The main database server is located in IKFIA SB
  RAS (Yakutsk) but there will be several mirrors of the database. The
  database and all its mirrors are up dated on the nearly real-time
  (1 hour) basis. The data access software includes WWW-interface, Perl
  scripts and C library, which may be linked to a user program. Most of
  frequently used functions are implemented to make it operable to users
  without SQL language knowledge. A draft of the data representation
  standard is suggested, based on common practice of neutron monitor
  community. The database engine is freely distributed open-sourced
  PostgreSQL server coupled with a set of replication to ols developed
  at Bio engineering division of the IRCCS E.Medea, Italy.

---------------------------------------------------------
Title: Long-Term Cosmic Ray Intensities: Physical Reconstruction
Authors: Usoskin, I. G.; Mursula, K.; Solanki, S. K.; Schuessler,
   M.; Kovaltsov, G. A.
2003ICRC....7.4041U    Altcode: 2003ICRC...28.4041U
  Solanki et al. (2000) have recently calculated the open solar magnetic
  flux for the last 400 years from sunspot data. Using this reconstructed
  magnetic flux as an input to a simple spherically symmetric quasi-steady
  state model of the heliosphere, we calculate the expected differential
  spectra and integral intensity of galactic cosmic rays at the Earth's
  orbit since 1610. The calculated cosmic ray integral intensity is in
  good agreement with the neutron monitor measurements during the last
  50 years. Moreover, using the specific yield function of cosmogenic
  10 Be radionuclide production in the atmosphere, we also calculate
  the expected 10 Be production rate which exhibits an excellent
  agreement with the actual 10 Be abundance in polar ice over the
  last 400 years. Here we present a physical model for the long-term
  reconstruction of cosmic ray intensity at 1 AU. The reconstruction
  is based on a combination of the solar magnetic flux model and a
  heliospheric model. This model allows us to calculate the expected
  intensity of galactic cosmic rays (GCR) at the Earth's orbit for the
  last 400 years. Details can be found in [25]. Using the numerical recip
  e of Solanki et al. [21] and the group sunspot number series (Fig. 1.a)
  [11] we have calculated the open solar magnetic flux Fo since 1610 as
  shown in Fig. 1.b. In order to calculate galactic cosmic ray (GCR)
  spectra we use a spherically symmetric quasi-steady sto chastic
  simulation model described in detail elsewhere [24], which reliably
  describes the long-term GCR modulation during the last 50 years. In this
  model, the most important parameter of the heliospheric modulation of
  GCR is the modulation strength [10]: Φ = (D - rE )V /(3κo), where D
  = 100 AU is the heliospheric boundary and rE = 1 AU, V = 400 km/s is
  the constant solar wind velocity and κo is the rigidity indep endent
  part of the diffusion coefficient. Thus, all changes in the modulation
  strength Φ in our model are related to the changing diffusion

---------------------------------------------------------
Title: Long-Term Cosmic Ray Modulation by Heliospheric Parameters:
    Non-linear Relations
Authors: Usoskin, I. G.; Kovaltsov, G. A.; Mursula, K.; Alkano, K.
2003ICRC....7.3803U    Altcode: 2003ICRC...28.3803U
  The heliospheric modulation strength is a good parameter for the
  long-term modulation of cosmic rays in the neutron monitor energy
  range. Here we study an empirical relation between the modulation
  strength and the global heliospheric parameters: the heliospheric
  current sheet tilt angle, the open solar magnetic flux and the global
  IMF polarity. The suggested relation closely repro duces the measured
  annual NM count rates. Using the measured IMF parameters and the
  modulation strength values computed since 1951, this relation allows
  us to reconstruct the annual tilt angle for about 25 years before
  the time of direct measurements of the tilt angle. In addition to more
  sophisticated theoretical models of galactic cosmic ray (GCR) modulation
  it is also useful to study empirical regression models. Usually
  such models linearly relate various heliospheric parameters to the
  GCR intensity at a fixed energy (see, e.g., [2]). Here we try to
  generalize this approach. A general parameter of the heliospheric
  modulation of GCR is the modulation strength Φ, which defines the
  shape of the modulated GCR spectrum for many practical purposes. E.g.,
  for a given value of Φ one can calculate an approximate shape of GCR
  differential energy spectrum and the expected count rate of a cosmic
  ray detector [1], [11]. The modulation strength is measured in MV,
  has the physical meaning of the average rigidity loss of CR particles
  in the heliosphere and takes the following form [4] Φ = (D - rE )V
  /(3κo ), where D is the distance of heliospheric boundary (termination
  shock), rE = 1 AU, V is the solar wind velocity and κo is the (rigidity
  indep endent part of the) GCR diffusion coefficient. Although defined
  only in 1D, Φ can also be used in the real conditions as a formal
  parameter that fits GCR spectra calculated in 1D model to the actual
  GCR spectrum measured at 1 AU. The values of Φ have been calculated
  for the last 50 years [11]. However, here we use an up dated Φ series
  (Fig. 1.a) where heavier species of GCR (α-particles) are also taken
  into account. The value of Φ depends on several global heliospheric
  parameters as discussed below. In con-

---------------------------------------------------------
Title: The lost sunspot cycle: Reanalysis of sunspot statistics
Authors: Usoskin, I. G.; Mursula, K.; Kovaltsov, G. A.
2003A&A...403..743U    Altcode:
  We have recently suggested that one low sunspot cycle was possibly lost
  in 1790s (Usoskin et al. 2001, A&amp;A, 370, L31). In this paper we
  present the results of a rigorous statistical analysis of all available
  sunspot observations around the suggested additional cycle minimum in
  1792-1793. First we estimate the uncertainty of a monthly mean sunspot
  number reconstructed from a single daily observation. Then we compare,
  using quantitative statistical tests, the average level of sunspot
  activity in 1792-1793 with the average activity during the minimum,
  mid-declining and maximum phases of cycles in the well-measured
  reference period 1850-1996. We show that, contrary to the results by
  Krivova et al. (2002), the level of sunspot activity in 1792-1793 is
  statistically similar to that in the minimum phase, and significantly
  different from that in the mid-declining and maximum phases. Using the
  estimated uncertainties, we also calculate new, weighted annual values
  of R<SUB>g</SUB> in 1790-1796 which show a clear minimum in 1792-1793
  and a maximum in 1794-1795, supporting the idea of an additional weak
  cycle in 1790's.

---------------------------------------------------------
Title: Reconstructing the long-term cosmic ray intensity: linear
    relations do not work
Authors: Mursula, K.; Usoskin, I. G.; Kovaltsov, G. A.
2003AnGeo..21..863M    Altcode:
  It was recently suggested (Lockwood, 2001) that the cosmic ray intensity
  in the neutron monitor energy range is linearly related to the coronal
  source flux, and can be reconstructed for the last 130 years using the
  long-term coronal flux estimated earlier. Moreover, Lockwood (2001)
  reconstructed the coronal flux for the last 500 years using a similar
  linear relation between the flux and the concentration of cosmogenic
  10 Be isotopes in polar ice. Here we show that the applied linear
  relations are oversimplified and lead to unphysical results on long
  time scales. In particular, the cosmic ray intensity reconstructed
  by Lockwood (2001) for the last 130 years has a steep trend which is
  considerably larger than the trend estimated from observations during
  the last 65 years. Accordingly, the reconstructed cosmic ray intensity
  reaches or even exceeds the local interstellar cosmic ray flux around
  1900. We argue that these unphysical results obtained when using
  linear relations are due to the oversimplified approach which does
  not take into account the complex and essentially nonlinear nature of
  long-term cosmic ray modulation in the heliosphere. We also compare
  the long-term cosmic ray intensity based on a linear treatment with
  the reconstruction based on a recent physical model which predicts a
  considerably lower cosmic ray intensity around 1900.

---------------------------------------------------------
Title: The lost sunspot cycle: Reanalyzing the sunspot statistics
Authors: Usoskin, I. G.; Mursula, K.; Kovaltsov, G. A.
2003EAEJA.....8819U    Altcode:
  It has been recently suggested that one sunspot cycle was possibly lost
  in 1790s (Usoskin et al., 2001, A&amp;A, 370, L31). Here we present
  results of a rigorous statistical analysis of all available sunspot
  observations around 1792-1793, when the additional cycle minimum was
  suggested to occur. First we estimate the uncertainty of a monthly
  sunspot number mean which consists of a single daily observation. Then
  we compare, using quantitative statistical tests, the pattern of sunspot
  activity in 1792-1793 and during the minimum, mid-declining and maximum
  phases of well-measured cycles in the reference period of 1850-1996. We
  show that the pattern of sunspot activity in 1792-1793 is statistically
  similar to that in the minimum phase, and significantly different
  from that in the mid-declining and maximum phases. We calculate the
  weighted annual values of R_g in 1790-1796 which clearly show a small
  cycle starting in 1793 and reaching its maximum in 1795. We discuss
  that the possible existence of a new cycle does not contradict to the
  indirect proxies of solar activity (e.g., cosmogenic isotope data). We
  also discuss the implications of the new cycle for solar activity,
  in particular for the cycle length distribution, the Gnevyshev-Ohl
  rule and the Waldmeier relation between the cycle amplitude and the
  length of the ascending and descending phase.

---------------------------------------------------------
Title: Lost sunspot cycle in the beginning of Dalton minimum: New
    evidence and consequences
Authors: Usoskin, I. G.; Mursula, K.; Kovaltsov, G. A.
2002GeoRL..29.2183U    Altcode: 2002GeoRL..29x..36U
  We have recently suggested that one solar cycle was lost in the
  beginning of the Dalton minimum during 1790s [Usoskin et al.,
  2001]. Earlier, this cycle has been combined with the preceding
  activity to form the exceptionally long solar cycle 4 in 1784-1799
  with an irregular phase evolution. Here we show that historical data
  of auroral occurrence provide independent evidence for the existence
  of the new cycle. Using a heliospheric model we demonstrate that
  <SUP>10</SUP>Be or any other cosmogenic isotope data do not exclude
  the possibility of a new cycle. We also discuss the other implications
  of the new cycle for solar activity, in particular the cycle length
  distribution and the Waldmeier relation between the cycle amplitude
  and the length of the ascending and descending phase. Including the
  new cycle also restores the Gnevyshev-Ohl rule of cycle pairing and
  removes the phase catastrophe in the beginning of the Dalton minimum.

---------------------------------------------------------
Title: Simulating regularity and randomness in sunspot activity
Authors: Usoskin, I. G.; Mursala, K.; Kovaltsov, G. A.
2002ESASP.506..863U    Altcode: 2002svco.conf..863U; 2002ESPM...10..863U
  The time series of sunspot activity displays both regular features
  and randomness, and their interrelation has been studied during last
  decades. We present here a model of sunspot production which employs
  three components of solar magnetic field: the 22-year dynamo field, a
  weak constant relic field, and a randomly fluctuating field. Within this
  model, sunspots are produced when the total field exceeds the buoyancy
  threshold. This model can reproduce the main features of sunspot
  activity throughout the 400-year period of direct solar observations,
  including two different sunspot activity modes, the present, normal
  sunspot activity and the Maunder minimum. The two sunspot activity
  modes could be modeled by only changing the level of the dynamo field
  while keeping the other two components constant. We discuss the role
  of the three components and how their relative importance changes
  between normal activity and great minimum times. We found that the
  relic field must be about few per cent of the dynamo field in normal
  activity times. Also, we find that the dynamo field during the Maunder
  minimum was small but non-zero, being suppressed typically by an order
  of magnitude with respect to its value during normal activity times.

---------------------------------------------------------
Title: A physical reconstruction of cosmic ray intensity since 1610
Authors: Usoskin, Ilya G.; Mursula, Kalevi; Solanki, Sami K.;
   Schüssler, Manfred; Kovaltsov, Gennady A.
2002JGRA..107.1374U    Altcode:
  The open solar magnetic flux has been recently reconstructed by [2000,
  2002] for the last 400 years from sunspot data. Using this reconstructed
  magnetic flux as an input to a spherically symmetric quasi-steady
  state model of the heliosphere, we calculate the expected intensity
  of galactic cosmic rays at the Earth's orbit since 1610. This new,
  physical reconstruction of the long-term cosmic ray intensity is
  in good agreement with the neutron monitor measurements during the
  last 50 years. Moreover, it resolves the problems related to previous
  reconstruction for the last 140 years based on linear correlations. We
  also calculate the flux of 2 GeV galactic protons and compare it to
  the cosmogenic <SUP>10</SUP>Be level in polar ice in Greenland and
  Antarctica. An excellent agreement between the calculated and measured
  levels is found over the last 400 years.

---------------------------------------------------------
Title: Heliospheric modulation strength during the neutron monitor era
Authors: Usoskin, I. G.; Alanko, K.; Mursula, K.; Kovaltsov, G. A.
2002SoPh..207..389U    Altcode:
  Using a stochastic simulation of a one-dimensional heliosphere we
  calculate galactic cosmic ray spectra at the Earth's orbit for different
  values of the heliospheric modulation strength Φ. Convoluting these
  spectra with the specific yield function of a neutron monitor, we
  obtain the expected neutron monitor count rates for different values
  of Φ. Finally, inverting this relation, we calculate the modulation
  strength using the actually recorded neutron monitor count rates. We
  present the reconstructed annual heliospheric modulation strengths for
  the neutron monitor era (1953-2000) using several neutron monitors from
  different latitudes, covering a large range of geomagnetic rigidity
  cutoffs from polar to equatorial regions. The estimated modulation
  strengths are shown to be in good agreement with the corresponding
  estimates reported earlier for some years.

---------------------------------------------------------
Title: Long-term cosmic ray intensity vs. solar proxies: a simple
    linear relation does not work
Authors: Mursula, K.; Usoskin, I. G.; Kovaltsov, G. A.
2002ESASP.477..463M    Altcode: 2002scsw.conf..463M
  It was recently suggested (Lockwood et al., 2000; 2001) that the cosmic
  ray intensity in the neutron monitor energy range is linearly related
  to coronal source flux, and can be reconstructed for 130 years using
  the estimated long term coronal flux. Moreover, by reversing this
  relation, they reconstructed the coornal flux on the 500-year scale
  using the cosmogenic <SUP>10</SUP>Be data as an index of cosmic ray
  intensity. Here we show that a linear regression is oversimplified
  and leads to unphysical results on long time scales. In particular,
  the reconstructed cosmic ray intensity has a steep trend which is four
  times larger than the allowed upper bound. The reconstructed cosmic
  ray intensity exceeds the local interstellar cosmic ray flux around
  1900. We argue that the unphysical results using a linear assumption
  are due to the oversimplified approach which does not account for
  complexity and significant nonlinearity of cosmic ray modulation in
  the heliosphere. We show also that there is no homogeneous linear
  relation between coronal source flux and cosmic rays.

---------------------------------------------------------
Title: The start of the Dalton minimum: Was one sunspot cycle lost
    in late XVIII century?
Authors: Usoskin, I. G.; Mursula, K.; Kovaltsov, G. A.
2002ESASP.477..257U    Altcode: 2002scsw.conf..257U
  We have recently suggested that one solar cycle was lost in the
  beginning of the Dalton minimum because of sparse and partly unreliable
  sunspot observations during 1790s (Usoskin et al. 2001). So far
  this cycle has been combined with the preceding activity to form the
  exceptionally long solar cycle #4 in 1784 - 1799 which has an irregular
  phase evolution (known as the phase catastrophe) and other problems
  discussed in earlier literature. Based on a re-analysis of available
  sunspot data, we have suggested that solar cycle #4 is in fact a
  superposition of two cycles: a normal cycle in 1784 - 1793 ending at
  the start of the Dalton minimum, and a new weak cycle in 1793 - 1800
  which was the first cycle within the Dalton minimum. Including the new
  cycle resolves the phase catastrophe and leads to a consistent view
  of sunspot activity around the Dalton minimum. It also restores the
  Gnevyshev-Ohl rule of cycle pairing across the Dalton minimum. Here
  we summarize these findings and show that the existence of a new cycle
  is supported by the auroral occurrence in Europe in late XVIII century.

---------------------------------------------------------
Title: A 22-year cycle in sunspot activity
Authors: Mursula, K.; Usoskin, I. G.; Kovaltsov, G. A.
2002AdSpR..29.1979M    Altcode:
  We study the recently presented group sunspot number series and show
  that a persistent 22-year periodicity exists in sunspot activity
  throughout the entire period of about 400 years of direct sunspot
  observations. The amplitude of this periodicity in total cycle intensity
  is about 20% of the present intensity level. A 22-year periodicity
  in sunspot activity is naturally produced by the 22-year magnetic
  dynamo cycle in the presence of a relic magnetic field. Accordingly,
  a persistent 22-year periodicity in sunspot activity gives strong
  evidence for the existence of such a relic magnetic field in the
  Sun. The stable phase and the roughly constant amplitude of this
  periodicity during times of very different sunspot activity level
  strongly support this interpretation.

---------------------------------------------------------
Title: Heliospheric Modulation Strength During The Neutron Monitor Era
Authors: Usoskin, I. G.; Alanko, K.; Mursula, K.; Kovaltsov, G. A.
2002EGSGA..27.3884U    Altcode:
  Using a stochastic simulation of a one-dimensional heliosphere we
  calculate galactic cosmic ray spectra at the Earth's orbit for different
  values of the heliospheric mod- ulation strength. Convoluting these
  spectra with the specific yield function of a neu- tron monitor, we
  obtain the expected neutron monitor count rates for different values of
  the modulation strength. Finally, inverting this relation, we calculate
  the modula- tion strength using the actually recorded neutron monitor
  count rates. We present the reconstructed annual heliospheric modulation
  strengths for the neutron monitor era (1953­2000) using several
  neutron monitors from different latitudes, covering a large range of
  geomagnetic rigidity cutoffs from polar to equatorial regions. The
  estimated modulation strengths are shown to be in good agreement with
  the corresponding esti- mates reported earlier for some years.

---------------------------------------------------------
Title: Missed sunspot cycle in late XVIII century: new evidences
Authors: Usoskin, I.; Mursula, K.; Nevanlinna, H.; Kovaltsov, G.
2002cosp...34E.862U    Altcode: 2002cosp.meetE.862U
  We suggest that one solar cycle was lost in the beginning of the
  Dalton minimum because of sparse and partly unreliable sunspot
  observations during 1790s. So far this cycle has been combined
  with the preceding activity to form the exceptionally long solar
  cycle #4 in 1784-1799 which has an irregular phase evolution (known
  as the phase catastrophe) and other problems discussed in earlier
  literature. Based on a reanalysis of available sunspot data, we have
  suggested that solar cycle #4 is in fact a superposition of two cycles:
  a normal cycle in 1784-1793 ending at the start of the Dalton minimum,
  and a new weak cycle in 1793-1800 which was the first cycle within the
  Dalton minimum. Including the new cycle resolves the phase catastrophe
  and leads to a consistent view of sunspot activity around the Dalton
  minimum. It also restores the Gnevyshev-Ohl rule of cycle pairing across
  the Daltom nimimum. Here we summarize these findings and present new
  independent geomagnetic evidences favouring the existence of a new
  cycle in late XVIII century. We also show that the available data
  of cosmogenic isotopes 10 B e and 14 C cannot serve as a test of the
  existence of the new cycle.

---------------------------------------------------------
Title: Heliospheric modulation strength during the neutron monitor era
Authors: Usoskin, I.; Alanko, K.; Mursula, K.; Kovaltsov, G.
2002cosp...34E.868U    Altcode: 2002cosp.meetE.868U
  The heliospheric modulation strengthis an important quantitative
  measure of the efficiency of heliospheric modulation of cosmic rays,
  however, it is not easy to estimate it in practice. Here we suggest a
  physical estimate of the modulation strength on yearly time scale from
  data of the neutron monitor network. Using a stochastic simulation
  of a one-dimensional heliosphere we calculate galactic cosmic ray
  spectra at the Earth's orbit for different values of the heliospheric
  modulation strength . Convoluting these spectra with the specific
  yield function of a neutron monitor, we obtain the expected neutron
  monitor count rates for different values of . Finally, inverting this
  relation, we calculate the modulation strength using the actually
  recorded neutron monitor count rates. We present the reconstructed
  annual heliospheric modulation strengths for the neutron monitor era
  (1951-2000) using several neutron monitors from different latitudes,
  covering a large range of geomagnetic rigidity cutoffs from polar to
  equatorial regions. The estimated modulation strengths are shown to
  be consistent among different neutron monitors and in good agreement
  with the corresponding estimates reported earlier for some years.

---------------------------------------------------------
Title: Physical reconstruction of the long-term heliospheric
    modulation of cosmic rays
Authors: Usoskin, I.; Mursula, K.; Solanki, S.; Shuessler, M.;
   Kovaltsov, G.
2002cosp...34E.902U    Altcode: 2002cosp.meetE.902U
  Open solar magnetic flux has been recently reconstructed by Solanki
  et al. (2000, 2002) for the last 400 years from sunspot data. Using
  this reconstructed magnetic flux as an input to a spherically symmetric
  quasi-steady state model of the heliosphere, we calculate the expected
  intensity of galactic cosmic rays at the Earth's orbit since 1610. This
  calculated cosmic ray intensity is in good agreement with the neutron
  monitor measurements during the last 50 years. Moreover, we calculate
  the flux of 2 GeV galactic protons and compare it to the cosmogenic
  10 B e level in polar ice in Greenland and Antarctica. An excellent
  agreement between the calculated and actual levels is found over the
  last 400 years.

---------------------------------------------------------
Title: Long-term Cosmic Ray Intensity Vs. Solar Proxies: A Simple
    Linear Relation Does Not Work
Authors: Mursula, K.; Usoskin, I. G.; Kovaltsov, G. A.
2002EGSGA..27.3882M    Altcode:
  It was recently suggested (Lockwood et al., 2000; 2001) that the cosmic
  ray intensity in the neutron monitor energy range is linearly related
  to coronal source flux, and can be reconstructed for 130 years using the
  estimated long term coronal flux. Moreover, by reversing this relation,
  they reconstructed the coronal flux on the 500-year scale us- ing
  the cosmogenic 10Be data as an index of cosmic ray intensity. Here we
  show that a linear regression is oversimplified and leads to unphysical
  results on long time scales. In particular, the reconstructed cosmic ray
  intensity has a steep trend which is four times larger than the allowed
  upper bound. The reconstructed cosmic ray intensity ex- ceeds the local
  interstellar cosmic ray flux around 1900. We argue that the unphysical
  results using a linear assumption are due to the oversimplified approach
  which does not account for complexity and significant nonlinearity of
  cosmic ray modulation in the heliosphere. We show also that there is no
  homogeneous linear relation between coronal source flux and cosmic rays.

---------------------------------------------------------
Title: Was One Sunspot Cycle Lost In Late Xviii Century?
Authors: Usoskin, I. G.; Mursula, K.; Kovaltsov, G. A.
2002EGSGA..27.3897U    Altcode:
  We suggest that one solar cycle was lost in the beginning of the Dalton
  minimum because of sparse and partly unreliable sunspot observations
  during 1790s. So far this cycle has been combined with the preceding
  activity to form the exceptionally long solar cycle #4 in 1784­1799
  which has an irregular phase evolution (known as the phase catastrophe)
  and other problems discussed in earlier literature. Based on a re-
  analysis of available sunspot data, we have suggested that solar
  cycle #4 is in fact a superposition of two cycles: a normal cycle
  in 1784­1793 ending at the start of the Dalton minimum, and a new
  weak cycle in 1793­1800 which was the first cycle within the Dalton
  minimum. Including the new cycle resolves the phase catastrophe and
  leads to a consistent view of sunspot activity around the Dalton
  minimum. It also restores the Gnevyshev-Ohl rule of cycle pairing
  across the Daltom nimimum. Here we summarize these findings and show
  that the existence of a new cycle is supported by the auroral occurrence
  in Europe in late XVIII century.

---------------------------------------------------------
Title: Reconstruction of Cosmic Ray Intensity Since 1610
Authors: Usoskin, I. G.; Mursula, K.; Solanki, S. K.; Schüssler,
   M.; Kovaltsov, G. A.
2002EGSGA..27.5173U    Altcode:
  Open solar magnetic flux has been recently reconstructed by Solanki
  et al. (2000, 2002) for the last 400 years from sunspot data. Using
  this reconstructed magnetic flux as an input to a spherically symmetric
  quasi-steady state model of the heliosphere, we calculate the expected
  intensity of galactic cosmic rays at the Earth's orbit since 1610. This
  calculated cosmic ray intensity is in good agreement with the neutron
  monitor measurements during the last 50 years. Moreover, we calculate
  the flux of 2 GeV galactic protons and compare it to the cosmogenic
  10Be level in polar ice in Greenland and Antarctica. An excellent
  agreement between the calculated and actual levels is found over the
  last 400 years.

---------------------------------------------------------
Title: Persistent active longitudes in sunspot activity
Authors: Berdyugina, S.; Usoskin, I.
2002cosp...34E.864B    Altcode: 2002cosp.meetE.864B
  It has been recently shown that spot activity of cool stars
  including solar analogues, is grouped in two clearly distinguished
  active longitudes which are persistent within at least one starspot
  cycle. Solar data including positional information of individual
  sunspots / groups extends back for about 130 years covering 12 solar
  cycles. Here we present the results of our research of longitudinal
  distribution of sunspot activity using an analysis similar to
  that applied to the stars. First, we synthesized, from the actual
  sunspot data, the sun's light curve as if it was defined only by
  spots. Then solar images were calculated from this light curve, giving
  a natural smoothing of the spot pattern. For each Carrington rotation,
  longitudinal position of these smoothed spot regions was calculated. The
  analysis reveals the following main features: - Sunspot activity
  is grouped in two active longitudes (with the differential rotation
  taken into account) 180o apart from each other which are persistent
  through the entire studied period of 12 cycles, similarly to stars. -
  The longitude migration is determined by changing the mean latitude of
  sunspot activity (the Maunder butterfly) and differential rotation. -
  The two longitudes periodically alternate the dominant activity with
  about 3.7 year period implying for the existence of the Sflip-flopT
  phenomenon known in - starspot activity.

---------------------------------------------------------
Title: Physical reconstruction of long-term solar activity
Authors: Usoskin, I.; Solanki, S.; Schuessler, M.; Mursula, K.;
   Kovaltsov, G.
2002cosp...34E.901U    Altcode: 2002cosp.meetE.901U
  For many applications in dynamo theory and solar-terrestrial research
  it is important to know the evolution of solar activity on long time
  scales (centuries to millennia). Previous reconstructions were based
  upon either multi-harmonic backward extrapolation of the known sunspot
  records or on the assumption of a linear relation between terrestrial
  proxies (e.g., cosmogenic isotope abundance) and solar activity. Here
  we present, for the first time, a physical reconstruction of sunspot
  activity on long time scales from the cosmogenic 10 Be records. We
  use a numerical inversion of a combined physical solar-heliospheric
  model (Usoskin et al., 2002), which is essentially non-linear. Using
  physical rather than empirical relations on all steps, we present a
  reconstruction of sunspot activity since the 15th century. Uncertainties
  of the reconstruction are discussed in details. It is important that
  the current high level of sunspot activity is unique on the millennium
  time scale.

---------------------------------------------------------
Title: Direct penetration of anisotropic solar proton flux through
the postnoon magnetopause: evidence of magnetosphere anomaly?
Authors: Vashenyuk, E.; Gvozdevsky, B.; Pchelkin, V.; Usoskin, I.;
   Mursula, K.; Kovaltsov, G.
2002cosp...34E2095V    Altcode: 2002cosp.meetE2095V
  Count rates of two closely located neutron monitors (NMs) at Oulu and
  Apatitysometimes depicted an unusually different behavior during an
  anisotropic onsetphase of a number of ground level enhancements (GLEs)
  caused by relativisticsolar cosmic rays. Of 24 years of observations
  ( 27 GLE) there were revealed 4 suchcases. In all of them the NM with
  a higher count rate (Oulu on 2 May 1998 and 15April 2001, Apatity on
  23 September, 1978 and 14 July 2000) was located in the so-called 14
  MLT region (14-16 hours of Magnetic Local Time) known as location
  ofintense field aligned currents, dayside auroras etc. At the same
  time the calculatedasymptotic cones of Apatity and Oulu stations
  were "looking" under the large angleto an IMF direction and in any
  way could not accept an anisotropic solar proton fluxpropagating
  along the IMF. Nevertheless one of the station pair which was
  locatedinside the 14-16 MLT sector showed an excess in count rate due to
  anisotropicfraction of solar proton flux. Together with the Apatity and
  Oulu NMs data ouranalysis comprised also the data on the worldwide NM
  network as well ascomputation of their asymptotic cones These were done
  by means of trajectorycalculations in the up -to date magneto pheric
  models of Tsyganenko 1989 and 1996.sOn the basis of observed data we
  can assume, that the cause of marked unusualdifference between Apatity
  and Oulu GLE effect can be the not discounted anomalyin the afternoon
  magnetosphere. .It can be connected, for example to the structure
  ofnagnetospheric cleft. The noted here effect specifies necessity of
  additional study ofmagnetosphere structure in the afternoon sector
  that may be a subject to occurringhere intensive geophysical processes.

---------------------------------------------------------
Title: Nitrate abundance in polar ice during the great solar activity
    minimum
Authors: Gladysheva, O. G.; Kocharov, G. E.; Kovaltsov, G. A.; Usoskin,
   I. G.
2002AdSpR..29.1707G    Altcode:
  In the present paper we study variations of the nitrate content in
  Greenland ice core for the last 400 years. These data were obtained by
  high-precision measurements performed by the University of Kansas. It
  is shown that approximately 20-year periodicity dominates in the
  nitrate series during the Maunder minimum (1645-1715) due to similar
  variations of galactic cosmic ray intensity. During times of normal
  high solar activity level, the 4-6-year periodicity dominates in the
  nitrate series. This is probably due to a superposition of fluxes of
  galactic and solar cosmic rays, and due to the creation of favourable
  conditions for the nitrate precipitation.

---------------------------------------------------------
Title: Evidence for charge drift modulation at intermediate solar
    activity from the flux variation of protons and α particles
Authors: Boella, G.; Gervasi, M.; Mariani, S.; Rancoita, P. G.;
   Usoskin, I. G.
2001JGR...10629355B    Altcode:
  We have studied the flux of galactic protons and helium nuclei measured
  at 1 AU along two consecutive solar activity cycles. We have correlated
  cosmic ray fluxes measured on IMP 8 satellite at low energy (50-300
  MeV amu<SUP>-1</SUP>) with neutron monitor counts registered at Climax
  station (at energies above few GeV) during the period 1973-1995. We have
  found a systematic excess in the flux of the positive charged particles
  during the periods with positive solar magnetic field polarity (A&gt;0)
  with respect to the flux during the periods of negative polarity
  (A&lt;0). This flux excess gives an experimental evidence that charge
  drift effect plays an important role in the modulation of galactic
  cosmic rays. A systematic investigation of charge drift modulation is
  presented. The dependence of the drift effect on the solar activity
  phase and the particle energy has been also studied. A variation of
  the proton (as well as helium) flux might be as large as 40%, at the
  solar activity minimum of two contiguous cycles, at energy &lt;=100 MeV.

---------------------------------------------------------
Title: Nitrate abundance in polar snow during last 50 year: connection
    to atmospheric ionization
Authors: Gladysheva, O. G.; Dmitriev, P. B.; Usoskin, I. G.; Barkov,
   N. I.; Ekaykin, A. A.; Nikanorov, V. V.
2001ICRC...10.4191G    Altcode: 2001ICRC...27.4191G
  A few yearly series of the nitrate abundance in polar snow are
  studied. One of them has been measured in the snow samples collected
  in a pit dug at russian Vostok Station (East Antarctic). The other
  series has been obtained in Antarctic and Greenland. The studied time
  interval covers the last 50 years. These series are influenced by
  different local terrestrial drivers while the extraterrestrial force
  is similar. The nitrate series are analysed along with calculations of
  the cosmic ray induced ionisation of the upper atmosphere. A relative
  role of extraterrestrial factors, in particular of strong solar proton
  events, is discussed.

---------------------------------------------------------
Title: The MUG experiment for observing muon fluxes underground:
    test data and development plans
Authors: Elo, A. -M.; Jaemsen, T.; Kangas, J.; Mursula, K.; Peltoniemi,
   J.; Usoskin, I. G.; Vallinkoski, M.; Valtonen, E.
2001ICRC....3.1249E    Altcode: 2001ICRC...27.1249E
  A new multilevel Muons UnderGround experiment (MUG) for observing
  muon fluxes underground is located in the Pyh¨asalmi zinc mine in
  Central Finland. The detectors consist of vertically overlapping plastic
  scintillator pairs. Three scintillator pairs are situated on the ground
  level. Six pairs are 90 metres un-derground and another six pairs
  are 210 metres underground. The counting rates of coincident pulses
  in scintillator pairs are recorded in the preliminary phase of the
  experiment. In this paper we study the test data obtained with the MUG
  instruments in order to check the acceptability of their operation. One
  purpose of the MUG experiment is to investigate the suitability of
  the Pyhasalmi mine as a location for scientific experiments. The test
  data are also examined in this respect. Development plans for the MUG
  experiment are also outlined in this paper.

---------------------------------------------------------
Title: Geomagnetic cutoff Penumbra structure: approach by
    transmissivity function
Authors: Bobik, P.; Kudela, K.; Usoskin, I.
2001ICRC...10.4056B    Altcode: 2001ICRC...27.4056B
  Numerical tracing of cosmic ray trajectories in the model magnetospheric
  field is widely used to understand the "magnetospheric optics" of the
  Earth's magnetosphere for primary cosmic rays and their access to ground
  based observation sites. Recent review on the subject can be found,
  e.g. in (Smart et al., 2000). Penumbra structure is usually described
  as a system of allowed and forbidden trajectories (A,F) between low,
  RL , and upper, RU , cutoff rigidities. The probability of a particle
  in a given rigidity interval within (RL,RU) to access the position of a
  cosmic ray station, the transmissivity function TF, is deduced from the
  (A,F) structure which is dependent on the elementary step in rigidity
  for computations, on local time (if the external field is included) and
  on the geomagnetic activity level. We study TF using Tsyganenko'89 field
  model with rigidity steps ∼R=10-5 GV - 10-1 GV, for the high latitude
  Oulu site (65.05o N 25.47o E). We illustrate the penumbra structure
  in terms of the divergence of asymptotic direction of neighbouring
  allowed trajectories. The TF function weighted statistically by the
  Kp distribution over long time may serve as a tool for CR transparency
  characteristic at a particular station.

---------------------------------------------------------
Title: A new multilevel experiment MUG for observing muon fluxes
    underground
Authors: Jaemsen, T.; Elo, A. -M.; Kangas, J.; Mursula, K.; Peltoniemi,
   J.; Usoskin, I. G.; Vallinkoski, M.; Valtonen, E.
2001ICRC....3.1250J    Altcode: 2001ICRC...27.1250J
  We describe a new Muons UnderGround experiment (MUG) for observing
  muon uxes underground. The experiment is situated in the Pyhasalmi
  zinc mine in Central Finland. The muon detectors consist of two
  vertically overlapping plastic scintillators. Six pairs of detectors
  are located 210 metres underground, another six pairs 90 metres
  underground, and three pairs are on the ground level. The dimensions
  of the scintillators are 50 cm × 50 cm in the horizontal plane
  and their thickness is 5 cm. Each scintillator is equipped with a
  Hamamatsu R329-02 photomultiplier tube with fast time response. In the
  preliminary phase of the experiment the counting rates of coincidences
  of the scintillator pairs are recorded. In this paper we describe the
  detectors and the experimental setup in more detail.

---------------------------------------------------------
Title: Heliospheric modulation strength during the neutron monitor
    epoch
Authors: Usoskin, I. G.; Alanko, K.; Mursula, K.; Kudela, K.;
   Kovaltsov, G. A.
2001ICRC....9.3810U    Altcode: 2001ICRC...27.3810U
  Using a simple stochastic 1D simulation model of the heliosphere we
  calculate galactic cosmic ray spectra at the Earth's orbit for different
  values of the heliospheric modulation strength Φ. Convoluting these
  spectra with the specific yield function of a neutron monitor, we obtain
  the expected neutron monitor count rates for different values of Φ. We
  present here a normalization method which allows to easily estimate
  the value of Φ on the basis of actually recorded neutron monitor
  count rates. By means of this approach we estimate the heliospheric
  modulation strength for the neutron monitor era using long-term records
  of count rates from the high-latitude Oulu and mid-latitude Hermanus
  neutron monitors.

---------------------------------------------------------
Title: The GLE of 14 July 2000: comparative analysis of increase
    effect on close neutron monitors in Apatity and Oulu
Authors: Vashenyuk, E. V.; Gvozdevsky, B. B.; Phelkin, V. V.; Usoskin,
   I. G.; Mursula, K.; Kovaltsov, G. A.
2001ICRC....8.3383V    Altcode: 2001ICRC...27.3383V
  Count rates of two closely located neutron monitors (NMs) at Oulu and
  Apatity depicted an unusually different behaviour during the onset
  phase of the ground- level enhancement (GLE) of 14 July 2000. Similar
  differences were observed during the onsets of GLEs of 2 May 1998
  and 15 April 2001. All these three events took place after a strong
  Forbush decrease, implying significantly disturbed interplanetary
  and geomagnetic conditions. In all cases the NM with a higher count
  rate (Oulu on 2 May 1998 and 15 April 2001, Apatity on 14 July 2000)
  was located in the so-called 14 MLT region (1416 hours of Magnetic
  Local Time) where the maximum dayside auroral intensity and some
  other anomalous geophysical phenomena are located. Here we analyse
  these events using data from Apatity, Oulu and some other NMs,
  as well as their asymptotic cones calculated using the Tsyganenko
  1989 magnetospheric model. We suggest that there is an anomaly in
  magnetospheric structure in the 14 MLT sector which facilitates the
  penetration of cosmic ray protons from the dayside magnetopause to
  the ground.

---------------------------------------------------------
Title: Heliospheric modulation of cosmic rays and solar activity
    during the Maunder minimum
Authors: Usoskin, Ilya G.; Mursula, Kalevi; Kovaltsov, Gennady A.
2001JGR...10616039U    Altcode:
  Modern models and direct cosmic ray experiments deal with heliospheric
  modulation of cosmic rays only during the recent times of rather
  high overall solar activity level. On the other hand, the question
  of cosmic ray modulation during the exceptional conditions of very
  quiet heliosphere is important. In the present paper we compare the
  variations of cosmic ray intensity with solar and auroral activity
  during the Maunder minimum (1645-1715) when the Sun was extremely
  quiet. We use the newly presented group sunspot number series as a
  measure of early solar activity, the auroral observations in central
  Europe as an indicator of transient phenomena in the inner heliosphere,
  and the radiocarbon data as a proxy of cosmic ray intensity. We find
  that both cosmic ray intensity and auroral activity closely follow
  the dominant 22-year cyclicity with sunspot activity during the
  Maunder minimum. Moreover, the strict antiphase between the 22-year
  variation of cosmic ray intensity and sunspot activity suggests that
  the 22-year variation in cosmic ray intensity can be explained by the
  diffusion-dominated terms of cosmic ray modulation without significant
  drift effects. We also discuss the possible origin of the behavior of
  the <SUP>10</SUP>Be data which is different from all other parameters
  during the Maunder minimum.

---------------------------------------------------------
Title: On-Line Database of Cosmic Ray Intensities*
Authors: Usoskin, I. G.; Mursula, K.; Kangas, J.
2001ICRC....9.3842U    Altcode: 2001ICRC...27.3842U
  Cosmic ray measurements in Oulu (65.05 o N, 25.47 o E) started in 1964
  with a standard 9-NM-64 neutron monitor. The 9-NM-64 neutron monitor
  consists of three independent units, each made of three proportional
  gas counters. The local vertical geomagnetic cutoff rigidity is about
  0.8 GV. The NM at Oulu is one of the most stable and reliable stations
  of the World Neutron Monitor Net-work. We have recently launched a
  web service of the Oulu NM data. All data on cosmic ray intensity
  as recorded by the Oulu NM since 1964 are available in a searchable
  on-line database at the URL: http://cosmicrays.oulu.fi The database
  contains 1-min resolution data since 1995, 5min resolution data since
  1985, and hourly data since 1964, as well as the full information
  about the reliability and stability of the recorded cosmic ray
  intensities. Besides, 10-sec uncorrected data are available since 1990
  upon special requests. *To the memory of the late NM station manager
  Hannu Kananen

---------------------------------------------------------
Title: Cosmogenic Variations of Nitrate Abundance in Polar Ice
Authors: Gladysheva, O. G.; Kocharov, G. E.; Kovaltsov, G. A.; Usoskin,
   I. G.
2001ICRC...27.....G    Altcode:
  Time variations of the nitrate content in Greenland ice core for
  the last 400 years are analysed. An approximately 20-year cyclicity
  dominates the nitrate series during the Maunder minimum (1645-1715)
  due to similar variations of galactic cosmic ray intensity. During
  times of normal high solar activity level, the 4-6-year periodicity
  dominates the nitrate series. This is probably due to a superposition
  of fluxes of galactic and solar cosmic rays, and due to favourable
  conditions for the nitrate precipitation.

---------------------------------------------------------
Title: Odd and even cycles in cosmic rays and solar activity
Authors: Usoskin, I. G.; Mursula, K.; Kovaltsov, G. A.
2001ICRC....9.3791U    Altcode: 2001ICRC...27.3791U
  We present here a new method to define the evolution of cosmic ray
  and solar activity cycles using the time delayed component method in
  a 2D phase space. This method is free from the ambiguousness related
  to the exact timing of cosmic ray maxima and minima. We study the
  relationship between solar activity and cosmic ray intensity for the
  last four 11-year cycles. We confirm that the evolution of cosmic
  ray intensity is different for odd and even cycles and show that odd
  cosmic ray cycles are longer and have longer autocorrelation lengths
  than even cycles. The momentary time lag between cosmic ray intensity
  and sunspot activity is about one year for odd cycles and small or
  negative for even cycles. This reflects the difference in the cosmic
  ray modulation conditions for odd and even cycles and is probably
  associated with the influence of drift effects.

---------------------------------------------------------
Title: Cosmic ray intensity vs. solar indices: Is there a simple
    linear relation?
Authors: Mursula, K.; Usoskin, I. G.; Kovaltsov, G. A.
2001ICRC....9.3838M    Altcode: 2001ICRC...27.3838M
  It was recently suggested by Lockwood et al. (2000, 2001) that the
  cosmic ray intensity in the neutron monitor energy range is linearly
  related to the coronal source flux, and can be reconstructed for much
  earlier times using the estimated long term coronal flux. Here we show
  that a linear regression is oversimplified and leads to unphysical
  results on long time scales. In particular, the reconstructed cosmic
  ray intensity has a steep trend which is four times larger than the
  allowed upper bound. The reconstructed cosmic ray intensity exceeds
  the local interstellar cosmic ray flux around 1900. Also, the 11-year
  cycle minimum of the reconstructed cosmic ray intensity in early
  1900s is higher than the highest measured maximum in 1965. We argue
  that the unphysical results using a linear assumption are due to the
  oversimplified approach which does not account for complexity and
  significant nonlinearity of CR modulation in the heliosphere.

---------------------------------------------------------
Title: Was one sunspot cycle lost in late XVIII century?
Authors: Usoskin, I. G.; Mursula, K.; Kovaltsov, G. A.
2001A&A...370L..31U    Altcode:
  We suggest that one solar cycle was lost in the beginning of the Dalton
  minimum because of sparse and partly unreliable sunspot observations. So
  far this cycle was combined with the preceding activity to form the
  exceptionally long solar cycle #4 in 1784-1799, leading to an irregular
  phase evolution of sunspot activity (known as a phase catastrophe) and
  other problems. We reanalyze the available group sunspot numbers and
  suggest that solar cycle #4 was in fact a superposition of two cycles: a
  normal cycle in 1784-1793 ending at the start of the Dalton minimum and
  a new weak cycle in 1793-1800 which was the first full cycle within the
  Dalton minimum. Including the new cycle resolves the problems mentioned
  above and leads to a consistent view of sunspot activity around the
  Dalton minimum. Moreover, it will restore the Gnevyshev-Ohl rule of
  cycle pairing throughout the 400-year interval of sunspot observations.

---------------------------------------------------------
Title: Cosmic Ray Intensity vs. Solar Coronal Source Flux: Is There
    a Simple Relation?
Authors: Usoskin, I.; Mursula, K.
2001AGUSM..SH52A03U    Altcode:
  It was recently suggested by Lockwood [2001] that cosmic ray (CR) flux
  in the neutron monitor (NM) energy range is directly related to the
  solar coronal source flux, and can be reconstructed in the past. Here
  we show that this approach is oversimplified and can not be applied
  to CR reconstruction in the past. We reanalyse the reconstructed CR
  flux comparing it with the observed (Climax) NM flux during the last
  four solar cycles. While the details of CR time profile are reasonably
  reproduced by the Lockwood's regression model, the overall trend is
  questionable. The trend in the Climax NM count rate is about -0.02%
  per year while the Lockwood model series gives a much larger trend
  of about -0.13% per year. In the observed CR intensity, all maxima
  are roughly equally high while the depth of minima varies. However,
  in the model series, both maxima and minima are decreasing with time,
  leading to an extraneously large trend. This trend also implies a very
  high CR flux in early times. E.g., the model CR flux minimum in early
  1900s is higher than recent CR maxima, although solar activity maxima
  were much higher during that time than present cycle minima. We have
  recently estimated the NM response to unmodulated GCR in case of no
  heliosphere. This unmodulated Climax NM count rate would be only about
  16% higher than the actual count rate in the CR maximum year 1977. On
  the other hand, the model Climax NM count rate is 20% higher in the CR
  minimum year 1990 than in 1977, thus exceeding the unmodulated CR flux.

---------------------------------------------------------
Title: Regular and Random Components of Sunspot Activity During
Active Sun and Great Minima: Model Simulation
Authors: Usoskin, I.; Mursula, K.; Kovaltsov, G. A.
2001AGUSM..SH41A22U    Altcode:
  We model sunspot production during the two different modes of sunspot
  activity (the normal activity level and great minima), using the
  idea of a threshold-like mechanism [Ruzmaikin, 1997, 2000]. The model
  includes a dynamo field, a constant relic field of the Sun and a random
  field. This model describes the main features of sunspot activity both
  during normal activity times (dominant 11-year cycle and weak 22-year
  cycle) and during the Maunder minimum (sparse sunspot occurrence with
  22-year cycle) with the same model parameters, only varying the dynamo
  amplitude. The relic field must be about 3-10 % of the dynamo field
  in normal activity times.

---------------------------------------------------------
Title: Simulation of Sunspot Activity During Active Sun and Great
    Minima Using Regular, Random and Relic Fields
Authors: Usoskin, I. G.; Mursula, K.; Kovaltsov, G. A.
2001SoPh..199..187U    Altcode:
  Developing the idea of Ruzmaikin (1997, 1998), we have constructed a
  model of sunspot production using three components of solar magnetic
  field: the 22-year dynamo field, a weak constant relic field, and a
  random field. This model can reproduce the main features of sunspot
  activity throughout the 400-year period of direct solar observations,
  including two different sunspot activity modes, the present, normal
  sunspot activity and the Maunder minimum. The two sunspot activity
  modes could be modeled by only changing the level of the dynamo field
  while keeping the other two components constant. We discuss the role of
  the three components and how their relative importance changes between
  normal activity and great minimum times. We found that the relic field
  must be about 3-10% of the dynamo field in normal activity times. Also,
  we find that the dynamo field during the Maunder minimum was small
  but non-zero, being suppressed typically by an order of magnitude with
  respect to its value during normal activity times.

---------------------------------------------------------
Title: Persistent 22-year cycle in sunspot activity: Evidence for
    a relic solar magnetic field
Authors: Mursula, K.; Usoskin, I. G.; Kovaltsov, G. A.
2001SoPh..198...51M    Altcode:
  We use the recently presented group sunspot number series to show that
  a persistent 22-year cyclicity exists in sunspot activity throughout
  the entire period of about 400 years of direct sunspot observations. The
  amplitude of this cyclicity is about 10% of the present sunspot activity
  level. A 22-year cyclicity in sunspot activity is naturally produced
  by the 22-year magnetic polarity cycle in the presence of a relic
  dipole magnetic field. Accordingly, a persistent 22-year cyclicity in
  sunspot activity gives an evidence for the existence of such a relic
  magnetic field in the Sun. The stable phase and the roughly constant
  amplitude of this cyclicity during times of very different sunspot
  activity level strongly support this interpretation.

---------------------------------------------------------
Title: Dependence of cosmic rays on solar activity for odd and even
    solar cycles
Authors: Usoskin, I. G.; Mursula, K.; Kananen, H.; Kovaltsov, G. A.
2001AdSpR..27..571U    Altcode:
  We study the relationship between solar activity and cosmic ray
  intensity for the last four full cycles, using the time delayed
  component method (Usoskin et al., 1998) in a 2 D phase space. We
  present a new method to define the cosmic ray cycle which is free from
  ambiguousness related to the exact timing of cosmic ray maxima and
  minima. Using this definition, we confirm that the evolution of cosmic
  ray intensity is different for odd and even cycles and we show that odd
  cosmic ray cycles are longer and have longer autocorrelation interval
  lengths than even cycles. The momentary time lag between cosmic ray
  intensity and sunspot activity is about one year for odd cycles and
  small or negative for even cycles. This reflects the difference in
  the cosmic ray modulation conditions for odd and even cycles and is
  probably associated with the influence of drift effects.

---------------------------------------------------------
Title: OULU Neutron Monitor Cosmic Ray Data, January 2000 -
    December 2000
Authors: Usoskin, Ilya; Kultima, Johannes
2001STIN...0253711U    Altcode:
  This report presents data on cosmic ray intensities recorded by the
  Oulu Cosmic Ray station (Oulu NM) during the year 2000. The data
  include pressure corrected hourly count rate of the Oulu NM. The data
  are presented in the form of digital tables as well as plots, for each
  month separately.

---------------------------------------------------------
Title: Sensitivity of a neutron monitor to galactic cosmic rays
Authors: Usoskin, I. G.; Bobik, P.; Gladysheva, O. G.; Kananen, H.;
   Kovaltsov, G. A.; Kudela, K.
2001AdSpR..27..565U    Altcode:
  We studied the sensitivity of a neutron monitor to Galactic cosmic
  rays depending on energy of cosmic ray particles in the interstellar
  medium. This is important for studying of the interstellar spectrum
  of cosmic rays and details of solar modulation by means of the
  world neutron monitor network. We calculated the expected response
  of a standard sea-level neutron monitor vs. energy of cosmic ray
  particles. First, we studied modulation of a monoenergetic flux
  of cosmic rays. Then the specific atmospheric yield function of a
  neutron monitor was applied to the calculated flux of cosmic rays at
  the Earth's orbit. The obtained response function, being convoluted
  with the model interstellar spectrum of cosmic rays, gives a maximum
  of neutron monitor sensitivity at around several GV of rigidity of
  cosmic ray particles. We performed calculations for weak (φ = 350
  MV) and medium (φ = 750 MV) modulation strength. A normalisation of
  neutron monitor count rate is suggested which can give an experimental
  measure of the overall solar modulation of cosmic rays.

---------------------------------------------------------
Title: Cyclic behaviour of sunspot activity during the Maunder minimum
Authors: Usoskin, I. G.; Mursula, K.; Kovaltsov, G. A.
2000A&A...354L..33U    Altcode:
  We study the behaviour of sunspot activity in 1610-1750, i.e. just
  prior to, during and slightly after the Maunder minimum, using the
  new series of group sunspot numbers (\cite{hoyt98}). We apply the
  delayed component technique and show that, while the transition
  from the normal cyclic evolution to the minimum was very abrupt,
  the recovery from the minimum was gradual, proceeding through a tiny
  but very regular cycle in 1700-1712 and a transition period with a
  phase catastrophe in 1712-1720. Exploiting the good coverage of the
  Maunder minimum by daily solar observations, we show that the sunspot
  ocurrence is concentrated, with a high statistical significance, to
  two intervals around 1658 and 1680. Together with the last sunspot
  maximum before the Maunder minimum in 1639/1640, and the maximum in
  1705, this implies a significant, approximately 22-year periodicity
  in sunspot activity during the Maunder minimum.

---------------------------------------------------------
Title: Persistent 22-year Cycle in Sunspot Activity: Evidence for
    a Relic Solar Magnetic Field
Authors: Mursula, K.; Usoskin, I. G.; Kovaltsov, G. A.
2000ESASP.463..387M    Altcode: 2000sctc.proc..387M
  No abstract at ADS

---------------------------------------------------------
Title: Regular and Random Components of Sunspot Activity during
Active Sun and Great Minima: Model Simulation
Authors: Usoskin, I. G.; Mursula, K.; Kovaltsov, G. A.
2000ESASP.463..447U    Altcode: 2000sctc.proc..447U
  No abstract at ADS

---------------------------------------------------------
Title: A 22-year cycle in sunspot activity
Authors: Usoskin, I. G.; Mursula, K.; Kovaltsov, G. A.
2000IAUJD...7E..28U    Altcode:
  Recently, using the new group sunspot number series introduced by Hoyt
  and Schatten, we have shown that the weak sunspot activity during
  the Maunder minimum is modulated by a 22-year periodicity. Here we
  demonstrate that, after subtracting the long-term trend due to the
  Gleissberg cycle and after averaging the 11-year cyclicity, the group
  sunspot series depicts a 22-year cycle with an amplitude of about 10%
  of the current sunspot activity level. The well known Gnevyshev-Ohl
  rule is a reflection of such a persistent 22-year periodicity. We
  discuss the origin of the 22-year cycle in sunspot activity in terms
  of a weak relic solar magnetic field.

---------------------------------------------------------
Title: Regular and random components of sunspot activity: model
    simulations
Authors: Usoskin, I. G.; Mursula, K.; Kovaltsov, G. A.
2000IAUJD...7E..27U    Altcode:
  In this contribution we study the question of the relationships between
  regularities and chaos in the dynamo mechanism producing sunspot
  activity. Following the idea of the threshold-like mechanism of sunspot
  production, we considered a simple phenomenological model consisiting
  of regular and random-driven components. The model describes pretty well
  the main features of the sunspot activity for both normal activity times
  (11-year, 22-year cycles, variations of cycle length and amplitude)
  and for the Maunder minimum (seemingly sporadic sunspot occurrence).

---------------------------------------------------------
Title: Protons in near earth orbit
Authors: Alcaraz, J.; Alvisi, D.; Alpat, B.; Ambrosi, G.; Anderhub,
   H.; Ao, L.; Arefiev, A.; Azzarello, P.; Babucci, E.; Baldini, L.;
   Basile, M.; Barancourt, D.; Barao, F.; Barbier, G.; Barreira, G.;
   Battiston, R.; Becker, R.; Becker, U.; Bellagamba, L.; Béné,
   P.; Berdugo, J.; Berges, P.; Bertucci, B.; Biland, A.; Bizzaglia,
   S.; Blasko, S.; Boella, G.; Boschini, M.; Bourquin, M.; Bruni, G.;
   Buenerd, M.; Burger, J. D.; Burger, W. J.; Cai, X. D.; Cavalletti,
   R.; Camps, C.; Cannarsa, P.; Capell, M.; Casadei, D.; Casaus, J.;
   Castellini, G.; Chang, Y. H.; Chen, H. F.; Chen, H. S.; Chen, Z. G.;
   Chernoplekov, N. A.; Chiarini, A.; Chiueh, T. H.; Chuang, Y. L.;
   Cindolo, F.; Commichau, V.; Contin, A.; Cotta-Ramusino, A.; Crespo,
   P.; Cristinziani, M.; da Cunha, J. P.; Dai, T. S.; Deus, J. D.; Dinu,
   N.; Djambazov, L.; D'Antone, I.; Dong, Z. R.; Emonet, P.; Engelberg,
   J.; Eppling, F. J.; Eronen, T.; Esposito, G.; Extermann, P.; Favier,
   J.; Feng, C. C.; Fiandrini, E.; Finelli, F.; Fisher, P. H.; Flaminio,
   R.; Fluegge, G.; Fouque, N.; Galaktionov, Y.; Gervasi, M.; Giusti,
   P.; Grandi, D.; Gu, W. Q.; Hangarter, K.; Hasan, A.; Hermel, V.;
   Hofer, H.; Huang, M. A.; Hungerford, W.; Ionica, M.; Ionica, R.;
   Jongmanns, M.; Karlamaa, K.; Karpinski, W.; Kenney, G.; Kenny, J.;
   Kim, W.; Klimentov, A.; Kossakowski, R.; Koutsenko, V.; Laborie, G.;
   Laitinen, T.; Lamanna, G.; Laurenti, G.; Lebedev, A.; Lee, S. C.; Levi,
   G.; Levtchenko, P.; Liu, C. L.; Liu, H. T.; Lolli, M.; Lopes, I.; Lu,
   G.; Lu, Y. S.; Lübelsmeyer, K.; Luckey, D.; Lustermann, W.; Maña,
   C.; Margotti, A.; Massera, F.; Mayet, F.; McNeil, R. R.; Meillon, B.;
   Menichelli, M.; Mezzanotte, F.; Mezzenga, R.; Mihul, A.; Molinari, G.;
   Mourao, A.; Mujunen, A.; Palmonari, F.; Pancaldi, G.; Papi, A.; Park,
   I. H.; Pauluzzi, M.; Pauss, F.; Perrin, E.; Pesci, A.; Pevsner, A.;
   Pilastrini, R.; Pimenta, M.; Plyaskin, V.; Pojidaev, V.; Postema, H.;
   Postolache, V.; Prati, E.; Produit, N.; Rancoita, P. G.; Rapin, D.;
   Raupach, F.; Recupero, S.; Ren, D.; Ren, Z.; Ribordy, M.; Richeux,
   J. P.; Riihonen, E.; Ritakari, J.; Roeser, U.; Roissin, C.; Sagdeev,
   R.; Santos, D.; Sartorelli, G.; Schultz von Dratzig, A.; Schwering, G.;
   Seo, E. S.; Shoutko, V.; Shoumilov, E.; Siedling, R.; Son, D.; Song,
   T.; Steuer, M.; Sun, G. S.; Suter, H.; Tang, X. W.; Ting, S. C. C.;
   Ting, S. M.; Tornikoski, M.; Torromeo, G.; Torsti, J.; Trümper,
   J.; Ulbricht, J.; Urpo, S.; Usoskin, I.; Valtonen, E.; Vandenhirtz,
   J.; Velcea, F.; Velikhov, E.; Verlaat, B.; Vetlitsky, I.; Vezzu, F.;
   Vialle, J. P.; Viertel, G.; Vité, D.; Von Gunten, H.; Waldmeier Wicki,
   S.; Wallraff, W.; Wang, B. C.; Wang, J. Z.; Wang, Y. H.; Wiik, K.;
   Williams, C.; Wu, S. X.; Xia, P. C.; Yan, J. L.; Yan, L. G.; Yang,
   C. G.; Yang, M.; Ye, S. W.; Yeh, P.; Xu, Z. Z.; Zhang, H. Y.; Zhang,
   Z. P.; Zhao, D. X.; Zhu, G. Y.; Zhu, W. Z.; Zhuang, H. L.; Zichichi, A.
2000PhLB..472..215A    Altcode: 2000hep.ex....2049A; 2000hep.ex....2049C
  The proton spectrum in the kinetic energy range 0.1 to 200 GeV
  was measured by the Alpha Magnetic Spectrometer (AMS) during
  space shuttle flight STS-91 at an altitude of 380km. Above the
  geomagnetic cutoff the observed spectrum is parameterized by a power
  law. Below the geomagnetic cutoff a substantial second spectrum
  was observed concentrated at equatorial latitudes with a flux
  /~70m<SUP>-2</SUP>s<SUP>-1</SUP>sr<SUP>-1</SUP>. Most of these second
  spectrum protons follow a complicated trajectory and originate from
  a restricted geographic region.

---------------------------------------------------------
Title: Connections between neutron monitor count rate and solar
    modulation strength
Authors: Usoskin, I. G.; Gladysheva, O. G.; Bobik, P.; Kudela, K.;
   Kananen, H.
1999CzJPh..49.1743U    Altcode:
  We suggest a new approach to the normalisation of neutron monitor
  response to galactic cosmic rays. The reference normalisation count
  rate is the neutron monitor response to the model unmodulated flux of
  galactic cosmic rays. A comparison of the actually recorded neutron
  monitor count rate with the calculated normalisation count rate can
  provide one with an observationally obtained true-of-date integral
  measure of the current level of solar modulation of galactic cosmic
  rays.

---------------------------------------------------------
Title: Search for antihelium in cosmic rays.
Authors: Alcaraz, J.; Alvisi, D.; Alpat, B.; Ambrosi, G.; Anderhub, H.;
   Ao, L.; Arefiev, A.; Azzarello, P.; Babucci, E.; Baldini, L.; Basile,
   M.; Barancourt, D.; Barao, F.; Barbier, G.; Barreira, G.; Battiston,
   R.; Becker, R.; Becker, U.; Bellagamba, L.; Bene, P.; Berdugo, J.;
   Berges, P.; Bertucci, B.; Biland, A.; Bizzaglia, S.; Blasko, S.;
   Boella, G.; Bourquin, M.; Bruni, G.; Buenerd, M.; Burger, J. D.;
   Burger, W. J.; Cai, X. D.; Cavalletti, R.; Camps, C.; Cannarsa, P.;
   Capell, M.; Casadei, D.; Casaus, J.; Catellini, G.; Chang, Y. H.; Chen,
   H. S.; Chen, Z. G.; Chernoplekov, N. A.; Chiarini, A.; Chiueh, T. H.;
   Chuang, Y. L.; Cindolo, F.; Commichau, V.; Contin, A.; Cotta-Ramusino,
   A.; Crespo, P.; Cristinziani, M.; da Cunha, J. P.; Dai, T. S.; Deus,
   J. D.; Ding, L. K.; Dinu, N.; Djambazov, L.; D'Antone, I.; Dong, Z. R.;
   Emonet, P.; Eppling, F. J.; Eronen, T.; Esposito, G.; Extermann, P.;
   Favier, J.; Feng, C. C.; Fiandrini, E.; Finelli, F.; Fisher, P. H.;
   Flaminio, R.; Fluegge, G.; Fouque, N.; Galaktionov, Yu.; Gervasi, M.;
   Giusti, P.; Gu, W. Q.; Guzik, T. G.; Hangarter, K.; Hasan, A.; Hermel,
   V.; Hofer, H.; Huang, M. A.; Hungerford, W.; Ionica, M.; Ionica,
   R.; Isbert, J.; Jongmanns, M.; Karpinski, W.; Kenney, G.; Kenny, J.;
   Kim, W.; Klimentov, A.; Krieger, J.; Kossakowski, R.; Koutsenko, V.;
   Laborie, G.; Laitinen, T.; Lamanna, G.; Laurenti, G.; Lebedev, A.;
   Lee, S. C.; Levi, G.; Levtchenko, P.; Li, T. P.; Liu, H. T.; Lolli,
   M.; Lopes, I.; Lu, G.; Lu, Y. S.; Lubelsmeyer, K.; Luckey, D.;
   Lustermann, W.; Maehlum, G.; Mana, C.; Margotti, A.; Massera, F.;
   Mayet, F.; McNeil, R. R.; Meillon, B.; Menichelli, M.; Mezzanotte,
   F.; Mezzenga, R.; Mihul, A.; Molinari, G.; Mourao, A.; Mujunen,
   A.; Palmonari, F.; Pancaldi, G.; Papi, A.; Park, I. H.; Pauluzzi,
   M.; Pauss, F.; Perrin, E.; Pesci, A.; Pevsner, A.; Pilastrini, R.;
   Pimenta, M.; Plyaskin, V.; Pojidaev, V.; Postema, H.; Prati, E.;
   Produit, N.; Rancoita, P. G.; Rapin, D.; Raupach, F.; Recupero, S.;
   Ren, D.; Ren, Z.; Ribordy, M.; Richeux, J. P.; Riihonen, E.; Ritakari,
   J.; Roeser, U.; Roissin, C.; Sagdeev, R.; Santos, D.; Sartorelli, G.;
   Schultz von Dratzig, A.; Schwering, G.; Shoutko, V.; Shoumilov, E.;
   Siedling, R.; Son, D.; Song, T.; Steuer, M.; Sun, G. S.; Suter, H.;
   Tang, X. W.; Ting, S. C. C.; Ting, S. M.; Tenbusch, F.; Torromeo,
   G.; Torsti, J.; Trumper, J.; Ulbricht, J.; Urpo, S.; Usoskin, I.;
   Valtonen, E.; Vandenhirtz, J.; Velikhov, E.; Verlaat, B.; Vetlitsky,
   I.; Vezzu, F.; Vialle, J. P.; Viertel, G.; Vite, D.; von Gunten, H.;
   Waldmeier Wicki, S.; Wallraff, W.; Wang, B. C.; Wang, J. Z.; Wang,
   Y. H.; Wefel, J. P.; Werner, E. A.; Williams, C.; Wu, S. X.; Xia,
   P. C.; Yan, J. L.; Yan, L. G.; Yang, C. G.; Yang, M.; Yeh, P.; Zhang,
   H. Y.; Zhao, D. X.; Zhu, G. Y.; Zhu, W. Z.; Zhuang, H. L.; Zichichi, A.
1999PhLB..461..387A    Altcode: 2000hep.ex....2048C; 2000hep.ex....2048A
  The alpha magnetic spectrometer (AMS) was flown on the space shuttle
  Discovery during flight STS-91 in a 51.7° orbit at altitudes between
  320 and 390 km. A total of 2.86×10<SUP>6</SUP> helium nuclei were
  observed in the rigidity range 1 to 140 GV. No antihelium nuclei were
  detected at any rigidity. An upper limit on the flux ratio of antihelium
  to helium of &lt;1.1×10<SUP>-6</SUP> is obtained.

---------------------------------------------------------
Title: Monte-Carlo approach to Galactic Cosmic Ray propagation in
    the Heliosphere
Authors: Gervasi, M.; Rancoita, P. G.; Usoskin, I. G.; Kovaltsov, G. A.
1999NuPhS..78...26G    Altcode:
  In the present paper we consider a possibility of using stochastic
  simulation (Monte-Carlo) technique approach to the study of Galactic
  Cosmic Ray propagation in the Heliosphere. We developed a technique for
  calculation of the cosmic ray propagation in a spherically symmetric
  steady state approximation of the Heliosphere. A comparison of the
  calculation results with those obtained by other methods as well as
  with an analytical approximation shows a good agreement. Besides,
  in the frameworks of the approximation used, we calculated the solar
  modulation of monoenergetic fluxes of Galactic Cosmic Rays entering the
  Heliosphere, in the particle's energy range 0.1 - 15 GeV. We studied the
  details of the modulation in their dependence of the initial particle's
  energy. In particular, a linear scaling of particle's energy losses
  vs. diffusion time is shown.

---------------------------------------------------------
Title: Secondary production antiproton flux: A comparison between
    interstellar models and expected flux at the Earth - presented by
    M. A. C. Potenza
Authors: Boella, G.; Gervasi, M.; Potenza, M. A. C.; Rancoita, P. G.;
   Usoskin, I.
1999foap.conf..379B    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: Time Evolution of Solar Activity and Cosmic Ray Intensity
    during the Maunder Minimum
Authors: Usoskin, I. G.
1999ICRC....7..127U    Altcode: 1999ICRC...26g.127U
  No abstract at ADS

---------------------------------------------------------
Title: Modulated antiproton fluxes for interstellar production models
Authors: Boella, G.; Gervasi, M.; Potenza, M. A. C.; Rancoita, P. G.;
   Usoskin, I.
1998APh.....9..261B    Altcode:
  Expected differential fluxes of antiprotons at the Earth's orbit are
  calculated for minimum and medium strength of the solar modulation. We
  used an analytical solution in the force-field approximation. Local
  interstellar spectra are taken as predictions of different theoretical
  models of secondary production of antiprotons in the Galaxy. All the
  antiproton- as well as proton-fluxes are modulated in the same way
  for the purpose of a direct comparison in order to avoid additional
  uncertainties. It is shown that, in order to compare experimental data
  with the existing models predictions, next generation experiments should
  be able to measure fluxes of particles with energies above 100 MeV.

---------------------------------------------------------
Title: Correlative study of solar activity and cosmic ray intensity
Authors: Usoskin, I. G.; Kananen, H.; Mursula, K.; Tanskanen, P.;
   Kovaltsov, G. A.
1998JGR...103.9567U    Altcode:
  We perform a correlative study of solar activity (sunspot numbers)
  and cosmic ray intensity (neutron monitor count rates) for the last
  four solar cycles. Analysis of the running cross correlation between
  the two series shows that the behavior of cosmic ray modulation is
  similar, in general, for particles with different energy. However,
  a strong rigidity dependence as well as an unusual behavior of the
  cross correlation function is found for the descending phase of cycle
  20. We study the evolution of cosmic ray and solar activity cycles
  in a three-dimensional phase space by means of the delayed component
  method. While all solar activity cycles and most cosmic ray cycles
  are planar, cosmic ray cycle 20 is significantly three-dimensional. A
  concept of the momentary phase of a cycle is introduced, and the phase
  evolution of cosmic ray and solar activity cycles is studied. We also
  discuss the heliospheric conditions responsible for the unusual behavior
  of cosmic ray modulation in the descending phase of cycle 20.

---------------------------------------------------------
Title: Effect of the Solar Modulation at Minimum Activity on Expected
    Ratio of Antiproton to Proton Flux
Authors: Boella, G.; Gervasi, M.; Potenza, M. A. C.; Rancoita, P. G.;
   Usoskin, I.
1998cosm.work..273B    Altcode:
  We evaluated differential fluxes of antiprotons at the Earth's
  orbit. Modulated antiproton spectra are calculated for minimum
  modulation strength. Local interstellar spectra are taken as predictions
  of different theoretical models of secondary production of antiprotons
  in the Galaxy. All the antiproton- as well as proton-fluxes are
  modulated in the same way for the purpose of a direct comparison in
  order to avoid additional uncertainties.

---------------------------------------------------------
Title: Period of Unusual Modulation of Cosmic Ray Intensity: The
    Declining Phase of Cycle 20
Authors: Usoskin, I. G.; Kananen, H.; Mursula, K.; Tanskanen, P.;
   Kovaltsov, G. A.
1997ESASP.415..491U    Altcode: 1997cpsh.conf..491U
  No abstract at ADS

---------------------------------------------------------
Title: On the Claimed 5.5-year Periodicity in Solar Activity
Authors: Mursula, K.; Usoskin, I.; Zieger, B.
1997SoPh..176..201M    Altcode:
  Recently, Djurovic and Pâquet (1996) claimed to have found an
  oscillation with a period of about 5.5 years in several solar and
  solar-terrestrial parameters, in particular in solar activity as
  indicated by sunspot numbers. Since the temporal evolution of the solar
  activity and solar-terrestrial environment is of great interest in many
  fields, we have examined their claim in detail. We show here that their
  conclusion is based on an artefact due a questionable method applied,
  and due to the asymmetric form of the solar cycle. Accordingly, there
  is no reasonable evidence for the existence of a fundamental 5.5-year
  periodicity in solar activity.

---------------------------------------------------------
Title: Impact of Magnetic Environment on the Generation of High-Energy
    Neutrons at the Sun
Authors: Kocharov, L. G.; Torsti, J.; Tang, F.; Zirin, H.; Kovaltsov,
   G. A.; Usoskin, I. G.
1997SoPh..172..271K    Altcode: 1997ESPM....8..271K
  This paper demonstrates the important interplanetary manifestation
  of strongly tilted magnetic fields at the flare site. We start with
  analysis of Big Bear Solar Observatory (BBSO) observations of magnetic
  structures at sites of two flares responsible for &gt;100 MeV neutron
  events. Based on these observations, a model of neutron production is
  considered. This model takes into account the observed large tilt of
  magnetic field lines at footpoints of flare magnetic loops. Results
  of the new calculations are compared with both previous calculations
  and observations. The tilt of magnetic field lines at the flare site
  is proved to be the most important parameter limiting anisotropy of
  high-energy secondary emission in solar flares.

---------------------------------------------------------
Title: The World Neutron Monitor Network as a tool for the study of
    solar neutrons
Authors: Usoskin, I. G.; Kovaltsov, G. A.; Kananen, H.; Tanskanen, P.
1997AnGeo..15..375U    Altcode: 1997AnG....15..375U
  The use of the World Neutron Monitor Network to detect high-energy
  solar neutrons is discussed in detail. It is shown that the existing
  network can be used for the routine detection of intense sporadic
  solar-neutron events whenever they occur. A technique is suggested
  involving the weighted summation of responses of separate monitors to
  solar neutrons. It is demonstrated that the use of this method improves
  the significance of solar-neutron event detection. Different results of
  the simulation of the neutron-monitor sensitivity to solar neutrons
  have been tested with respect to their application for practical
  use. It is shown that the total number of neutrons with energy above
  300 MeV injected from the Sun during a solar flare can be estimated
  directly from the time-integrated neutron-monitor response to solar
  neutrons without any model assumptions. The estimation technique has
  been developed

---------------------------------------------------------
Title: Phase Evolution of Solar Activity and Cosmic-Ray Variation
    Cycles
Authors: Usoskin, I. G.; Kovaltsov, G. A.; Kananen, H.; Mursula, K.;
   Tanskanen, P. J.
1997SoPh..170..447U    Altcode:
  Cycles of phase evolution of solar activity and cosmic-ray variations
  are reconstructed by means of the delay component method, which allows
  us to study the temporal behaviour of time lag between solar activity
  and cosmic-ray cycle phases. It is shown that the period of the late
  20th cycle was very unusual. We have found a delay in the phase of the
  solar activity cycle with respect to that of cosmic rays and discuss
  the heliospheric conditions responsible for this delay.

---------------------------------------------------------
Title: Impact of Magnetic Environment on the Generation of High-Energy
    Neutrons and Gamma-Rays During Solar Flares
Authors: Kocharov, L. G.; Kovaltsov, G.; Torsti, J.; Usoskin, I.
1997ICRC....1...65K    Altcode: 1997ICRC...25a..65K
  No abstract at ADS

---------------------------------------------------------
Title: Phases of Charged Particles Acceleration during Powerful
    Solar Gamma-Flares Detected by the Gamma - 1
Authors: Galper, A. M.; Luchkov, B. I.; Ozerov, Yu. V.; Khodarovich,
   A. M.; Rinchinov, S. B.; Kovaltsov, G. A.; Usoskin, I. G.
1997ICRC....1..169G    Altcode: 1997ICRC...25a.169G
  No abstract at ADS

---------------------------------------------------------
Title: Period of Unusual Cosmic Ray Modulation in Late 20th Cycle:
    Correlative Study of Cosmic Ray variations vs. Solar Activity
Authors: Usoskin, I. G.; Kovaltsov, G. A.; Kananen, H.; Mursula, K.;
   Tanskanen, P.
1997ICRC....2..201U    Altcode: 1997ICRC...25b.201U
  No abstract at ADS

---------------------------------------------------------
Title: Direct Deduction of the Number of Neutrons Injected from the
    Sun on the Basis of Neutron Monitor Response
Authors: Kananen, H.; Kovaltsov, G. A.; Tanskanen, P.; Usoskin, I. G.
1997ICRC....1...49K    Altcode: 1997ICRC...25a..49K
  No abstract at ADS

---------------------------------------------------------
Title: A Joint Analysis of High-Energy Neutrons and Neutron-Decay
    Protons from a Flare
Authors: Kocharov, L. G.; Torsti, J.; Vainio, R.; Kovaltsov, G. A.;
   Usoskin, I. G.
1996SoPh..169..181K    Altcode:
  A joint analysis of neutron monitor and GOES data is performed to
  study the production of high-energy neutrons at the Sun. The main
  objects of the research are the spectrum of &gt;50 MeV neutrons and
  a possible spectrum of primary (interacting) protons which produced
  those neutrons during the major 1990 May 24 solar flare. Different
  possible scenarios of the neutron production are presented. The high
  magnitude of the 1990 May 24 neutron event provided an opportunity to
  detect neutron decay protons of higher energies than ever before. We
  compare predictions of the proposed models of neutron production with
  the observations of protons on board GOES 6 and 7. It is shown that the
  `precursor' in high-energy GOES channels observed during 20:55-21:09 UT
  can be naturally explained as originating from decay of neutrons in the
  interplanetary medium. The ratio of counting rates observed in different
  GOES channels can ensure the selection of the model parameters.

---------------------------------------------------------
Title: The 1990 May 24 solar flare and cosmic ray event
Authors: Kocharov, Leon; Kovaltsov, Gennadi; Torsti, Jarmo; Usoskin,
   Ilya; Zirin, Harold; Anttila, Antti; Vainio, Rami
1996AIPC..374..246K    Altcode: 1996hesp.conf..246K
  We have analyzed data on solar protons, neutrons, electrons, gamma-ray,
  optical and microwave emissions for the 1990 May 24 solar flare. Taking
  into account high energy neutron and gamma-ray observations, we have
  suggested two neutron injections occurred during the flare. These two
  injections are called f- (first) and s- (second). Two components of
  interacting protons correspondingly existed to produce these neutrons
  at the Sun. The flare gave also a rise to solar cosmic ray event, which
  was detected by the neutron monitor network and GOES satellites. Two
  components of protons were observed in the interplanetary medium (p-
  (prompt) and d- (delayed) components). A possible spectrum of the
  s-component of interacting protons coincided with injection spectrum
  of p-component of interplanetary protons. For this reason, s- and p-
  components of protons may be considered as different portions of a
  single population of accelerated particles in the solar corona. The
  net result is that three proton components (f-, p/s-, and d-) were
  accelerated during flare process developing from the Sun to the
  interplanetary medium.

---------------------------------------------------------
Title: Temporal and spectral characteristics of solar gamma flares
    observed in the Gamma-1 experiment.
Authors: Galper, A. M.; Zverev, V. G.; Luchkov, B. I.; Ozerov, Yu. V.;
   Khodarovitch, A. M.; Kovaltsov, G. A.; Usoskin, I. G.
1996JMoPS...6..399G    Altcode:
  The results of a comparative analysis of the high-energy (Eγ &gt;
  30 MeV) powerful solar gamma flares of 26.03.91 and 15.06.91 are
  presented. These flares are estimated to have an active phase with
  an exponential intensity decay lasting up to 10 minutes (and possibly
  more for 15.06.91) and repeated multiple acts of electron and proton
  acceleration, followed by a longer phase without such repeated multiple
  acts of acceleration. Limits on parameters for particle acceleration and
  propagation in the solar atmosphere are estimated from the observational
  data for these flares.

---------------------------------------------------------
Title: Erratum: The 1991 March 22 Flare: Possible Anistrophy of
    High-Energy Neutral Emission
Authors: Kocharov, L. G.; Lee, Jeongwoo W.; Wang, H.; Zirin, H.;
   Kovaltsov, G. A.; Usoskin, I. G.
1995SoPh..161..407K    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: Neutron Monitor Data on the 15 June 1991 Flare: Neutrons as
    a Test for Proton Acceleration Scenario
Authors: Kovaltsov, G. A.; Usoskin, I. G.; Kocharov, L. G.; Kananen,
   H.; Tanskanen, P. J.
1995SoPh..158..395K    Altcode:
  Response of Alma-Ata neutron monitor for solar neutrons from the
  15 June 1991 was studied. We considered this response as a test for
  various scenarios of proton acceleration during the flare. The analysis
  of neutron monitor is an evidence in favour of the assumption of two
  acts of proton acceleration at impulsive and post-impulsive phases of
  the flare.

---------------------------------------------------------
Title: The 1991 March 22 Flare: Possible Anisotropy of High-Energy
    Neutral Emission
Authors: Kocharov, L. G.; Lee, Jeongwoo W.; Wang, H.; Zirin, H.;
   Kovaltsov, G. A.; Usoskin, I. G.
1995SoPh..158...95K    Altcode:
  We made a parameter fit to the Haleakala neutron monitor counting
  rate during the 1991 March 22 solar flare (Pyle and Simpson, 1991)
  using the time profiles of γ-rays at 0.42-80 MeV obtained with
  the GRANAT satellite (Vilmeret al., 1994) and the microwave data
  from Owens Valley Radio Observatory. We use a two-component neutron
  injection function to find that either an impulsive injection or the
  `impulsive-plus-prolonged' neutron injection is possible. In both
  cases, the number of &gt; 300 MeV neutrons emitted towards the Earth
  is estimated as ≈ 2 × 10<SUP>27</SUP> sr<SUP>−1</SUP>, which is
  less than that of the 1990 May 24 flare by an order of magnitude.

---------------------------------------------------------
Title: Correlative Investigations of the 1990 May 24 Solar Flare
Authors: Kocharov, L. G.; Kovaltsov, G. A.; Torsti, J.; Usoskin,
   I. G.; Zirin, H.
1995ICRC....4..159K    Altcode: 1995ICRC...24d.159K
  No abstract at ADS

---------------------------------------------------------
Title: High Energy Neutrons from the June 15, 1991 Solar Flare as
    Detected by the Neutron Monitor
Authors: Usoskin, I. G.; Kovaltsov, G. A.; Kocharov, L. G.; Kananen,
   H.; Tanskanen, P.
1995ICRC....4..151U    Altcode: 1995ICRC...24d.151U
  No abstract at ADS

---------------------------------------------------------
Title: The June 3, 1982 Solar Flare as a Test for Neutron Monitor
    Sensitivity for Solar Neutrons
Authors: Kananen, H.; Kocharov, L. G.; Kovaltsov, G. A.; Tanskanen,
   P.; Usoskin, I. G.
1995ICRC....4..147K    Altcode: 1995ICRC...24d.147K
  No abstract at ADS

---------------------------------------------------------
Title: Two Injections of High Energy Neutrons during the May 24,
    1990 Solar Flare
Authors: Kovaltsov, G. A.; Kocharov, L. G.; Usoskin, I. G.; Kananen,
   H.; Taskanen, P.
1995ICRC....4..155K    Altcode: 1995ICRC...24d.155K
  No abstract at ADS

---------------------------------------------------------
Title: High-energy gamma-ray signature of proton acceleration during
    1991 June 15 solar flare
Authors: Kocharov, G. E.; Chuikin, E. I.; Kovaltsov, G. A.; Usoskin,
   I. G.; Kocharov, L. G.
1994AIPC..294...45K    Altcode: 1994hesp.conf...45K
  We consider the γ-ray and radio observations for the 06.15.1991
  flare. It is shown that these data give the first possibility for
  precise determination of proton spectrum in 10 MeV-10 GeV energy range
  in flare site. The power law γ-ray spectrum up to 1 GeV indicates
  that the maximum energy in power law primary proton spectrum is &gt;=10
  GeV. The time profiles of cm-radioemission and of γ-ray in 0.8-10 MeV
  energy band and above 50 MeV coincide. A continuous and simultaneous
  acceleration of protons and relativistic electrons at the gradual
  phase of the flare gives a natural explanation of the data.

---------------------------------------------------------
Title: Neutron and electromagnetic emissions during the 1990 May 24
    solar flare
Authors: Kocharov, L. G.; Lee, Jeongwoo W.; Zirin, H.; Kovaltsov,
   G. A.; Usoskin, I. G.; Pyle, K. R.; Shea, M. A.; Smart, D. F.
1994SoPh..155..149K    Altcode:
  In this paper, we are primarily concerned with the solar neutron
  emission during the 1990 May 24 flare, utilizing the counting rate
  of the Climax neutron monitor and the time profiles of hard X-rays
  and γ-rays obtained with the GRANAT satellite (Pelaezet al., 1992;
  Talonet al., 1993; Terekhovet al., 1993). We compare the derived
  neutron injection function with macroscopic parameters of the flare
  region as obtained from theHα and microwave observations made at the
  Big Bear Solar Observatory and the Owens Valley Radio Observatory,
  respectively. Our results are summarized as follows: (1) to explain the
  neutron monitor counting rate and 57.5-110 MeV and 2.2 MeV γ-ray time
  profiles, we consider a two-component neutron injection function,Q(E,
  t), with the form Q(E,t) = N<SUB>f</SUB>exp[-E/E<SUB>f</SUB>
  -t/T<SUB>f</SUB>] + N<SUB>2</SUB> exp[-E/E<SUB>s</SUB> -
  t/T<SUB>s</SUB>], where N<SUB>f(s)</SUB>,E<SUB>f(s)</SUB>,
  andT<SUB>f(s)</SUB> denote number, energy, and decay time of the fast
  (slow) injection component, respectively. By comparing the calculated
  neutron counting rate with the observations from the Climax neutron
  monitor we derive the best-fit parameters asT<SUB>f</SUB> ≈ 20
  s,E<SUB>f</SUB> ≈ 310 MeV,T<SUB>s</SUB> ≈ 260 s,E<SUB>s</SUB>
  ≈ 80 MeV, andN<SUB>f</SUB>(E &gt; 100 MeV)/N<SUB>s</SUB>(E &gt;
  100 MeV) ≈ 0.2. (2) From the Hα observations, we find a relatively
  small loop of length ≈ 2 × 10<SUP>4</SUP> km, which may be regarded
  as the source for the fast-decaying component of γ-rays (57.5-110
  MeV) and for the fast component of neutron emission. From microwave
  visibility and the microwave total power spectrum we postulate the
  presence of a rather big loop (≈ 2 × 10<SUP>5</SUP> km), which we
  regard as being responsible for the slow-decaying component of the
  high-energy emission. We show how the neutron and γ-ray emission
  data can be explained in terms of the macroscopic parameters derived
  from the Hα and microwave observations. (3) The Hα observations
  also reveal the presence of a fast mode MHD shock (the Moreton wave)
  which precedes the microwave peak by 20-30 s and the peak of γ-ray
  intensity by 40-50 s. From this relative timing and the single-pulsed
  time profiles of both radiations, we can attribute the whole event
  as due to a prompt acceleration of both electrons and protons by the
  shock and subsequent deceleration of the trapped particles while they
  propagate inside the magnetic loops.

---------------------------------------------------------
Title: Generation of neutrons during the solar flare of May 24, 1990
Authors: Koval'Tsov, G. A.; Kocharov, G. E.; Kocharov, L. G.; Usoskin,
   I. G.
1994AstL...20..658K    Altcode: 1994PAZh...20..762K
  No abstract at ADS

---------------------------------------------------------
Title: Electromagnetic and corpuscular emission from the solar flare
of 1991 June 15: Continuous acceleraton of relativistic particles
Authors: Kocharov, L. G.; Kovaltsov, G. A.; Kocharov, G. E.; Chuikin,
   E. I.; Usoskin, I. G.; Shea, M. A.; Smart, D. F.; Melnikov, V. F.;
   Podstrigach, T. S.; Armstrong, T. P.; Zirin, H.
1994SoPh..150..267K    Altcode:
  Data on X-,γ-ray, optical and radio emission from the 1991 June
  15 solar flare are considered. We have calculated the spectrum of
  protons that producesγ-rays during the gradual phase of the flare. The
  primary proton spectrum can be described as a Bessel-function-type up
  to 0.8 GeV and a power law with the spectral index ≈3 from 0.8 up
  to 10 GeV or above. We have also analyzed data on energetic particles
  near the Earth. Their spectrum differed from that of primary protons
  producingγ-ray line emission. In the gradual phase of the flare
  additional pulses of energy release occurred and the time profiles of
  cm-radio emission andγ-rays in the 0.8-10 MeV energy band and above 50
  MeV coincided. A continuous and simultaneous stochastic acceleration
  of the protons and relativistic electrons at the gradual phase of the
  flare is considered as a natural explanation of the data.

---------------------------------------------------------
Title: Gamma-radiation from the solar flare of 15 June 1991 as
    evidence of long-term acceleration of protons up to 10 GeV
Authors: Koval'Tsov, G. A.; Kocharov, G. E.; Kocharov, L. G.;
   Mel'Nikov, V. F.; Podstrigach, T. S.; Usoskin, I. G.; Chujkin, E. I.
1993RoIzF..57..138K    Altcode:
  The power spectrum of gamma-radiation up to 2 GeV observed during the
  flare of 15 June 1991 indicates that the primary protons had a power
  spectrum extending at least to 10 GeV. Comparing the time profiles
  of centimeter-wave emission, gamma-radiation in nuclear lines in the
  0.8-8 MeV range, and high-energy gamma-radiation from pion decay,
  their coincidence is found, indicating the simultaneous long-term
  acceleration of particles after the impulsive phase of the solar flare.

---------------------------------------------------------
Title: Detection of solar neutrinos by the worldwide network of
    neutron monitors
Authors: Efimov, Yu. E.; Koval'Tsov, G. A.; Kocharov, G. E.; Kocharov,
   L. G.; Usoskin, I. G.
1993RoIzF..57..142E    Altcode:
  The possibility of detecting solar neutrinos by the worldwide network
  of neutron monitors is examined. The neutron-monitor response function
  to high-energy solar neutrinos is reexamined. It is shown that the
  probability of detecting high-energy solar neutrinos with the worldwide
  neutron-monitor network is higher than previously thought.

---------------------------------------------------------
Title: High Energy Gamma Rays from 1991 June 15 Solar Flare as
    Evidence of Proton Acceleration up to 10 GeV
Authors: Kocharov, G. E.; Chuikin, E. I.; Kocharov, L. G.; Kovaltsov,
   G. A.; Melnikov, V. F.; Podstrigach, T. S.; Usoskin, I. G.
1993ICRC....3..123K    Altcode: 1993ICRC...23c.123K
  No abstract at ADS

---------------------------------------------------------
Title: Solar Flare Neutrinos
Authors: Kocharov, G. E.; Kovaltsov, G. A.; Usoskin, I. G.
1991ICRC....3..752K    Altcode: 1991ICRC...22c.752K
  No abstract at ADS

---------------------------------------------------------
Title: Solar flare neutrinos.
Authors: Kocharov, G. E.; Koval'Tsov, G. A.; Usoskin, I. G.
1991NCimC..14..417K    Altcode:
  The theory of high-energy neutrinos generation in the solar atmosphere
  during flares is developed. A possible effect in different neutrino
  detectors is discussed.

---------------------------------------------------------
Title: On the Dimension of Solar Attractor
Authors: Ostriakov, V. M.; Usoskin, I. G.
1990SoPh..127..405O    Altcode:
  Analyzing the average over a year (a) and over a month (b) of Wolf
  numbers and radiocarbon data (c), we have obtained the dimensions d
  of the solar attractor which are: 3.3 (a), 4.3 (b), 4.7 (c). During
  the Maunder minimum such a dimension turns out to be significantly
  higher: 8.0 (c); whereas during the period of a phase catastrophe
  (1792-1828) Wolf numbers averaged over a month yield d = 3.0 (b). We
  have also investigated the sensitivity of our inferences to the number
  of available experimental points. Positive values of the Kolmogorov
  entropy and first Lyapunov exponent explicitly show the stochastic
  behaviour of the Sun.

---------------------------------------------------------
Title: On the dimension of the solar attractor.
Authors: Ostryakov, V. M.; Usoskin, I. G.
1988BSolD1988...91O    Altcode:
  Analysing the year-averaged (a), monthly-averaged (b) Wolf numbers
  and radio carbon data (c) the authors have obtained dimensions d of
  the solar attractor which are: 3.25 (a), 4.3 (b), 4.7 (c). During the
  Maunder minimum the dimension turns out to be sufficiently higher:
  7.5 (c) whereas during the period of phase catastrophe (1792 - 1828)
  monthly-averaged Wolf numbers give d = 3.0 (b). Some consequences
  of calculations for modulation of galactic CR by solar activity are
  discussed.