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Author name code: vissers
ADS astronomy entries on 2022-09-14
author:"Vissers, Gregal J.M." 

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Title: Active region chromospheric magnetic fields. Observational
    inference versus magnetohydrostatic modelling
Authors: Vissers, G. J. M.; Danilovic, S.; Zhu, X.; Leenaarts, J.;
   Díaz Baso, C. J.; da Silva Santos, J. M.; de la Cruz Rodríguez,
   J.; Wiegelmann, T.
2022A&A...662A..88V    Altcode: 2021arXiv210902943V
  Context. A proper estimate of the chromospheric magnetic fields is
  thought to improve modelling of both active region and coronal mass
  ejection evolution. However, because the chromospheric field is not
  regularly obtained for sufficiently large fields of view, estimates
  thereof are commonly obtained through data-driven models or field
  extrapolations, based on photospheric boundary conditions alone and
  involving pre-processing that may reduce details and dynamic range in
  the magnetograms. <BR /> Aims: We investigate the similarity between
  the chromospheric magnetic field that is directly inferred from
  observations and the field obtained from a magnetohydrostatic (MHS)
  extrapolation based on a high-resolution photospheric magnetogram. <BR
  /> Methods: Based on Swedish 1-m Solar Telescope Fe I 6173 Å and
  Ca II 8542 Å observations of NOAA active region 12723, we employed
  the spatially regularised weak-field approximation (WFA) to derive
  the vector magnetic field in the chromosphere from Ca II, as well as
  non-local thermodynamic equilibrium (non-LTE) inversions of Fe I and Ca
  II to infer a model atmosphere for selected regions. Milne-Eddington
  inversions of Fe I serve as photospheric boundary conditions for the
  MHS model that delivers the three-dimensional field, gas pressure,
  and density self-consistently. <BR /> Results: For the line-of-sight
  component, the MHS chromospheric field generally agrees with the
  non-LTE inversions and WFA, but tends to be weaker by 16% on average
  than these when larger in magnitude than 300 G. The observationally
  inferred transverse component is systematically stronger, up to an
  order of magnitude in magnetically weaker regions, but the qualitative
  distribution with height is similar to the MHS results. For either
  field component, the MHS chromospheric field lacks the fine structure
  derived from the inversions. Furthermore, the MHS model does not
  recover the magnetic imprint from a set of high fibrils connecting
  the main polarities. <BR /> Conclusions: The MHS extrapolation and
  WFA provide a qualitatively similar chromospheric field, where the
  azimuth of the former is better aligned with Ca II 8542 Å fibrils than
  that of the WFA, especially outside strong-field concentrations. The
  amount of structure as well as the transverse field strengths are,
  however, underestimated by the MHS extrapolation. This underscores the
  importance of considering a chromospheric magnetic field constraint in
  data-driven modelling of active regions, particularly in the context
  of space weather predictions.

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Title: Heating of the solar chromosphere through current dissipation
Authors: da Silva Santos, J. M.; Danilovic, S.; Leenaarts, J.; de
   la Cruz Rodríguez, J.; Zhu, X.; White, S. M.; Vissers, G. J. M.;
   Rempel, M.
2022A&A...661A..59D    Altcode: 2022arXiv220203955D
  Context. The solar chromosphere is heated to temperatures higher than
  predicted by radiative equilibrium. This excess heating is greater
  in active regions where the magnetic field is stronger. <BR />
  Aims: We aim to investigate the magnetic topology associated with an
  area of enhanced millimeter (mm) brightness temperatures in a solar
  active region mapped by the Atacama Large Millimeter/submillimeter
  Array (ALMA) using spectropolarimetric co-observations with the 1-m
  Swedish Solar Telescope (SST). <BR /> Methods: We used Milne-Eddington
  inversions, nonlocal thermodynamic equilibrium (non-LTE) inversions,
  and a magnetohydrostatic extrapolation to obtain constraints on the
  three-dimensional (3D) stratification of temperature, magnetic field,
  and radiative energy losses. We compared the observations to a snapshot
  of a magnetohydrodynamics simulation and investigate the formation
  of the thermal continuum at 3 mm using contribution functions. <BR />
  Results: We find enhanced heating rates in the upper chromosphere of up
  to ∼5 kW m<SUP>−2</SUP>, where small-scale emerging loops interact
  with the overlying magnetic canopy leading to current sheets as shown
  by the magnetic field extrapolation. Our estimates are about a factor
  of two higher than canonical values, but they are limited by the ALMA
  spatial resolution (∼1.2″). Band 3 brightness temperatures reach
  about ∼10<SUP>4</SUP> K in the region, and the transverse magnetic
  field strength inferred from the non-LTE inversions is on the order
  of ∼500 G in the chromosphere. <BR /> Conclusions: We are able to
  quantitatively reproduce many of the observed features including the
  integrated radiative losses in our numerical simulation. We conclude
  that the heating is caused by dissipation in current sheets. However,
  the simulation shows a complex stratification in the flux emergence
  region where distinct layers may contribute significantly to the
  emission in the mm continuum. <P />The movie is available at <A
  href="https://www.aanda.org/10.1051/0004-6361/202243191/olm">https://www.aanda.org</A>

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Title: COCOPLOT: COlor COllapsed PLOTting software Using colour to
    view 3D data as a 2D image
Authors: Druett, Malcolm K.; Pietrow, Alexander G. M.; Vissers,
   Gregal J. M.; Robustini, Carolina; Calvo, Flavio
2022RASTI...1...29D    Altcode: 2021arXiv211110786D
  Most modern solar observatories deliver data products formatted as 3D
  spatio-temporal data cubes, that contain additional, higher dimensions
  with spectral and/or polarimetric information. This multi-dimensional
  complexity presents a major challenge when browsing for features of
  interest in several dimensions simultaneously. We developed the COlor
  COllapsed PLOTting (COCOPLOT) software as a quick-look and context image
  software, to convey spectral profile or time evolution from all the
  spatial pixels ($x,y$) in a 3D [$n_x,n_y,n_\lambda$] or [$n_x,n_y,n_t$]
  data cube as a single image, using color. This can avoid the need to
  scan through many wavelengths, creating difference and composite images
  when searching for signals satisfying multiple criteria. Filters are
  generated for the red, green, and blue channels by selecting values
  of interest to highlight in each channel, and their weightings. These
  filters are combined with the data cube over the third dimension axis
  to produce an $n_x \times n_y \times 3$ cube displayed as one true
  color image. Some use cases are presented for data from the Swedish 1-m
  Solar Telescope (SST) and IRIS, including H$\alpha$ solar flare data,
  a comparison with $k$-means clustering for identifying asymmetries
  in the Ca II K line and off-limb coronal rain in IRIS C II slit-jaw
  images. These illustrate identification by color alone using COCOPLOT
  of locations including line wing or central enhancement, broadening,
  wing absorption, and sites with intermittent flows or time-persistent
  features. COCOPLOT is publicly available in both IDL and Python.

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Title: COCOPLOT: COlor COllapsed PLOTting software
Authors: Druett, Malcolm K.; Pietrow, Alexander G. M.; Vissers,
   Gregal J. M.; Robustini, Carolina
2021ascl.soft11008D    Altcode:
  The COCOPLOT (COlor COllapsed PLOTting) quick-look and context image
  code conveys spectral profile information from all of the spatial
  pixels in a 3D datacube as a single image using color. It can also
  identify and expose temporal behavior and display and highlight
  solar features. COCOPLOT thus aids in identifying regions of interest
  quickly. The software is available in Python and IDL, and can be used
  as a standalone package or integrated into other software.

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Title: ISP-SST/ISPy: ISPy release v0.2.0
Authors: Díaz Baso, Carlos José; Vissers, Gregal; Calvo, Flavio;
   Pietrow, Alexander; Yadav, Rahul; De La Cruz Rodríguez, Jaime;
   Zivadinovic, Lazar
2021zndo...5608441D    Altcode: 2021zndo...5608441J
  This new version includes all previous features (basic functionality
  for SST data I/O and calibration, image alignment and inversion
  result visualisations) and the following new ones: neuralDenoising,
  potentialExtrapolation, field-dependent crosstalk, mapping to CEA
  coordinates, neuralEstimation, cube visualisation and routines for
  creating SST spectral line programs.

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Title: SSTRED: Data- and metadata-processing pipeline for CHROMIS
    and CRISP
Authors: Löfdahl, Mats G.; Hillberg, Tomas; de la Cruz Rodríguez,
   Jaime; Vissers, Gregal; Andriienko, Oleksii; Scharmer, Göran B.;
   Haugan, Stein V. H.; Fredvik, Terje
2021A&A...653A..68L    Altcode: 2018arXiv180403030L
  Context. Data from ground-based, high-resolution solar telescopes
  can only be used for science with calibrations and processing, which
  requires detailed knowledge about the instrumentation. Space-based
  solar telescopes provide science-ready data, which are easier to
  work with for researchers whose expertise is in the interpretation of
  data. Recently, data-processing pipelines for ground-based instruments
  have been constructed. <BR /> Aims: We aim to provide observers
  with a user-friendly data pipeline for data from the Swedish 1-meter
  Solar Telescope (SST) that delivers science-ready data together with
  the metadata needed for proper interpretation and archiving. <BR />
  Methods: We briefly describe the CHROMospheric Imaging Spectrometer
  (CHROMIS) instrument, including its (pre)filters, as well as recent
  upgrades to the CRisp Imaging SpectroPolarimeter (CRISP) prefilters and
  polarization optics. We summarize the processing steps from raw data
  to science-ready data cubes in FITS files. We report calibrations
  and compensations for data imperfections in detail. Misalignment
  of Ca II data due to wavelength-dependent dispersion is identified,
  characterized, and compensated for. We describe intensity calibrations
  that remove or reduce the effects of filter transmission profiles
  as well as solar elevation changes. We present REDUX, a new version
  of the MOMFBD image restoration code, with multiple enhancements and
  new features. It uses projective transforms for the registration of
  multiple detectors. We describe how image restoration is used with
  CRISP and CHROMIS data. The science-ready output is delivered in FITS
  files, with metadata compliant with the SOLARNET recommendations. Data
  cube coordinates are specified within the World Coordinate System
  (WCS). Cavity errors are specified as distortions of the WCS wavelength
  coordinate with an extension of existing WCS notation. We establish
  notation for specifying the reference system for Stokes vectors with
  reference to WCS coordinate directions. The CRIsp SPectral EXplorer
  (CRISPEX) data-cube browser has been extended to accept SSTRED output
  and to take advantage of the SOLARNET metadata. <BR /> Results: SSTRED
  is a mature data-processing pipeline for imaging instruments, developed
  and used for the SST/CHROMIS imaging spectrometer and the SST/CRISP
  spectropolarimeter. SSTRED delivers well-characterized, science-ready,
  archival-quality FITS files with well-defined metadata. The SSTRED
  code, as well as REDUX and CRISPEX, is freely available through git
  repositories.

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Title: Non-LTE inversions of a confined X2.2 flare. I. The vector
    magnetic field in the photosphere and chromosphere
Authors: Vissers, G. J. M.; Danilovic, S.; de la Cruz Rodríguez,
   J.; Leenaarts, J.; Morosin, R.; Díaz Baso, C. J.; Reid, A.; Pomoell,
   J.; Price, D. J.; Inoue, S.
2021A&A...645A...1V    Altcode: 2020arXiv200901537V
  Context. Obtaining an accurate measurement of magnetic field vector
  in the solar atmosphere is essential for studying changes in field
  topology during flares and reliably modelling space weather. <BR />
  Aims: We tackle this problem by applying various inversion methods to a
  confined X2.2 flare that occurred in NOAA AR 12673 on 6 September 2017
  and comparing the photospheric and chromospheric magnetic field vector
  with the results of two numerical models of this event. <BR /> Methods:
  We obtained the photospheric magnetic field from Milne-Eddington
  and (non-)local thermal equilibrium (non-LTE) inversions of Hinode
  SOT/SP Fe I 6301.5 Å and 6302.5 Å. The chromospheric field was
  obtained from a spatially regularised weak-field approximation (WFA)
  and non-LTE inversions of Ca II 8542 Å observed with CRISP at the
  Swedish 1 m Solar Telescope. We investigated the field strengths
  and photosphere-to-chromosphere shear in the field vector. <BR />
  Results: The LTE- and non-LTE-inferred photospheric magnetic field
  components are strongly correlated across several optical depths in
  the atmosphere, with a tendency towards a stronger field and higher
  temperatures in the non-LTE inversions. For the chromospheric field,
  the non-LTE inversions correlate well with the spatially regularised
  WFA, especially in terms of the line-of-sight field strength and field
  vector orientation. The photosphere exhibits coherent strong-field
  patches of over 4.5 kG, co-located with similar concentrations
  exceeding 3 kG in the chromosphere. The obtained field strengths
  are up to two to three times higher than in the numerical models,
  while the photosphere-to-chromosphere shear close to the polarity
  inversion line is more concentrated and structured. <BR /> Conclusions:
  In the photosphere, the assumption of LTE for Fe I line formation
  does not yield significantly different magnetic field results in
  comparison to the non-LTE case, while Milne-Eddington inversions
  fail to reproduce the magnetic field vector orientation where Fe
  I is in emission. In the chromosphere, the non-LTE-inferred field
  is excellently approximated by the spatially regularised WFA. Our
  inversions confirm the locations of flux rope footpoints that have
  been predicted by numerical models. However, pre-processing and lower
  spatial resolution lead to weaker and smoother field in the models than
  what our data indicate. This highlights the need for higher spatial
  resolution in the models to better constrain pre-eruptive flux ropes.

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Title: Probing chromospheric heating with millimeter interferometry
Authors: da Silva Santos, J. M.; de la Cruz Rodriguez, J.; White,
   S. M.; Leenaarts, J.; Vissers, G. J. M.; Hansteen, V. H.; Danilovic, S.
2020AGUFMSH0010001D    Altcode:
  Observations at visible and ultraviolet wavelengths have shown that
  solar active regions host different kinds of small-scale, transient,
  bright structures that are believed to be heating events resulting
  from the release of magnetic energy in the low atmosphere of the Sun,
  especially at the early stages of flux emergence. It is of great
  scientific interest to be able to accurately infer temperatures and
  formation heights of the most localized events, which are still
  matter of debate, in the hope of learning about the evolution of
  active regions where occasionally more energetic phenomena lead to
  much larger outbursts that propagate across the Solar System. The
  millimeter (mm) continuum is a new complementary diagnostic for
  chromospheric heating that is now available thanks to the Atacama
  Large Millimeter/submillimeter Array (ALMA). <P />We report on the
  first ALMA 3 mm observations of small-scale heating events in a
  solar active region. In contrast with the low-amplitude brightness
  temperature variations in the quiet-Sun, the interferometric maps show
  that the active region consists of long, warm, fibril-like structures
  that connect magnetic concentrations of opposite polarity and often
  flare up along with compact, flickering mm-bursts -- reminiscent of
  ultraviolet bursts -- with brightness temperatures of up to 14000 K at
  1.2" scales. These events also show simultaneous EUV emission observed
  by the Solar Dynamics Observatory (SDO). We find a weak correlation
  between the photospheric bright patches and the 3 mm continuum
  brightness and, in particular, we do not detect any mm counterpart of
  Ellerman bombs which confirms that they are photospheric phenomena. <P
  />Our observations and modelling highlight the diagnostic capabilities
  of ALMA for local heating in solar active regions and emphasize the
  need for coordinated observations with IRIS and DKIST in the future.

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Title: ALMA observations of transient heating in a solar active region
Authors: da Silva Santos, J. M.; de la Cruz Rodríguez, J.; White,
   S. M.; Leenaarts, J.; Vissers, G. J. M.; Hansteen, V. H.
2020A&A...643A..41D    Altcode: 2020arXiv200614564D
  <BR /> Aims: We aim to investigate the temperature enhancements and
  formation heights of solar active-region brightenings such as Ellerman
  bombs (EBs), ultraviolet bursts (UVBs), and flaring active-region
  fibrils (FAFs) using interferometric observations in the millimeter
  (mm) continuum provided by the Atacama Large Millimeter/submillimeter
  Array (ALMA). <BR /> Methods: We examined 3 mm signatures of heating
  events identified in Solar Dynamics Observatory observations of an
  active region and compared the results with synthetic spectra from a 3D
  radiative magnetohydrodynamic simulation. We estimated the contribution
  from the corona to the mm brightness using differential emission measure
  analysis. <BR /> Results: We report the null detection of EBs in the 3
  mm continuum at ∼1.2″ spatial resolution, which is evidence that
  they are sub-canopy events that do not significantly contribute to
  heating the upper chromosphere. In contrast, we find the active region
  to be populated with multiple compact, bright, flickering mm-bursts -
  reminiscent of UVBs. The high brightness temperatures of up to ∼14 200
  K in some events have a contribution (up to ∼7%) from the corona. We
  also detect FAF-like events in the 3 mm continuum. These events show
  rapid motions of &gt; 10 kK plasma launched with high plane-of-sky
  velocities (37 - 340 km s<SUP>-1</SUP>) from bright kernels. The mm FAFs
  are the brightest class of warm canopy fibrils that connect magnetic
  regions of opposite polarities. The simulation confirms that ALMA
  should be able to detect the mm counterparts of UVBs and small flares
  and thus provide a complementary diagnostic for localized heating in the
  solar chromosphere. <P />Movie associated to Fig. 5 is available at <A
  href="https://www.aanda.org/10.1051/0004-6361/202038755/olm">https://www.aanda.org</A>

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Title: Stratification of canopy magnetic fields in a plage
    region. Constraints from a spatially-regularized weak-field
    approximation method
Authors: Morosin, Roberta; de la Cruz Rodríguez, Jaime; Vissers,
   Gregal J. M.; Yadav, Rahul
2020A&A...642A.210M    Altcode: 2020arXiv200614487M
  Context. The role of magnetic fields in the chromospheric heating
  problem remains greatly unconstrained. Most theoretical predictions from
  numerical models rely on a magnetic configuration, field strength, and
  connectivity; the details of which have not been well established with
  observational studies for many chromospheric scenarios. High-resolution
  studies of chromospheric magnetic fields in plage are very scarce
  or non existent in general. <BR /> Aims: Our aim is to study the
  stratification of the magnetic field vector in plage regions. Previous
  studies predict the presence of a magnetic canopy in the chromosphere
  that has not yet been studied with full-Stokes observations. We
  use high-spatial resolution full-Stokes observations acquired with
  the CRisp Imaging Spectro-Polarimeter (CRISP) at the Swedish 1-m
  Solar Telescope in the Mg I 5173 Å, Na I 5896 Å and Ca II 8542
  Å lines. <BR /> Methods: We have developed a spatially-regularized
  weak-field approximation (WFA) method, based on the idea of spatial
  regularization. This method allows for a fast computation of magnetic
  field maps for an extended field of view. The fidelity of this new
  technique has been assessed using a snapshot from a realistic 3D
  magnetohydrodynamics simulation. <BR /> Results: We have derived the
  depth-stratification of the line-of-sight component of the magnetic
  field from the photosphere to the chromosphere in a plage region. The
  magnetic fields are concentrated in the intergranular lanes in the
  photosphere and expand horizontally toward the chromosphere, filling
  all the space and forming a canopy. Our results suggest that the
  lower boundary of this canopy must be located around 400 - 600 km
  from the photosphere. The mean canopy total magnetic field strength
  in the lower chromosphere (z ≈ 760 km) is 658 G. At z = 1160 km,
  we estimate ⟨B<SUB>∥</SUB>⟩ ≈ 417 G. <BR /> Conclusions:
  In this study we propose a modification to the WFA that improves
  its applicability to data with a worse signal-to-noise ratio. We
  have used this technique to study the magnetic properties of the hot
  chromospheric canopy that is observed in plage regions. The methods
  described in this paper provide a quick and reliable way of studying
  multi layer magnetic field observations without the many difficulties
  inherent to other inversion methods.

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Title: High-resolution observations of the solar photosphere,
    chromosphere, and transition region. A database of coordinated IRIS
    and SST observations
Authors: Rouppe van der Voort, L. H. M.; De Pontieu, B.; Carlsson,
   M.; de la Cruz Rodríguez, J.; Bose, S.; Chintzoglou, G.; Drews, A.;
   Froment, C.; Gošić, M.; Graham, D. R.; Hansteen, V. H.; Henriques,
   V. M. J.; Jafarzadeh, S.; Joshi, J.; Kleint, L.; Kohutova, P.;
   Leifsen, T.; Martínez-Sykora, J.; Nóbrega-Siverio, D.; Ortiz, A.;
   Pereira, T. M. D.; Popovas, A.; Quintero Noda, C.; Sainz Dalda, A.;
   Scharmer, G. B.; Schmit, D.; Scullion, E.; Skogsrud, H.; Szydlarski,
   M.; Timmons, R.; Vissers, G. J. M.; Woods, M. M.; Zacharias, P.
2020A&A...641A.146R    Altcode: 2020arXiv200514175R
  NASA's Interface Region Imaging Spectrograph (IRIS) provides
  high-resolution observations of the solar atmosphere through ultraviolet
  spectroscopy and imaging. Since the launch of IRIS in June 2013, we
  have conducted systematic observation campaigns in coordination with
  the Swedish 1 m Solar Telescope (SST) on La Palma. The SST provides
  complementary high-resolution observations of the photosphere and
  chromosphere. The SST observations include spectropolarimetric imaging
  in photospheric Fe I lines and spectrally resolved imaging in the
  chromospheric Ca II 8542 Å, Hα, and Ca II K lines. We present
  a database of co-aligned IRIS and SST datasets that is open for
  analysis to the scientific community. The database covers a variety
  of targets including active regions, sunspots, plages, the quiet Sun,
  and coronal holes.

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Title: Dissecting bombs and bursts: non-LTE inversions of
    low-atmosphere reconnection in SST and IRIS observations
Authors: Vissers, G. J. M.; de la Cruz Rodríguez, J.; Libbrecht,
   T.; Rouppe van der Voort, L. H. M.; Scharmer, G. B.; Carlsson, M.
2019A&A...627A.101V    Altcode: 2019arXiv190502035V
  Ellerman bombs and UV bursts are transient brightenings that are
  ubiquitously observed in the lower atmospheres of active and emerging
  flux regions. As they are believed to pinpoint sites of magnetic
  reconnection in reconfiguring fields, understanding their occurrence
  and detailed evolution may provide useful insight into the overall
  evolution of active regions. Here we present results from inversions
  of SST/CRISP and CHROMIS, as well as IRIS data of such transient
  events. Combining information from the Mg II h &amp; k, Si IV, and Ca
  II 8542 Å and Ca II H &amp; K lines, we aim to characterise their
  temperature and velocity stratification, as well as their magnetic
  field configuration. We find average temperature enhancements of
  a few thousand kelvin, close to the classical temperature minimum
  and similar to previous studies, but localised peak temperatures
  of up to 10 000-15 000 K from Ca II inversions. Including Mg II
  appears to generally dampen these temperature enhancements to below
  8000 K, while Si IV requires temperatures in excess of 10 000 K at
  low heights, but may also be reproduced with secondary temperature
  enhancements of 35 000-60 000 K higher up. However, reproducing Si
  IV comes at the expense of overestimating the Mg II emission. The
  line-of-sight velocity maps show clear bi-directional jet signatures
  for some events and strong correlation with substructure in the
  intensity images in general. Absolute line-of-sight velocities range
  between 5 and 20 km s<SUP>-1</SUP> on average, with slightly larger
  velocities towards, rather than away from, the observer. The inverted
  magnetic field parameters show an enhancement of the horizontal
  field co-located with the brightenings at heights similar to that of
  the temperature increase. We are thus able to largely reproduce the
  observational properties of Ellerman bombs with the UV burst signature
  (e.g. intensities, profile asymmetries, morphology, and bi-directional
  jet signatures), with temperature stratifications peaking close
  to the classical temperature minimum. Correctly modelling the Si
  IV emission in agreement with all other diagnostics is however an
  outstanding issue and remains paramount in explaining its apparent
  coincidence with Hα emission. Fine-tuning the approach (accounting for
  resolution differences, fitting localised temperature enhancements,
  and/or performing spatially coupled inversions) is likely necessary
  in order to obtain better agreement between all considered diagnostics.

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Title: Automating Ellerman bomb detection in ultraviolet continua
Authors: Vissers, Gregal J. M.; Rouppe van der Voort, Luc H. M.;
   Rutten, Robert J.
2019A&A...626A...4V    Altcode: 2019arXiv190107975V
  Ellerman bombs are transient brightenings in the wings of Hα 6563 Å
  that pinpoint photospheric sites of magnetic reconnection in solar
  active regions. Their partial visibility in the 1600 Å and 1700 Å
  continua registered routinely by the Atmospheric Imaging Assembly (AIA)
  onboard the Solar Dynamics Observatory (SDO) offers a unique opportunity
  to inventory such magnetic-field disruptions throughout the AIA database
  if a reliable recipe for their detection can be formulated. This is
  done here. We have improved and applied an Hα Ellerman bomb detection
  code to ten data sets spanning viewing angles from solar disc centre
  to the limb. They combine high-quality Hα imaging spectroscopy from
  the Swedish 1 m Solar Telescope with simultaneous AIA imaging around
  1600 Å and 1700 Å. A trial grid of brightness, lifetime and area
  constraints is imposed on the AIA images to define optimal recovery
  of the 1735 Ellerman bombs detected in Hα. The best results when
  optimising simultaneously for recovery fraction and reliability are
  obtained from 1700 Å images by requiring 5σ brightening above the
  average 1700 Å nearby quiet-Sun intensity, lifetime above one minute,
  area of 1-18 AIA pixels. With this recipe 27% of the AIA detections are
  Hα-detected Ellerman bombs while it recovers 19% of these (of which
  many are smaller than the AIA resolution). Better yet, among the top
  10% AIA 1700 Å detections selected with combined brightness, lifetime
  and area thresholds as many as 80% are Hα Ellerman bombs. Automated
  selection of the best 1700 Å candidates therefore opens the entire
  AIA database for detecting most of the more significant photospheric
  reconnection events. This proxy is applicable as a flux-dynamics
  tell-tale in studying any Earth-side solar active region since early
  2010 up to the present.

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Title: Solar Ultraviolet Bursts
Authors: Young, Peter R.; Tian, Hui; Peter, Hardi; Rutten, Robert J.;
   Nelson, Chris J.; Huang, Zhenghua; Schmieder, Brigitte; Vissers, Gregal
   J. M.; Toriumi, Shin; Rouppe van der Voort, Luc H. M.; Madjarska, Maria
   S.; Danilovic, Sanja; Berlicki, Arkadiusz; Chitta, L. P.; Cheung, Mark
   C. M.; Madsen, Chad; Reardon, Kevin P.; Katsukawa, Yukio; Heinzel, Petr
2018SSRv..214..120Y    Altcode: 2018arXiv180505850Y
  The term "ultraviolet (UV) burst" is introduced to describe small,
  intense, transient brightenings in ultraviolet images of solar active
  regions. We inventorize their properties and provide a definition
  based on image sequences in transition-region lines. Coronal signatures
  are rare, and most bursts are associated with small-scale, canceling
  opposite-polarity fields in the photosphere that occur in emerging flux
  regions, moving magnetic features in sunspot moats, and sunspot light
  bridges. We also compare UV bursts with similar transition-region
  phenomena found previously in solar ultraviolet spectrometry and
  with similar phenomena at optical wavelengths, in particular Ellerman
  bombs. Akin to the latter, UV bursts are probably small-scale magnetic
  reconnection events occurring in the low atmosphere, at photospheric
  and/or chromospheric heights. Their intense emission in lines with
  optically thin formation gives unique diagnostic opportunities
  for studying the physics of magnetic reconnection in the low solar
  atmosphere. This paper is a review report from an International Space
  Science Institute team that met in 2016-2017.

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Title: Intermittent Reconnection and Plasmoids in UV Bursts in the
    Low Solar Atmosphere
Authors: Rouppe van der Voort, L.; De Pontieu, B.; Scharmer, G. B.;
   de la Cruz Rodríguez, J.; Martínez-Sykora, J.; Nóbrega-Siverio,
   D.; Guo, L. J.; Jafarzadeh, S.; Pereira, T. M. D.; Hansteen, V. H.;
   Carlsson, M.; Vissers, G.
2017ApJ...851L...6R    Altcode: 2017arXiv171104581R
  Magnetic reconnection is thought to drive a wide variety of dynamic
  phenomena in the solar atmosphere. Yet, the detailed physical mechanisms
  driving reconnection are difficult to discern in the remote sensing
  observations that are used to study the solar atmosphere. In this
  Letter, we exploit the high-resolution instruments Interface Region
  Imaging Spectrograph and the new CHROMIS Fabry-Pérot instrument at
  the Swedish 1-m Solar Telescope (SST) to identify the intermittency
  of magnetic reconnection and its association with the formation of
  plasmoids in so-called UV bursts in the low solar atmosphere. The Si IV
  1403 Å UV burst spectra from the transition region show evidence of
  highly broadened line profiles with often non-Gaussian and triangular
  shapes, in addition to signatures of bidirectional flows. Such profiles
  had previously been linked, in idealized numerical simulations, to
  magnetic reconnection driven by the plasmoid instability. Simultaneous
  CHROMIS images in the chromospheric Ca II K 3934 Å line now provide
  compelling evidence for the presence of plasmoids by revealing highly
  dynamic and rapidly moving brightenings that are smaller than 0.″2 and
  that evolve on timescales of the order of seconds. Our interpretation
  of the observations is supported by detailed comparisons with synthetic
  observables from advanced numerical simulations of magnetic reconnection
  and associated plasmoids in the chromosphere. Our results highlight
  how subarcsecond imaging spectroscopy sensitive to a wide range of
  temperatures combined with advanced numerical simulations that are
  realistic enough to compare with observations can directly reveal the
  small-scale physical processes that drive the wide range of phenomena
  in the solar atmosphere.

---------------------------------------------------------
Title: Observing the Formation of Flare-driven Coronal Rain
Authors: Scullion, E.; Rouppe van der Voort, L.; Antolin, P.;
   Wedemeyer, S.; Vissers, G.; Kontar, E. P.; Gallagher, P. T.
2016ApJ...833..184S    Altcode: 2016arXiv161009255S
  Flare-driven coronal rain can manifest from rapidly cooled plasma
  condensations near coronal loop tops in thermally unstable postflare
  arcades. We detect five phases that characterize the postflare decay:
  heating, evaporation, conductive cooling dominance for ∼120 s,
  radiative/enthalpy cooling dominance for ∼4700 s, and finally
  catastrophic cooling occurring within 35-124 s, leading to rain
  strands with a periodicity of 55-70 s. We find an excellent agreement
  between the observations and model predictions of the dominant
  cooling timescales and the onset of catastrophic cooling. At the
  rain-formation site, we detect comoving, multithermal rain clumps
  that undergo catastrophic cooling from ∼1 MK to ∼22,000 K. During
  catastrophic cooling, the plasma cools at a maximum rate of 22,700
  K s<SUP>-1</SUP> in multiple loop-top sources. We calculated the
  density of the extreme-ultraviolet (EUV) plasma from the differential
  emission measure of the multithermal source employing regularized
  inversion. Assuming a pressure balance, we estimate the density of
  the chromospheric component of rain to be 9.21 × 10<SUP>11</SUP>
  ± 1.76 × 10<SUP>11</SUP> cm<SUP>-3</SUP>, which is comparable with
  quiescent coronal rain densities. With up to eight parallel strands
  in the EUV loop cross section, we calculate the mass loss rate from
  the postflare arcade to be as much as 1.98 × 10<SUP>12</SUP> ±
  4.95 × 10<SUP>11</SUP> g s<SUP>-1</SUP>. Finally, we reveal a close
  proximity between the model predictions of {10}<SUP>5.8</SUP> K and the
  observed properties between {10}<SUP>5.9</SUP> and {10}<SUP>6.2</SUP>
  K, which defines the temperature onset of catastrophic cooling. The
  close correspondence between the observations and numerical models
  suggests that indeed acoustic waves (with a sound travel time of 68 s)
  could play an important role in redistributing energy and sustaining
  the enthalpy-based radiative cooling.

---------------------------------------------------------
Title: Reconnection brightenings in the quiet solar photosphere
Authors: Rouppe van der Voort, Luc H. M.; Rutten, Robert J.; Vissers,
   Gregal J. M.
2016A&A...592A.100R    Altcode: 2016arXiv160603675R
  We describe a new quiet-Sun phenomenon which we call quiet-Sun
  Ellerman-like brightenings (QSEB). QSEBs are similar to Ellerman bombs
  (EB) in some respects but differ significantly in others. EBs are
  transient brightenings of the wings of the Balmer Hα line that mark
  strong-field photospheric reconnection in complex active regions. QSEBs
  are similar but smaller and less intense Balmer-wing brightenings
  that occur in quiet areas away from active regions. In the Hα wing,
  we measure typical lengths of less than 0.5 arcsec, widths of 0.23
  arcsec, and lifetimes of less than a minute. We discovered them
  using high-quality Hα imaging spectrometry from the Swedish 1-m
  Solar Telescope (SST) and show that, in lesser-quality data, they
  cannot be distinguished from more ubiquitous facular brightenings,
  nor in the UV diagnostics currently available from space platforms. We
  add evidence from concurrent SST spectropolarimetry that QSEBs also
  mark photospheric reconnection events, but in quiet regions on the
  solar surface. <P />The movies are available in electronic form at <A
  href="http://www.aanda.org/10.1051/0004-6361/201628889/olm">http://www.aanda.org</A>

---------------------------------------------------------
Title: Evidence for a Transition Region Response to Penumbral
    Microjets in Sunspots
Authors: Vissers, G. J. M.; Rouppe van der Voort, L. H. M.; Carlsson,
   M.
2015ApJ...811L..33V    Altcode: 2015arXiv150901402V
  Penumbral microjets (PMJs) are short-lived, fine-structured, and
  bright jets that are generally observed in chromospheric imaging of the
  penumbra of sunspots. Here we investigate their potential transition
  region signature by combining observations with the Swedish 1-m Solar
  Telescope in the Ca ii H and Ca ii 8542 Å lines with ultraviolet
  imaging and spectroscopy obtained with the Interface Region Imaging
  Spectrograph (IRIS), which includes the C ii 1334/1335 Å, Si iv
  1394/1403 Å, and Mg ii h &amp; k 2803/2796 Å lines. We find a clear
  corresponding signal in the IRIS Mg ii k, C ii, and Si iv slit-jaw
  images, typically offset spatially from the Ca ii signature in the
  direction along the jets: from base to top, the PMJs are predominantly
  visible in Ca ii, Mg ii k, and C ii/Si iv, suggesting progressive
  heating to transition region temperatures along the jet extent. Hence,
  these results support the suggestion from earlier studies that PMJs
  may heat to transition region temperatures.

---------------------------------------------------------
Title: Ellerman Bombs at High Resolution. III. Simultaneous
    Observations with IRIS and SST
Authors: Vissers, G. J. M.; Rouppe van der Voort, L. H. M.; Rutten,
   R. J.; Carlsson, M.; De Pontieu, B.
2015ApJ...812...11V    Altcode: 2015arXiv150700435V
  Ellerman bombs (EBs) are transient brightenings of the extended wings
  of the solar Balmer lines in emerging active regions. We describe
  their properties in the ultraviolet lines sampled by the Interface
  Region Imaging Spectrograph (IRIS), using simultaneous imaging
  spectroscopy in Hα with the Swedish 1-m Solar Telescope (SST) and
  ultraviolet images from the Solar Dynamics Observatory for Ellerman
  bomb detection and identification. We select multiple co-observed
  EBs for detailed analysis. The IRIS spectra strengthen the view that
  EBs mark reconnection between bipolar kilogauss fluxtubes with the
  reconnection and the resulting bi-directional jet located within the
  solar photosphere and shielded by overlying chromospheric fibrils in
  the cores of strong lines. The spectra suggest that the reconnecting
  photospheric gas underneath is heated sufficiently to momentarily reach
  stages of ionization normally assigned to the transition region and the
  corona. We also analyze similar outburst phenomena that we classify as
  small flaring arch filaments and ascribe to reconnection at a higher
  location. They have different morphologies and produce hot arches in
  million-Kelvin diagnostics.

---------------------------------------------------------
Title: Ellerman Bombs at High Resolution. IV. Visibility in Na I
    and Mg I
Authors: Rutten, R. J.; Rouppe van der Voort, L. H. M.; Vissers,
   G. J. M.
2015ApJ...808..133R    Altcode: 2015arXiv150604426R
  Ellerman bombs are transient brightenings of the wings of the solar
  Balmer lines that mark reconnection in the photosphere. Ellerman noted
  in 1917 that he did not observe such brightenings in the Na i D and
  Mg i b lines. This non-visibility should constrain EB interpretation,
  but has not been addressed in published bomb modeling. We therefore
  test Ellerman’s observation and confirm it using high-quality imaging
  spectrometry with the Swedish 1-m Solar Telescope. However, we find
  a diffuse brightness in these lines that seems to result from prior
  EBs. We tentatively suggest this is a post-bomb hot-cloud phenomenon
  also found in recent EB spectroscopy in the ultraviolet.

---------------------------------------------------------
Title: The Multithermal and Multi-stranded Nature of Coronal Rain
Authors: Antolin, P.; Vissers, G.; Pereira, T. M. D.; Rouppe van der
   Voort, L.; Scullion, E.
2015ApJ...806...81A    Altcode: 2015arXiv150404418A
  We analyze coordinated observations of coronal rain in loops,
  spanning chromospheric, transition region (TR), and coronal
  temperatures with sub-arcsecond spatial resolution. Coronal rain
  is found to be a highly multithermal phenomenon with a high degree
  of co-spatiality in the multi-wavelength emission. EUV darkening
  and quasi-periodic intensity variations are found to be strongly
  correlated with coronal rain showers. Progressive cooling of coronal
  rain is observed, leading to a height dependence of the emission. A
  fast-slow two-step catastrophic cooling progression is found, which
  may reflect the transition to optically thick plasma states. The
  intermittent and clumpy appearance of coronal rain at coronal heights
  becomes more continuous and persistent at chromospheric heights
  just before impact, mainly due to a funnel effect from the observed
  expansion of the magnetic field. Strong density inhomogeneities of
  0\buildrel{\prime\prime}\over{.} 2-0\buildrel{\prime\prime}\over{.} 5
  are found, in which a transition from temperatures of 10<SUP>5</SUP>
  to 10<SUP>4</SUP> K occurs. The 0\buildrel{\prime\prime}\over{.}
  2-0\buildrel{\prime\prime}\over{.} 8 width of the distribution
  of coronal rain is found to be independent of temperature. The
  sharp increase in the number of clumps at the coolest temperatures,
  especially at higher resolution, suggests that the bulk distribution
  of the rain remains undetected. Rain clumps appear organized in
  strands in both chromospheric and TR temperatures. We further find
  structure reminiscent of the magnetohydrodynamic (MHD) thermal mode
  (also known as entropy mode), thereby suggesting an important role of
  thermal instability in shaping the basic loop substructure. Rain core
  densities are estimated to vary between 2 × 10<SUP>10</SUP> and 2.5×
  {{10}<SUP>11</SUP>} cm<SUP>-3</SUP>, leading to significant downward
  mass fluxes per loop of 1-5 × 10<SUP>9</SUP> g s<SUP>-1</SUP>, thus
  suggesting a major role in the chromosphere-corona mass cycle.

---------------------------------------------------------
Title: Ellerman bombs: Advances driven by high-resolution observations
Authors: Vissers, Gregal
2014cosp...40E3533V    Altcode:
  Ellerman bombs, transient brightenings that have traditionally been
  observed in the wings of the Balmer Halpha line, are a ubiquitous
  phenomenon in the lower atmosphere of active regions with considerable
  flux emergence. These explosive events display sub-arcsecond fine
  structure, fast dynamical evolution and their energies tend to
  fall in the nanoflare ballpark. Over the past decade and a half,
  several high-resolution ground-based and space-based telescopes
  have contributed greatly to further characterising Ellerman bombs,
  offering a view in spectral diagnostics ranging from the UV to the
  infrared. I will highlight some of the recent advances that have been
  made - both observationally and from a theoretical point of view -
  in determining their properties (quantitative morphology, energies,
  flows and proper motion, driving mechanism, etc.), and discuss the
  potential of observations from relatively new space-based telescopes,
  such as SDO and IRIS, to add to our understanding of this phenomenon.

---------------------------------------------------------
Title: Ellerman Bombs at High Resolution. II. Triggering, Visibility,
    and Effect on Upper Atmosphere
Authors: Vissers, Gregal J. M.; Rouppe van der Voort, Luc H. M.;
   Rutten, Robert J.
2013ApJ...774...32V    Altcode: 2013arXiv1307.1547V
  We use high-resolution imaging spectroscopy with the Swedish 1-m Solar
  Telescope (SST) to study the transient brightenings of the wings
  of the Balmer Hα line in emerging active regions that are called
  Ellerman bombs. Simultaneous sampling of Ca II 8542 Å with the SST
  confirms that most Ellerman bombs also occur in the wings of this
  line, but with markedly different morphology. Simultaneous images
  from the Solar Dynamics Observatory (SDO) show that Ellerman bombs
  are also detectable in the photospheric 1700 Å continuum, again with
  differing morphology. They are also observable in 1600 Å SDO images,
  but with much contamination from C IV emission in transition-region
  features. Simultaneous SST spectropolarimetry in Fe I 6301 Å shows that
  Ellerman bombs occur at sites of strong-field magnetic flux cancellation
  between small bipolar strong-field patches that rapidly move together
  over the solar surface. Simultaneous SDO images in He II 304 Å, Fe IX
  171 Å, and Fe XIV 211 Å show no clear effect of the Ellerman bombs
  on the overlying transition region and corona. These results strengthen
  our earlier suggestion, based on Hα morphology alone, that the Ellerman
  bomb phenomenon is a purely photospheric reconnection phenomenon.

---------------------------------------------------------
Title: Ellerman bombs: fallacies, fads, usage
Authors: Rutten, Robert J.; Vissers, Gregal J. M.; Rouppe van der
   Voort, Luc H. M.; Sütterlin, Peter; Vitas, Nikola
2013JPhCS.440a2007R    Altcode: 2013arXiv1304.1364R
  Ellerman bombs are short-lived brightenings of the outer wings of Hα
  that occur in active regions with much flux emergence. We point out
  fads and fallacies in the extensive Ellerman bomb literature, discuss
  their appearance in various spectral diagnostics, and advocate their
  use as indicators of field reconfiguration in active-region topography
  using AIA 1700 Å images.

---------------------------------------------------------
Title: On-Disk Coronal Rain
Authors: Antolin, Patrick; Vissers, Gregal; Rouppe van der Voort, Luc
2012SoPh..280..457A    Altcode: 2012SoPh..tmp...78A; 2012arXiv1203.2077A
  Small and elongated, cool and dense blob-like structures are being
  reported with high resolution telescopes in physically different regions
  throughout the solar atmosphere. Their detection and the understanding
  of their formation, morphology, and thermodynamical characteristics can
  provide important information on their hosting environment, especially
  concerning the magnetic field, whose understanding constitutes a major
  problem in solar physics. An example of such blobs is coronal rain, a
  phenomenon of thermal non-equilibrium observed in active region loops,
  which consists of cool and dense chromospheric blobs falling along
  loop-like paths from coronal heights. So far, only off-limb coronal
  rain has been observed, and few reports on the phenomenon exist. In
  the present work, several data sets of on-disk Hα observations with
  the CRisp Imaging SpectroPolarimeter (CRISP) at the Swedish 1-m Solar
  Telescope (SST) are analyzed. A special family of on-disk blobs is
  selected for each data set, and a statistical analysis is carried out
  on their dynamics, morphology, and temperature. All characteristics
  present distributions which are very similar to reported coronal rain
  statistics. We discuss possible interpretations considering other
  similar blob-like structures reported so far and show that a coronal
  rain interpretation is the most likely one. The chromospheric nature
  of the blobs and the projection effects (which eliminate all direct
  possibilities of height estimation) on one side, and their small sizes,
  fast dynamics, and especially their faint character (offering low
  contrast with the background intensity) on the other side, are found
  as the main causes for the absence until now of the detection of this
  on-disk coronal rain counterpart.

---------------------------------------------------------
Title: Implications for Coronal Heating from Coronal Rain
Authors: Antolin, P.; Shibata, K.; Carlsson, M.; Rouppe van der Voort,
   L.; Vissers, G.; Hansteen, V.
2012ASPC..454..171A    Altcode:
  Coronal rain is a phenomenon above active regions in which cool plasma
  condensations fall down from coronal heights. Numerical simulations of
  loops have shown that such condensations can naturally form in the case
  of footpoint concentrated heating through the “catastrophic cooling”
  mechanism. In this work we analize high resolution limb observations in
  Ca II H and Hα of coronal rain performed by Hinode/SOT and by Crisp of
  SST and derive statistical properties. We further investigate the link
  between coronal rain and the coronal heating mechanisms by performing
  1.5-D MHD simulations of a loop subject to footpoint heating and to
  Alfvén waves generated in the photosphere. It is found that if a loop
  is heated predominantly from Alfvén waves coronal rain is inhibited
  due to the characteristic uniform heating they produce. Hence coronal
  rain can point both to the spatial distribution of the heating and to
  the agent of the heating itself, thus acting as a marker for coronal
  heating mechanisms.

---------------------------------------------------------
Title: A Sharp Look at Coronal Rain with Hinode/SOT and SST/CRISP
Authors: Antolin, P.; Carlsson, M.; Rouppe van der Voort, L.;
   Verwichte, E.; Vissers, G.
2012ASPC..455..253A    Altcode: 2012arXiv1202.0787A
  The tropical wisdom that when it is hot and dense we can expect
  rain might also apply to the Sun. Indeed, observations and numerical
  simulations have showed that strong heating at footpoints of loops,
  as is the case for active regions, puts their coronae out of thermal
  equilibrium, which can lead to a phenomenon known as catastrophic
  cooling. Following local pressure loss in the corona, hot plasma
  locally condenses in these loops and dramatically cools down to
  chromospheric temperatures. These blobs become bright in Hα and
  Ca ii H in time scales of minutes, and their dynamics seem to be
  subject more to internal pressure changes in the loop rather than to
  gravity. They thus become trackers of the magnetic field, which results
  in the spectacular coronal rain that is observed falling down coronal
  loops. In this work we report on high resolution observations of coronal
  rain with the Solar Optical Telescope (SOT) on Hinode and CRISP at
  the Swedish Solar Telescope (SST). A statistical study is performed in
  which properties such as velocities and accelerations of coronal rain
  are derived. We show how this phenomenon can constitute a diagnostic
  tool for the internal physical conditions inside loops. Furthermore, we
  analyze transverse oscillations of strand-like condensations composing
  coronal rain falling in a loop, and discuss the possible nature of the
  wave. This points to the important role that coronal rain can play in
  the fields of coronal heating and coronal seismology.

---------------------------------------------------------
Title: Flocculent Flows in the Chromospheric Canopy of a Sunspot
Authors: Vissers, Gregal; Rouppe van der Voort, Luc
2012ApJ...750...22V    Altcode: 2012arXiv1202.5453V
  High-quality imaging spectroscopy in the Hα line, obtained with the
  CRisp Imaging SpectroPolarimeter (CRISP) at the Swedish 1-m solar
  Telescope (SST) at La Palma and covering a small sunspot and its
  surroundings, is studied. They exhibit ubiquitous flows both along
  fibrils making up the chromospheric canopy away from the spot and
  in the superpenumbra. We term these flows "flocculent" to describe
  their intermittent character, that is, morphologically reminiscent
  of coronal rain. The flocculent flows are investigated further in
  order to determine their dynamic and morphological properties. For
  the measurement of their characteristic velocities, accelerations,
  and sizes, we employ a new versatile analysis tool, the CRisp
  SPectral EXplorer (CRISPEX), which we describe in detail. Absolute
  velocities on the order of 7.2-82.4 km s<SUP>-1</SUP> are found,
  with an average value of 36.5 ± 5.9 km s<SUP>-1</SUP> and slightly
  higher typical velocities for features moving toward the sunspot than
  away. These velocities are much higher than those determined from the
  shift of the line core, which shows patches around the sunspot with
  velocity enhancements of up to 10-15 km s<SUP>-1</SUP> (both red- and
  blueshifted). Accelerations are determined for a subsample of features
  that show clear accelerating or decelerating behavior, yielding an
  average of 270 ± 63 m s<SUP>-2</SUP> and 149 ± 63 m s<SUP>-2</SUP>
  for the accelerating and decelerating features, respectively. Typical
  flocculent features measure 627 ± 44 km in length and 304 ± 30 km
  in width. On average, 68 features are detected per minute, with an
  average lifetime of 67.7 ± 8.8 s. The dynamics and phenomenology
  of the flocculent flows suggest they may be driven by a siphon flow,
  where the flocculence could arise from a density perturbation close
  to one of the footpoints or along the loop structure.

---------------------------------------------------------
Title: Ellerman Bombs at High Resolution. I. Morphological Evidence
    for Photospheric Reconnection
Authors: Watanabe, Hiroko; Vissers, Gregal; Kitai, Reizaburo; Rouppe
   van der Voort, Luc; Rutten, Robert J.
2011ApJ...736...71W    Altcode: 2011arXiv1105.4008W
  High-resolution imaging-spectroscopy movies of solar active region NOAA
  10998 obtained with the Crisp Imaging Spectropolarimeter at the Swedish
  1-m Solar Telescope show very bright, rapidly flickering, flame-like
  features that appear intermittently in the wings of the Balmer Hα line
  in a region with moat flows and likely some flux emergence. They show
  up at regular Hα blue-wing bright points that outline the magnetic
  network, but flare upward with much larger brightness and distinct "jet"
  morphology seen from aside in the limbward view of these movies. We
  classify these features as Ellerman bombs and present a morphological
  study of their appearance at the unprecedented spatial, temporal, and
  spectral resolution of these observations. The bombs appear along the
  magnetic network with footpoint extents up to 900 km. They show apparent
  travel away from the spot along the pre-existing network at speeds
  of about 1 km s<SUP>-1</SUP>. The bombs flare repetitively with much
  rapid variation at timescales of seconds only, in the form of upward
  jet-shaped brightness features. These reach heights of 600-1200 km and
  tend to show blueshifts; some show bi-directional Doppler signature
  and some seem accompanied with an Hα surge. They are not seen in the
  core of Hα due to shielding by overlying chromospheric fibrils. The
  network where they originate has normal properties. The morphology of
  these jets strongly supports deep-seated photospheric reconnection of
  emergent or moat-driven magnetic flux with pre-existing strong vertical
  network fields as the mechanism underlying the Ellerman bomb phenomenon.

---------------------------------------------------------
Title: Dynamics of fine structure in the atmosphere of solar active
    regions
Authors: Vissers, Gregal Joan María
2011PhDT.......106V    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: Coronal Rain as a Marker for Coronal Heating Mechanisms
Authors: Antolin, P.; Shibata, K.; Vissers, G.
2010ApJ...716..154A    Altcode: 2009arXiv0910.2383A
  Reported observations in Hα, Ca II H, and K or other chromospheric
  lines of coronal rain trace back to the days of the Skylab
  mission. Corresponding to cool and dense plasma, coronal rain is often
  observed falling down along coronal loops in active regions. A physical
  explanation for this spectacular phenomenon has been put forward
  thanks to numerical simulations of loops with footpoint-concentrated
  heating, a heating scenario in which cool condensations naturally
  form in the corona. This effect has been termed "catastrophic cooling"
  and is the predominant explanation for coronal rain. In this work, we
  further investigate the link between this phenomenon and the heating
  mechanisms acting in the corona. We start by analyzing observations of
  coronal rain at the limb in the Ca II H line performed by the Hinode
  satellite, and derive interesting statistical properties concerning
  the dynamics. We then compare the observations with 1.5-dimensional
  MHD simulations of loops being heated by small-scale discrete events
  concentrated toward the footpoints (that could come, for instance,
  from magnetic reconnection events), and by Alfvén waves generated at
  the photospheric level. Both our observation and simulation results
  suggest that coronal rain is a far more common phenomenon than
  previously thought. Also, we show that the structure and dynamics of
  condensations are far more sensitive to the internal pressure changes
  in loops than to gravity. Furthermore, it is found that if a loop is
  predominantly heated from Alfvén waves, coronal rain is inhibited due
  to the characteristic uniform heating they produce. Hence, coronal
  rain may not only point to the spatial distribution of the heating
  in coronal loops but also to the agent of the heating itself. We thus
  propose coronal rain as a marker for coronal heating mechanisms.

---------------------------------------------------------
Title: On-disk Counterparts of Type II Spicules in the Ca II 854.2
    nm and Hα Lines
Authors: Rouppe van der Voort, L.; Leenaarts, J.; de Pontieu, B.;
   Carlsson, M.; Vissers, G.
2009ApJ...705..272R    Altcode: 2009arXiv0909.2115R
  Recently, a second type of spicules was discovered at the solar
  limb with the Solar Optical Telescope onboard the Japanese Hinode
  spacecraft. These previously unrecognized type II spicules are thin
  chromospheric jets that are shorter lived (10-60 s) and that show much
  higher apparent upward velocities (of order 50-100 km s<SUP>-1</SUP>)
  than the classical spicules. Since they have been implicated in
  providing hot plasma to coronal loops, their formation, evolution,
  and properties are important ingredients for a better understanding
  of the mass and energy balance of the low solar atmosphere. Here, we
  report on the discovery of the disk counterparts of type II spicules
  using spectral imaging data in the Ca II 854.2 nm and Hα lines with
  the CRisp Imaging SpectroPolarimeter at the Swedish Solar Telescope in
  La Palma. We find rapid blueward excursions in the line profiles of
  both chromospheric lines that correspond to thin, jet-like features
  that show apparent velocities of order 50 km s<SUP>-1</SUP>. These
  blueward excursions seem to form a separate absorbing component with
  Doppler shifts of order 20 and 50 km s<SUP>-1</SUP> for the Ca II 854.2
  nm and Hα line, respectively. We show that the appearance, lifetimes,
  longitudinal and transverse velocities, and occurrence rate of these
  rapid blue excursions on the disk are very similar to those of the type
  II spicules at the limb. A detailed study of the spectral line profiles
  in these events suggests that plasma is accelerated along the jet,
  and plasma is being heated throughout the short lifetime of the event.