explanation      blue bibcodes open ADS page with paths to full text
Author name code: braun
ADS astronomy entries on 2022-09-14
author:"Braun, Douglas C." 

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Title: Performance of the X-Calibur hard X-ray polarimetry mission
    during its 2018/19 long-duration balloon flight
Authors: Abarr, Q.; Beheshtipour, B.; Beilicke, M.; Bose, R.;
   Braun, D.; de Geronimo, G.; Dowkontt, P.; Errando, M.; Gadson, T.;
   Guarino, V.; Heatwole, S.; Hossen, M.; Iyer, N.; Kislat, F.; Kiss,
   M.; Kitaguchi, T.; Krawczynski, H.; Lanzi, J.; Li, S.; Lisalda, L.;
   Okajima, T.; Pearce, M.; Peterson, Z.; Press, L.; Rauch, B.; Simburger,
   G.; Stuchlik, D.; Takahashi, H.; Tang, J.; Uchida, N.; West, A.
2022APh...14302749A    Altcode: 2022arXiv220409761A
  X-Calibur is a balloon-borne telescope that measures the polarization of
  high-energy X-rays in the 15-50 keV energy range. The instrument makes
  use of the fact that X-rays scatter preferentially perpendicular to the
  polarization direction. A beryllium scattering element surrounded by
  pixellated CZT detectors is located at the focal point of the InFOCμS
  hard X-ray mirror. The instrument was launched for a long-duration
  balloon (LDB) flight from McMurdo (Antarctica) on December 29, 2018,
  and obtained the first constraints of the hard X-ray polarization of
  an accretion-powered pulsar. Here, we describe the characterization
  and calibration of the instrument on the ground and its performance
  during the flight, as well as simulations of particle backgrounds and
  a comparison to measured rates. The pointing system and polarimeter
  achieved the excellent projected performance. The energy detection
  threshold for the anticoincidence system was found to be higher than
  expected and it exhibited unanticipated dead time. Both issues will
  be remedied for future flights. Overall, the mission performance was
  nominal, and results will inform the design of the follow-up mission
  XL-Calibur, which is scheduled to be launched in summer 2022.

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Title: SuperTIGER Abundances of Galactic Cosmic Rays for the Atomic
    Number (Z) Interval 30 to 56
Authors: Walsh, N. E.; Akaike, Y.; Binns, W. R.; Bose, R. G.; Brandt,
   T. J.; Braun, D.; Cannady, N.; Dowkontt, P. F.; Hams, T.; Israel,
   M. H.; Krizmanic, J. F.; Labrador, A. W.; Link, J. T.; Mewaldt, R. A.;
   Mitchell, J. W.; Murphy, R. P.; Rauch, B. F.; Sakai, K.; Sasaki, M.;
   Simburger, G.; Stone, E. C.; Tatoli, T.; Ward, J. E.; Wiedenbeck,
   M. E.; Zober, W. V.; deNolfo, G. A.
2022icrc.confE.118W    Altcode: 2022PoS...395E.118W
  No abstract at ADS

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Title: Erratum: "Probing the Solar Meridional Circulation Using
    Fourier Legendre Decomposition" (2021, ApJ, 911, 54)
Authors: Braun, D. C.; Birch, A. C.; Fan, Y.
2022ApJ...924..140B    Altcode:
  No abstract at ADS

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Title: Global solar flows and their impact on magnetic activity
Authors: Dikpati, Mausumi; Braun, Douglas; Featherstone, Nicholas;
   Hindman, Bradley; Komm, Rudolf; Liu, Yang; Scherrer, Philip; Upton,
   Lisa; Wang, Haimin
2021AGUFMSH55D1872D    Altcode:
  This poster presents the second year progress report of the LWS
  focused-science team-4 of 2019. The main science objective is to
  jointly develop the most comprehensive, dynamically consistent picture
  of solar flows at the surface, in the convection zone and tachocline,
  and determine the MHD effects induced by these motions. Our major
  team-achievements in the second year include: (i) consensus about active
  regions' flow and their contributions in modifying the global flow;
  (ii) long-term global flow map from various magnetograms, and their
  specific properties as function of cycle phase, (iii) impacts of the
  flows in polar field evolutions, (iv) simulations of global flows with
  various solar-like interior conditions, (v) roles of simulated flows
  in driving the nonlinear dynamics of spot-producing magnetic fields
  and producing their spatio-temporal patterns, which are compared with
  that manifested as active regions patterns in surface magnetograms. We
  will describe in detail how these observationally constrained local and
  global flows are leading us to improved simulations of model-outputs of
  magnetic activity and flows. In turn, these outputs can reliably be used
  as inputs to heliospheric models, for example, for simulating properties
  of reconnection of active regions' magnetic fields, high-speed streams,
  sector passages, all of which have profound influence on various
  aspects of space weather and impact on terrestrial atmosphere.

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Title: Probing the Solar Meridional Circulation Using Fourier
    Legendre Decomposition
Authors: Braun, D. C.; Birch, A. C.; Fan, Y.
2021ApJ...911...54B    Altcode: 2021arXiv210302499B
  We apply the helioseismic methodology of Fourier Legendre decomposition
  to 88 months of Dopplergrams obtained by the Helioseismic and Magnetic
  Imager (HMI) as the basis of inferring the depth variation of the mean
  meridional flow, as averaged between 20° and 60° latitude and in
  time, in both the northern and southern hemispheres. We develop and
  apply control procedures designed to assess and remove center-to-limb
  artifacts using measurements obtained by performing the analysis with
  respect to artificial poles at the east and west limbs. Forward modeling
  is carried out using sensitivity functions proportional to the mode
  kinetic energy density to evaluate the consistency of the corrected
  frequency shifts with models of the depth variation of the meridional
  circulation in the top half of the convection zone. The results, taken
  at face value, imply substantial differences between the meridional
  circulation in the northern and southern hemispheres. The inferred
  presence of a return (equatorward propagating) flow at a depth of
  approximately 40 Mm below the photosphere in the northern hemisphere is
  surprising and appears to be inconsistent with many other helioseismic
  analyses. This discrepancy may be the result of the inadequacy of our
  methodology to remove systematic errors in HMI data. Our results appear
  to be at least qualitatively similar to those by Gizon et al., which
  point to an anomaly in HMI data that is not present in MDI or GONG data.

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Title: Global Solar Flows and Magnetic Fields: Observing, Simulating
    and Predicting Their Impact on the Heliosphere and Terrestrial
    Atmosphere
Authors: Dikpati, M.; Braun, D. C.; Featherstone, N. A.; Komm, R.;
   Liu, Y.; Scherrer, P. H.; Upton, L.; Wang, H.
2020AGUFMSH0020008D    Altcode:
  Understanding origins and evolution of solar magnetic activity occurring
  on a wide range of time-scales, and the space weather effects caused
  by the particles and electromagnetic outputs that reach the Earth,
  requires knowledge of the physical origins of this activity below
  photosphere. Despite much progress, our knowledge of processes
  responsible for driving the magnetohydrodynamics of flows and fields
  below photosphere and their relation to observed flows and magnetic
  activity is far from complete. For example, there is no consensus as to
  the number of meridional circulation-cells that exist in the Sun and the
  depth at which the poleward-flow switches direction to equatorward. Main
  objective of our LWS focused-science team is to jointly develop the
  most comprehensive, dynamically consistent picture of solar flows
  at the surface, in the convection zone and tachocline, and determine
  the MHD effects induced by these motions. We will present how we are
  developing consensus sets of observational constraints and simulating
  model-outputs of magnetic activity and flows, which can reliably be
  used as inputs to heliospheric and terrestrial- atmospheric models. The
  ultimate success will be in our ability to predict the features of
  solar cycle 25, including the active-latitudes and -longitudes, global-
  and localized-flows several months to years ahead.

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Title: Submerged Sources of Transient Acoustic Emission from Solar
    Flares
Authors: Lindsey, Charles; Buitrago-Casas, J. C.; Martínez Oliveros,
   Juan Carlos; Braun, Douglas; Martínez, Angel D.; Quintero Ortega,
   Valeria; Calvo-Mozo, Benjamín; Donea, Alina-Catalina
2020ApJ...901L...9L    Altcode:
  We report the discovery of ultra-impulsive acoustic emission from
  a solar flare, emission with a seismic signature that indicates
  submersion of its source approximately a Mm beneath the photosphere
  of the active region that hosted the flare. Just over two decades ago
  V. V. Zharkova and A. G. Kosovichev discovered the first acoustic
  transient released into the Sun's interior by a solar flare. These
  acoustic waves, refracted back upward to the solar surface after
  their release, make conspicuous Doppler ripples spreading outward
  from the flaring region that tell us a lot about their sources. The
  mechanism by which these transients are driven has stubbornly eluded
  our understanding. Some of the source regions, for example, are devoid
  of secondary Doppler, magnetic, or thermal disturbances in the outer
  atmosphere of the source regions that would signify the driving agent
  of an intense seismic transient in the outer atmosphere. In this
  study, we have applied helioseismic holography, a diagnostic based
  upon standard wave optics, to reconstruct a 3D image of the sources
  of acoustic waves emanating from the M9.3-class flare of 2011 July
  30. These images contain a source component that is submerged a full
  Mm beneath the active-region photosphere. The signature of acoustic
  sources this deep in the solar interior opens new considerations into
  the physics that must be involved in transient acoustic emission from
  flares—and possibly of flare physics at large. We develop analogies
  to seismicity remotely triggered by tremors from distant earthquakes,
  and consider prospects of new insight into the architecture of magnetic
  flux beneath flaring active regions.

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Title: Average motion of emerging solar active region
    polarities. II. Joy's law
Authors: Schunker, H.; Baumgartner, C.; Birch, A. C.; Cameron, R. H.;
   Braun, D. C.; Gizon, L.
2020A&A...640A.116S    Altcode: 2020arXiv200605565S
  Context. The tilt of solar active regions described by Joy's law
  is essential for converting a toroidal field to a poloidal field in
  Babcock-Leighton dynamo models. In thin flux tube models the Coriolis
  force causes what we observe as Joy's law, acting on east-west flows
  as they rise towards the surface. <BR /> Aims: Our goal is to measure
  the evolution of the average tilt angle of hundreds of active regions
  as they emerge, so that we can constrain the origins of Joy's law. <BR
  /> Methods: We measured the tilt angle of the primary bipoles in 153
  emerging active regions (EARs) in the Solar Dynamics Observatory
  Helioseismic Emerging Active Region survey. We used line-of-sight
  magnetic field measurements averaged over 6 h to define the polarities
  and measure the tilt angle up to four days after emergence. <BR />
  Results: We find that at the time of emergence the polarities are on
  average aligned east-west, and that neither the separation nor the
  tilt depends on latitude. We do find, however, that EARs at higher
  latitudes have a faster north-south separation speed than those closer
  to the equator at the emergence time. After emergence, the tilt
  angle increases and Joy's law is evident about two days later. The
  scatter in the tilt angle is independent of flux until about one day
  after emergence, when we find that higher-flux regions have a smaller
  scatter in tilt angle than lower-flux regions. <BR /> Conclusions:
  Our finding that active regions emerge with an east-west alignment
  is consistent with earlier observations, but is still surprising
  since thin flux tube models predict that tilt angles of rising flux
  tubes are generated below the surface. Previously reported tilt angle
  relaxation of deeply anchored flux tubes can be largely explained
  by the change in east-west separation. We conclude that Joy's law is
  caused by an inherent north-south separation speed present when the
  flux first reaches the surface, and that the scatter in the tilt angle
  is consistent with buffeting of the polarities by supergranulation.

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Title: Majorana representation for mixed states
Authors: Serrano-Ensástiga, E.; Braun, D.
2020PhRvA.101b2332S    Altcode: 2019arXiv190907740S
  We generalize the Majorana stellar representation of spin-s pure states
  to mixed states, and in general to any Hermitian operator, defining
  a bijective correspondence between three spaces: the spin-density
  matrices, a projective space of homogeneous polynomials of four
  variables, and a set of equivalence classes of points (constellations)
  on spheres of different radii. The representation behaves well under
  rotations by construction, and also under partial traces where the
  reduced density matrices inherit their constellation classes from
  the original state ρ . We express several concepts and operations
  related to density matrices in terms of the corresponding polynomials,
  such as the anticoherence criterion and the tensor representation of
  spin-s states described in Giraud et al. [Phys. Rev. Lett. 114, 080401
  (2015)]., 10.1103/PhysRevLett.114.080401

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Title: Probing the Variation with Depth of the Solar Meridional
    Circulation Using Legendre Function Decomposition
Authors: Braun, D. C.; Birch, A.; Fan, Y.
2020ASSP...57..125B    Altcode:
  We apply the helioseismic methodology of Legendre Function Decomposition
  to 7.5 years of Dopplergrams obtained by the Helioseismic and
  Magnetic Imager (HMI) as the basis of inferring the depth variation
  of the meridional flow between 20<SUP>∘</SUP> and 60<SUP>∘</SUP>
  latitude in both hemispheres. We assess and remove center-to-limb
  artifacts using measurements obtained by applying the procedure to
  pseudo poles at the east and west limbs. Forward modeling is carried
  out to evaluate the consistency of the corrected frequency shifts
  with models of the depth variation of the meridional circulation in
  the top half of the convection zone. The observations are consistent
  with a return flow in the northern hemisphere below about 40 Mm depth,
  but no obvious return flow in the south.

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Title: Average surface flows before the formation of solar active
    regions and their relationship to the supergranulation pattern
Authors: Birch, A. C.; Schunker, H.; Braun, D. C.; Gizon, L.
2019A&A...628A..37B    Altcode:
  Context. The emergence of solar active regions is an important but
  poorly understood aspect of the solar dynamo. <BR /> Aims: Knowledge
  of the flows associated with the rise of active-region-forming
  magnetic concentrations through the near-surface layers will help
  determine the mechanisms of active region formation. <BR /> Methods:
  We used helioseismic holography and granulation tracking to measure
  the horizontal flows at the surface that precede the emergence of
  active regions. We then averaged these flows over about sixty emerging
  active regions to reduce the noise, selecting active regions that
  emerge into relatively quiet Sun. To help interpret the results,
  we constructed a simple model flow field by generating synthetic
  "emergence locations" that are probabilistically related to the
  locations of supergranulation-scale convergence regions in the quiet
  Sun. <BR /> Results: The flow maps obtained from helioseismology and
  granulation tracking are very similar (correlation coefficients for
  single maps around 0.96). We find that active region emergence is,
  on average, preceded by converging horizontal flows of amplitude
  about 40 m s<SUP>-1</SUP>. The convergence region extends over about
  40 Mm in the east-west direction and about 20 Mm in the north-south
  direction and is centered in the retrograde direction relative to the
  emergence location. This flow pattern is largely reproduced by a model
  in which active region emergence occurs preferentially in the prograde
  direction relative to supergranulation inflows. <BR /> Conclusions:
  Averaging over many active regions reveals a statistically significant
  pattern of near-surface flows prior to emergence. The qualitative
  success of our simple model suggests that rising flux concentrations
  and supergranule-scale flows interact during the emergence process.

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Title: Probing the Variation with Depth of the Solar Meridional
    Circulation using Legendre Function Decomposition
Authors: Braun, Douglas; Birch, Aaron C.; Fan, Yuhong
2019AAS...23431802B    Altcode:
  The solar meridional circulation is a crucial component of magnetic flux
  transport and dynamo models. Despite decades of helioseismic study,
  no consensus exists regarding the variation of its properties with
  depth. It has become apparent that the main challenges consist of 1)
  overcoming realization noise with multi-year long datasets, and 2)
  the identification and robust removal of systematic center-to-limb
  effects. Here we apply the helioseismic methodology of Legendre
  Function Decomposition (LFD) to 7.5 years of Dopplergrams obtained by
  the Helioseismic and Magnetic Imager (HMI) as the basis of inferring
  the depth variation of the meridional flow between 20 and 60 degrees
  latitude in both hemispheres. The LFD method, first developed by Braun
  and Fan in 1998, probes subsurface flows through the Doppler-effect
  induced distortion of power spectra. The procedure is optimized for
  the detection of meridional flows and uses Legendre functions (of
  the first and second kind) to characterize poleward and equatorward
  wave propagation in spherical coordinates. For this study we have
  developed control procedures which assess and remove center-to-limb
  artifacts, using measurements obtained by applying the procedure to
  pseudo poles at the east and west limbs. Forward modeling is carried
  out to evaluate the consistency of the corrected LFD frequency shifts
  with various assumed models of the depth variation of the meridional
  circulation. <P />DB is supported by the NASA Heliophysics Division
  (awards 80NSSC18K0066 and 80NSSC18K0068) and by the Solar Terrestrial
  program of the National Science Foundation (award AGS-1623844).

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Title: Active Region Flows and their Contribution to Varying Global
    Dynamics
Authors: Braun, Douglas
2019AAS...23430210B    Altcode:
  We explore the general properties of the near-surface dynamics of
  solar active regions (ARs) and show how AR flows may contribute
  to longitudinally averaged measurements of global properties such
  as meridional circulation and torsional oscillations. Helioseismic
  holography is applied to HMI Dopplergrams yielding about 5000 flow
  measurements of 336 ARs observed by SDO between 2010 and 2014. Ensemble
  averages of the AR flows are presented, binned into subsets based on
  total magnetic flux. These averages show converging flows, with speeds
  about 10 m/s and spanning 10 degrees from the active region centers,
  which are apparent for most ARs above the flux limit of our survey at
  10<SUP>21</SUP> Mx. Retrograde flows are also detected, with amplitudes
  around 10 m/s, which predominantly, but not exclusively, flank the polar
  side of the ARs. The high signal-to-noise levels of these averages makes
  possible the assessment of individual AR contributions to time-varying
  global flows. We demonstrate this for several solar rotations, showing
  that individual active regions contribute substantially to these global
  flows. <P />This work is supported by the Solar Terrestrial program
  of the National Science Foundation (award AGS-1623844) and by the NASA
  Heliophysics Division (awards 80NSSC18K0066 and 80NSSC18K0068).

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Title: Average motion of emerging solar active region
    polarities. I. Two phases of emergence
Authors: Schunker, H.; Birch, A. C.; Cameron, R. H.; Braun, D. C.;
   Gizon, L.; Burston, R. B.
2019A&A...625A..53S    Altcode: 2019arXiv190311839S
  <BR /> Aims: Our goal is to constrain models of active region
  formation by tracking the average motion of active region polarity
  pairs as they emerge onto the surface. <BR /> Methods: We measured
  the motion of the two main opposite polarities in 153 emerging active
  regions using line-of-sight magnetic field observations from the Solar
  Dynamics Observatory Helioseismic Emerging Active Region (SDO/HEAR)
  survey. We first measured the position of each of the polarities
  eight hours after emergence, when they could be clearly identified,
  using a feature recognition method. We then tracked their location
  forwards and backwards in time. <BR /> Results: We find that, on
  average, the polarities emerge with an east-west orientation and the
  separation speed between the polarities increases. At about 0.1 days
  after emergence, the average separation speed reaches a peak value
  of 229 ± 11 ms<SUP>-1</SUP>, and then starts to decrease. About
  2.5 days after emergence the polarities stop separating. We also
  find that the separation and the separation speed in the east-west
  direction are systematically larger for active regions that have
  higher flux. The scatter in the location of the polarities increases
  from about 5 Mm at the time of emergence to about 15 Mm at two days
  after emergence. <BR /> Conclusions: Our results reveal two phases of
  the emergence process defined by the rate of change of the separation
  speed as the polarities move apart. Phase 1 begins when the opposite
  polarity pairs first appear at the surface, with an east-west alignment
  and an increasing separation speed. We define Phase 2 to begin when
  the separation speed starts to decrease, and ends when the polarities
  have stopped separating. This is consistent with a previous study: the
  peak of a flux tube breaks through the surface during Phase 1. During
  Phase 2 the magnetic field lines are straightened by magnetic tension,
  so that the polarities continue to move apart, until they eventually
  lie directly above their anchored subsurface footpoints. The scatter
  in the location of the polarities is consistent with the length and
  timescales of supergranulation, supporting the idea that convection
  buffets the polarities as they separate.

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Title: Flows around Averaged Solar Active Regions
Authors: Braun, D. C.
2019ApJ...873...94B    Altcode: 2019arXiv190202298B
  We explore the general properties of near-surface flows around
  solar active regions. Helioseismic holography is applied to HMI
  Dopplergrams yielding nearly 5000 flow measurements of 336 unique
  active regions observed by the Solar Dynamics Observatory between 2010
  and 2014. Ensemble averages of the flows, over subsets of regions
  sorted on the basis of magnetic flux, are performed. These averages
  show that converging flows, with speeds of about 10 m s<SUP>-1</SUP>
  and extending up to 10° from the active-region centers, are prevalent
  and have similar properties for all regions with magnetic flux above
  10<SUP>21</SUP> Mx. Retrograde flows are also detected, with amplitudes
  around 10 m s<SUP>-1</SUP>, which predominantly, but not exclusively,
  flank the polar side of the active regions. We estimate the expected
  contribution of these active-region flows to longitudinal averages
  of zonal and meridional flows and demonstrate the plausibility that
  they are responsible for at least some component of the time-varying
  global-scale flows. The reliability of our flow determination is tested
  using publicly available MHD simulations of both quiet-Sun convection
  and of a sunspot. While validating the overall methodology in general,
  the sunspot simulation demonstrates the presence of artifacts that
  may compromise quantitative flow inferences from some helioseismic
  measurements.

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Title: Validating Forward Modeling and Inversions of Helioseismic
    Holography Measurements
Authors: DeGrave, K.; Braun, D. C.; Birch, A. C.; Crouch, A. D.;
   Javornik, B.
2018ApJ...863...34D    Altcode: 2018arXiv180703841D
  Here, we use synthetic data to explore the performance of forward models
  and inverse methods for helioseismic holography. Specifically, this work
  presents the first comprehensive test of inverse modeling for flows
  using lateral-vantage (deep-focus) holography. We derive sensitivity
  functions in the Born approximation. We then use these sensitivity
  functions in a series of forward models and inversions of flows from a
  publicly available magnetohydrodynamic quiet-Sun simulation. The forward
  travel times computed using the kernels generally compare favorably with
  measurements obtained by applying holography, in a lateral-vantage
  configuration, on a 15 hr time series of artificial Dopplergrams
  extracted from the simulation. Inversions for the horizontal flow
  components are able to reproduce the flows in the upper 3 Mm of the
  domain, but are compromised by noise at greater depths.

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Title: Helioseismic Holography of Flows Around the Averaged Active
    Region
Authors: Braun, Douglas C.
2018tess.conf10628B    Altcode:
  We apply helioseismic holography to HMI observations of several
  hundred of the largest active regions and assess the inferred flows
  averaged after spatially aligning active regions selected in several
  ranges of magnetic flux. This ensemble averaging helps greatly reduce
  the dominating effect of the supergranulation signal. We also report
  progress on inferring the depth variation of these flows from modeling
  the variation of the helioseismic signatures as a function of focus
  depth. Some general features of the active-region flows among all flux
  groups include 1) compact outflows centered on both magnetic polarities,
  and 2) surrounding inflows with greater amplitudes in the trailing
  polarities. <P />This work is supported by the NSF Solar Terrestrial
  Program through grant AGS-1623844.

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Title: Helioseismic Constraints on the Subsurface Flows of the
    Averaged Supergranule
Authors: Braun, Douglas C.; Duvall, Thomas L., Jr.; Felipe, Tobias;
   DeGrave, Kyle
2018tess.conf11506B    Altcode:
  We report progress on constraining the subsurface flow properties
  of supergranulation from helioseismic holography applied to HMI/SDO
  observations of over 63,000 individual supergranules. First, using
  surface-focused measurements, we confirm the advantages of broader
  phase-speed filters in reducing diffraction effects, noted by Duvall
  and collaborators in prior time-distance analyses. Second, we expand
  the type of measurements to include deep-focusing geometries. Third,
  we compare all measurements with predictions made using numerical
  wave-propagation simulations performed with the 3D MANCHA code using
  a number of prescribed flow patterns. These model flows include those
  inferred from prior time-distance analyses as well as a model based
  on results of recent fully-convective MURaM-based computations. While
  the model predictions are in general qualitative agreement with the
  ensemble averaged measurements, no single model is fully consistent
  with the complete set of measurements. This suggests there is room
  for improvement in constraining the subsurface flows. <P />This work
  is supported by NASA grant 80NSSC18K0068 awarded to NWRA, as well as
  by the NASA High-End Computing program at Ames Research Center.

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Title: EMIC wave events during the four QARBM challenge intervals
Authors: Engebretson, M. J.; Posch, J. L.; Braun, D.; Li, W.;
   Angelopoulos, V.; Kellerman, A. C.; Kletzing, C.; Lessard, M.; Mann,
   I. R.; Tero, R.; Shiokawa, K.; Wygant, J. R.
2017AGUFMSM51B2433E    Altcode:
  We present observations of EMIC waves from multiple data sources
  during the four GEM challenge events in 2013 selected by the GEM
  focus group on Quantitative Assessment of Radiation Belt Modeling:
  March 17-18 (Stormtime Enhancement), May 31-June 2 (Stormtime Dropout),
  September 19-20 (Non-storm Enhancement), and September 23-25 (Non-storm
  Dropout). Observations include EMIC wave data from the Van Allen Probes
  and THEMIS spacecraft in the inner magnetosphere and from several
  arrays of ground-based search coil magnetometers worldwide, as well as
  localized ring current proton precipitation data from the low-altitude
  POES spacecraft. Each of these data sets provides only limited spatial
  coverage, but their combination reveals consistent occurrence patterns,
  which are then used to evaluate the effectiveness of EMIC waves in
  causing dropouts of radiation belt electrons during these GEM events.

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Title: Nightside High Latitude Magnetic Impulse Events
Authors: Engebretson, M. J.; Connors, M. G.; Braun, D.; Posch, J. L.;
   Kaur, M.; Guillon, S.; Hartinger, M.; Kim, H.; Behlke, R.; Reiter,
   K.; Jackel, B. J.; Russell, C. T.
2017AGUFMSM31B2629E    Altcode:
  High latitude Magnetic Impulse Events (MIEs), isolated pulses with
  periods 5-10 min, were first noted in ground-based magnetometer
  data near local noon, and are now understood to be signatures of
  transient pressure increases in the solar wind (sudden impulses -
  SIs) and/or in the ion foreshock (traveling convection vortex events
  - TCVs). However, solitary pulses with considerably larger amplitude
  (ΔB up to 1500 nT) have often been observed in the night sector at
  these same latitudes. These events are not directly associated with
  transient external pressure increases, and are often large enough
  to produce significant ground induced currents. Although many night
  sector MIEs occur in association with substorm signatures, others
  appear to be very isolated. We present here a survey of intense MIE
  events identified in magnetometer data from the AUTUMNX and MACCS
  arrays in eastern Arctic Canada at all local times between July 1,
  2014 and June 30, 2017. We also show maps of horizontal and vertical
  perturbations and maximum dB/dt values, as well as sample magnetograms,
  for several example events using data from these and other arrays in
  Arctic Canada, as well as in West Greenland and Antarctica, the latter
  to show the conjugate nature of these events. A basic relation to GIC
  data in the Hydro-Québec electrical transmission network in eastern
  Canada has been determined and will be discussed.

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Title: Helioseismic holography of simulated sunspots: dependence of
    the travel time on magnetic field strength and Wilson depression
Authors: Felipe, T.; Braun, D. C.; Birch, A. C.
2017A&A...604A.126F    Altcode: 2017arXiv170509135F
  Improving methods for determining the subsurface structure of sunspots
  from their seismic signature requires a better understanding of the
  interaction of waves with magnetic field concentrations. We aim to
  quantify the impact of changes in the internal structure of sunspots
  on local helioseismic signals. We have numerically simulated the
  propagation of a stochastic wave field through sunspot models with
  different properties, accounting for changes in the Wilson depression
  between 250 and 550 km and in the photospheric umbral magnetic field
  between 1500 and 3500 G. The results show that travel-time shifts at
  frequencies above approximately 3.50 mHz (depending on the phase-speed
  filter) are insensitive to the magnetic field strength. The travel
  time of these waves is determined exclusively by the Wilson depression
  and sound-speed perturbation. The travel time of waves with lower
  frequencies is affected by the direct effect of the magnetic field,
  although photospheric field strengths below 1500 G do not leave a
  significant trace on the travel-time measurements. These results could
  potentially be used to develop simplified travel-time inversion methods.

---------------------------------------------------------
Title: VizieR Online Data Catalog: Statistical analysis of solar
    active regions (Barnes+, 2014)
Authors: Barnes, G.; Birch, A. C.; Leka, K. D.; Braun, D. C.
2017yCat..17860019B    Altcode:
  In brief, samples from two populations are considered: "pre-emergence"
  targets (PE) that track a 32°x32° patch of the Sun prior to the
  emergence of a NOAA-numbered AR and "non-emergence" targets (NE)
  selected for lack of emergence and lack of strong fields in the
  central portions of the tracked patch. The PE sample size comprises
  107 targets obtained between 2001 and 2007, matched to 107 NE targets
  drawn from an initially larger sample and selected further to match
  the PE distributions in time and observing location on the disk. <P
  />(2 data files).

---------------------------------------------------------
Title: Driving Early Biochemical Reactions by the Thermal Accumulation
    of ATP over ADP/AMP?
Authors: Kühnlein, A.; Mast, C. B.; Benk, A.; Spatz, J. P.; Braun, D.
2017LPICo1967.4142K    Altcode:
  We propose a system which uses the prebiotically realistic thermal
  trap to locally shift the equilibrium of ADP and ATP towards an ATP
  bias and thereby allows biochemical reactions to take off.

---------------------------------------------------------
Title: Hosting Early Evolution in Heated Pores of Rock
Authors: Mast, C. B.; Möller, F.; Lanzmich, S.; Keil, L.; Braun, D.
2017LPICo1967.4037M    Altcode:
  Recent experiments with non-equilibrium micro­systems suggest that
  porous rock conditions drive early molecular evolution in many ways,
  including accumulation, polymerization, replication, length selection
  and gelation.

---------------------------------------------------------
Title: Thermally Driven Accumulation and Dry-Wet Cycles of Nucleotides
Authors: Morasch, M.; Liu, J.; Braun, D.
2017LPICo1967.4153M    Altcode:
  We show how a nonequilibrium system in form of a temperature gradient
  across porous rock creates high local concentrations and dry-wet cycles
  of nucleotides and other molecules.

---------------------------------------------------------
Title: Elucidating Signatures of the Genetic Code with Binding Assays
Authors: Edeleva, E. V.; Schwintek, P. J.; Braun, D.
2017LPICo1967.4036E    Altcode:
  What defined specific assignment of amino acids to their cognate
  codons during the emergence of the genetic code? In this project,
  we develop experimental strategies to test the stereochemical theory
  of the genetic code origin.

---------------------------------------------------------
Title: A Fixed-point Scheme for the Numerical Construction of
    Magnetohydrostatic Atmospheres in Three Dimensions
Authors: Gilchrist, S. A.; Braun, D. C.; Barnes, G.
2016SoPh..291.3583G    Altcode: 2016arXiv160900733G; 2016SoPh..tmp..182G
  Magnetohydrostatic models of the solar atmosphere are often based on
  idealized analytic solutions because the underlying equations are too
  difficult to solve in full generality. Numerical approaches, too, are
  often limited in scope and have tended to focus on the two-dimensional
  problem. In this article we develop a numerical method for solving the
  nonlinear magnetohydrostatic equations in three dimensions. Our method
  is a fixed-point iteration scheme that extends the method of Grad and
  Rubin (Proc. 2nd Int. Conf. on Peaceful Uses of Atomic Energy31, 190,
  1958) to include a finite gravity force. We apply the method to a test
  case to demonstrate the method in general and our implementation in
  code in particular.

---------------------------------------------------------
Title: SDO/HMI survey of emerging active regions for helioseismology
Authors: Schunker, H.; Braun, D. C.; Birch, A. C.; Burston, R. B.;
   Gizon, L.
2016A&A...595A.107S    Altcode: 2016arXiv160808005S
  Context. Observations from the Solar Dynamics Observatory (SDO) have
  the potential for allowing the helioseismic study of the formation of
  hundreds of active regions, which would enable us to perform statistical
  analyses. <BR /> Aims: Our goal is to collate a uniform data set of
  emerging active regions observed by the SDO/HMI instrument suitable for
  helioseismic analysis, where each active region is centred on a 60° ×
  60° area and can be observed up to seven days before emergence. <BR />
  Methods: We restricted the sample to active regions that were visible in
  the continuum and emerged into quiet Sun largely avoiding pre-existing
  magnetic regions. As a reference data set we paired a control region
  (CR), with the same latitude and distance from central meridian, with
  each emerging active region (EAR). The control regions do not have
  any strong emerging flux within 10° of the centre of the map. Each
  region was tracked at the Carrington rotation rate as it crossed
  the solar disk, within approximately 65° from the central meridian
  and up to seven days before, and seven days after, emergence. The
  mapped and tracked data, consisting of line-of-sight velocity,
  line-of-sight magnetic field, and intensity as observed by SDO/HMI,
  are stored in datacubes that are 410 min in duration and spaced 320
  min apart. We call this data set, which is currently comprised of 105
  emerging active regions observed between May 2010 and November 2012,
  the SDO Helioseismic Emerging Active Region (SDO/HEAR) survey. <BR />
  Results: To demonstrate the utility of a data set of a large number of
  emerging active regions, we measure the relative east-west velocity of
  the leading and trailing polarities from the line-of-sight magnetogram
  maps during the first day after emergence. The latitudinally averaged
  line-of-sight magnetic field of all the EARs shows that, on average,
  the leading (trailing) polarity moves in a prograde (retrograde)
  direction with a speed of 121 ± 22 m s<SUP>-1</SUP> (-70 ± 13 m
  s<SUP>-1</SUP>) relative to the Carrington rotation rate in the first
  day. However, relative to the differential rotation of the surface
  plasma, the east-west velocity is symmetric, with a mean of 95 ± 13
  m s<SUP>-1</SUP>. <BR /> Conclusions: The SDO/HEAR data set will not
  only be useful for helioseismic studies, but will also be useful to
  study other features such as the surface magnetic field evolution of
  a large sample of EARs. We intend to extend this survey forwards in
  time to include more EARs observed by SDO/HMI.

---------------------------------------------------------
Title: Helioseismic Holography of Simulated Sunspots: Magnetic and
    Thermal Contributions to Travel Times
Authors: Felipe, T.; Braun, D. C.; Crouch, A. D.; Birch, A. C.
2016ApJ...829...67F    Altcode: 2016arXiv160804893F
  Wave propagation through sunspots involves conversion between waves of
  acoustic and magnetic character. In addition, the thermal structure
  of sunspots is very different than that of the quiet Sun. As a
  consequence, the interpretation of local helioseismic measurements of
  sunspots has long been a challenge. With the aim of understanding these
  measurements, we carry out numerical simulations of wave propagation
  through sunspots. Helioseismic holography measurements made from
  the resulting simulated wavefields show qualitative agreement with
  observations of real sunspots. We use additional numerical experiments
  to determine, separately, the influence of the thermal structure of the
  sunspot and the direct effect of the sunspot magnetic field. We use the
  ray approximation to show that the travel-time shifts in the thermal
  (non-magnetic) sunspot model are primarily produced by changes in the
  wave path due to the Wilson depression rather than variations in the
  wave speed. This shows that inversions for the subsurface structure
  of sunspots must account for local changes in the density. In some
  ranges of horizontal phase speed and frequency there is agreement
  (within the noise level in the simulations) between the travel times
  measured in the full magnetic sunspot model and the thermal model. If
  this conclusion proves to be robust for a wide range of models, it
  would suggest a path toward inversions for sunspot structure.

---------------------------------------------------------
Title: Constraining the common properties of active region formation
    using the SDO/HEAR dataset
Authors: Schunker, H.; Braun, D. C.; Birch, A. C.
2016usc..confE...2S    Altcode:
  Observations from the Solar Dynamics Observatory (SDO) have the
  potential for allowing the helioseismic study of the formation of
  hundreds of active regions, which enable us to perform statistical
  analyses. We collated a uniform data set of emerging active regions
  (EARs) observed by the SDO/HMI instrument suitable for helioseismic
  analysis, where each active region can be observed up to 7 days before
  emergence. We call this dataset the SDO Helioseismic Emerging Active
  Region (SDO/HEAR) survey. We have used this dataset to to understand
  the nature of active region emergence. The latitudinally averaged
  line-of-sight magnetic field of all the EARs shows that the leading
  (trailing) polarity moves in a prograde (retrograde) direction with
  a speed of 110 ± 15 m/s (-60 ± 10 m/s) relative to the Carrington
  rotation rate in the first day after emergence. However, relative
  to the differential rotation of the surface plasma the East-West
  velocity is symmetric, with a mean of 90 ± 10 m/s. We have also
  compared the surface flows associated with the EARs at the time
  of emergence with surface flows from numerical simulations of flux
  emergence with different rise speeds. We found that the surface flows
  in simulations of emerging flux with a low rise speed of 70 m/s best
  match the observations.

---------------------------------------------------------
Title: A low upper limit on the subsurface rise speed of solar
    active regions
Authors: Birch, A. C.; Schunker, H.; Braun, D. C.; Cameron, R.; Gizon,
   L.; Lo ptien, B.; Rempel, M.
2016SciA....2E0557B    Altcode: 2016arXiv160705250B
  Magnetic field emerges at the surface of the Sun as sunspots and active
  regions. This process generates a poloidal magnetic field from a rising
  toroidal flux tube, it is a crucial but poorly understood aspect of
  the solar dynamo. The emergence of magnetic field is also important
  because it is a key driver of solar activity. We show that measurements
  of horizontal flows at the solar surface around emerging active regions,
  in combination with numerical simulations of solar magnetoconvection,
  can constrain the subsurface rise speed of emerging magnetic flux. The
  observed flows imply that the rise speed of the magnetic field is
  no larger than 150 m/s at a depth of 20 Mm, that is, well below the
  prediction of the (standard) thin flux tube model but in the range
  expected for convective velocities at this depth. We conclude that
  convective flows control the dynamics of rising flux tubes in the upper
  layers of the Sun and cannot be neglected in models of flux emergence.

---------------------------------------------------------
Title: Helioseismic Survey of the Near-surface Flows Around the
    Largest Active Regions with SDO-HMI Observations
Authors: Braun, Douglas; DeGrave, Kyle
2016SPD....47.0702B    Altcode:
  We report on the properties of the near-surface flows, determined from
  helioseismic holography applied to HMI Dopplergrams, of approximately
  250 of the largest active regions observed during the first five
  years of SDO observations. A recent study which examined the potential
  association of flows with the production of solar flares in this survey
  has recently been published (Braun 2016, ApJ 819, 106). We discuss here
  additional findings on general flow properties of the regions in our
  survey derived from ensemble averages of the flows. This averaging
  eliminates the dominating effect of the supergranulation signal,
  and shows outflows from sunspots surrounded by compact inflows. The
  properties of these flows are described. The potential use of these
  measurements for determining the contribution of active-region related
  flows to global dynamics (including differential rotation and meridional
  circulation) and flux-transport models is discussed. This work is
  supported by the NSF Solar Terrestrial Program through grant AGS-1127327
  and by the NASA Heliophysics Division through NNH12CF68C and NNX16AG88G.

---------------------------------------------------------
Title: Forward and Inverse Modeling of Helioseismic Holography
    Measurements of MHD Simulations of Convection and Sunspot Flows
Authors: DeGrave, Kyle; Braun, Douglas; Birch, Aaron; Crouch, Ashley
   D.; Javornik, Brenda; Rempel, Matthias D.
2016SPD....4720303D    Altcode:
  We test and validate newly-developed, empirically-derived sensitivity
  kernels for use in helioseismic analysis. These kernels are based on
  the Born approximation and derived from applying direct measurements to
  artificial realizations of incoming and scattered wavefields. These
  kernels are employed in a series of forward and inverse modeling
  of flows from the near-surface layers of two publicly available
  magnetohydrodynamic (MURaM-based) solar simulations - a quiet-Sun
  simulation, and one containing a sunspot. Forward travel times
  computed using the kernels generally compare favorably in non-magnetic
  regions. One finding of note is the presence of flow-like artifacts in
  the sunspot measurements which appear when the spot umbra or penumbra
  falls within the measurement pupils. Inversions for the horizontal flow
  components are able to reproduce the large-scale supergranule-sized
  flows in the upper 3Mm of both domains, but are compromised by noise
  at greater depths. In spite of the magnetic artifact, the moat flow
  surrounding the spot is at least qualitatively recovered. This work
  is supported by the NASA Heliophysics Division through NNH12CF68C,
  NNH12CF23C, and NNX16AG88G, and by the NSF Solar-Terrestrial Program
  through grant AGS-1127327.

---------------------------------------------------------
Title: Numerical construction of magneto-hydrostatic atmospheres in
    three dimensions
Authors: Gilchrist, Stuart; Braun, Douglas; Barnes, Graham
2016SPD....47.0706G    Altcode:
  There is a general interest in constructing magneto-hydrostatic
  models of the solar atmosphere. These models describe large-scale,
  long-lived magnetic structures like sunspots, prominences, coronal
  loops, and the corona itself on global scales. The nonlinearity
  of the magneto-hydrostatic equations prohibits direct analytic
  solution except when idealized approximations like self-similarity
  are made. Numerical approaches, too, are limited in scope, and
  primarily focus on the two-dimensional problem --- the general
  three-dimensional magneto-hydrostatic problem is not treated. In
  this presentation we present a new numerical scheme for solving the
  magneto-hydrostatic equations in three dimensions. We are presently
  using this method to construct sunspot models for helioseismic MHD
  wave-propagation simulations with the goal of comparing the simulations
  to local-helioseismic measurements. We will present the details of
  the method and its application to test cases.This work is supported
  by NASA Heliophysics Division through grant NNX14AD42G and by the NSF
  Solar-Terrestrial program through grant AGS-1127327.

---------------------------------------------------------
Title: Magnetic and Thermal Contributions to Helioseismic Travel
    times in Simulated Sunspots
Authors: Braun, Douglas; Felipe, Tobias; Birch, Aaron; Crouch,
   Ashley D.
2016SPD....47.0701B    Altcode:
  The interpretation of local helioseismic measurements of sunspots
  has long been a challenge, since waves propagating through sunspots
  are potentially affected by both mode conversion and changes in the
  thermal structure of the spots. We carry out numerical simulations of
  wave propagation through a variety of models which alternately isolate
  either the thermal or magnetic structure of the sunspot or include
  both of these. We find that helioseismic holography measurements made
  from the resulting simulated wavefields show qualitative agreement
  with observations of real sunspots. Using insight from ray theory,
  we find that travel-time shifts in the thermal (non-magnetic) sunspot
  model are primarily produced by changes in the wave path due to the
  Wilson depression rather than variations in the wave speed. This shows
  that inversions for the subsurface structure of sunspots must account
  for local changes in the density. In some ranges of horizontal phase
  speed and frequency there is agreement (within the noise level of the
  measurements) between the travel times measured in the full magnetic
  sunspot model and the thermal model. If this conclusion proves to
  be robust for a wide range of models, it suggests a path towards
  inversions for sunspot structure. This research has been funded
  by the Spanish MINECO through grant AYA2014-55078-P, by the NASA
  Heliophysics Division through NNX14AD42G and NNH12CF23C, and the NSF
  Solar Terrestrial program through AGS-1127327.

---------------------------------------------------------
Title: A Helioseismic Survey of Near-surface Flows Around Active
    Regions and their Association with Flares
Authors: Braun, D. C.
2016ApJ...819..106B    Altcode: 2016arXiv160200038B
  We use helioseismic holography to study the association of shallow
  flows with solar flare activity in about 250 large sunspot groups
  observed between 2010 and 2014 with the Helioseismic and Magnetic
  Imager on the Solar Dynamics Observatory. Four basic flow parameters:
  horizontal speed, horizontal component of divergence, vertical component
  of vorticity, and a vertical kinetic helicity proxy, are mapped for
  each active region (AR) during its passage across the solar disk. Flow
  indices are derived representing the mean and standard deviation of
  these parameters over magnetic masks and compared with contemporary
  measures of flare X-ray flux. A correlation exists for several of the
  flow indices, especially those based on the speed and the standard
  deviation of all flow parameters. However, their correlation with
  X-ray flux is similar to that observed with the mean unsigned magnetic
  flux density over the same masks. The temporal variation of the flow
  indices are studied, and a superposed epoch analysis with respect to the
  occurrence to 70 M and X-class flares is made. While flows evolve with
  the passage of the ARs across the disk, no discernible precursors or
  other temporal changes specifically associated with flares are detected.

---------------------------------------------------------
Title: Measurements with local helioseismology
Authors: Braun, D. C.
2015exse.book...77B    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: Influence of Magnetic and Thermal Effects on Helioseismic
    Travel-time Shifts in Sunspot Models
Authors: Felipe, Tobias; Braun, Douglas; Crouch, Ashley D.; Birch,
   Aaron
2014AAS...22420206F    Altcode:
  Sunspots are one of the most prominent manifestations of solar
  magnetic activity and have been studied using local helioseismology for
  decades. Recent modeling and observational studies indicate that the
  interpretation of travel-time shifts is still subject to uncertainties
  regarding the physical causes of the wave perturbations. Numerical wave
  propagation has proved useful in addressing this problem. In this work,
  we have analyzed travel-time shifts obtained from three dimensional
  numerical simulations of wave propagation in a magnetohydrostatic
  sunspot-like atmosphere. In particular, we isolate the individual
  effects of the magnetic field and thermal perturbations on the
  measurements by means of simulations where only one kind of perturbation
  (magnetic or thermal) is included. The resulting travel-time shift maps,
  obtained by applying helioseismic holography to the photospheric Doppler
  signals in the simulated domain, will be compared and discussed. We
  plan to make the artificial data available to the community for the
  development and validation of other helioseismic methods. This work
  is supported by the NASA SDO Science Center program (through contract
  NNH09CE41C) and by the NASA Living With a Star Program (through grant
  NNX14AD42G).

---------------------------------------------------------
Title: A Helioseismic Survey of Emerging Active Regions Using
    HMI-SDO Data
Authors: Braun, Douglas; Schunker, Hannah; Birch, Aaron
2014AAS...22420201B    Altcode:
  A survey of the subsurface properties of approximately 100 emerging
  active regions, determined from the application of helioseismic
  holography to Dopplergrams obtained with the HMI instrument onboard
  the Solar Dynamics Observatory, is being carried out. The goal of
  this research is to use helioseismology and numerical simulations to
  identify and understand possible signatures, in the form of acoustic
  travel time shifts, due to rising magnetic flux concentrations
  prior to their emergence at the solar photosphere. The status of
  the project and current results will be discussed. We make use of
  ensemble averages of travel-time shift measurements as proxies for
  near-surface depth-integrated wave-speed changes and flows. The latter
  include horizontal components of the flows as well as their horizontal
  divergence and the vertical component of the flow vorticity. A control
  sample of a similar number of quiet-Sun regions is used for comparison
  and for identifying potential systematic effects. Preliminary results
  confirm previous suggestions (obtained from a prior survey using GONG
  data) that emergence sites are associated with converging photospheric
  flows, such as the boundaries of supergranulation.This work is supported
  by the NASA Heliophysics Supporting Research program through contract
  NNH12CF23C.

---------------------------------------------------------
Title: A Helioseismic Survey to Investigate Relationships between
    Subsurface Flows beneath Large Active Regions and Solar Flares
Authors: Braun, Douglas; Leka, K D.; Barnes, Graham
2014AAS...22421815B    Altcode:
  A survey of the subsurface flow properties of about 120 of the largest
  active regions, determined from the application of helioseismic
  holography to Dopplergrams obtained with the HMI instrument onboard
  the Solar Dynamics Observatory, is being carried out. The overriding
  goal is to characterize differences in the subsurface flows between
  active regions associated with eruptive flares and the flows observed in
  relatively quiescent regions. Applications to flare forecasting comprise
  only one part of this investigation, since the potential response of
  the subsurface environment to eruptive events during and after their
  occurrence is also of scientific interest. Other priorities include
  understanding the limitations of the helioseismic methods, identifying
  and correcting systematic effects, and validating the reliability of
  the measurements using artificial data. While inversions to determine
  the variation with depth of subsurface flows are planned, preliminary
  results will be discussed which make use of proxies for near-surface
  depth-integrated properties, including the horizontal component of the
  flow divergence and the vertical component of the flow vorticity.This
  work is supported by the Solar Terrestrial Program of the National
  Science Foundation, through grant AGS-1127327, and by the National
  Oceanic and Atmospheric Administration SBIR program.

---------------------------------------------------------
Title: Studies on Forecasting Solar Flares
Authors: Leka, K. D.; Barnes, G.; Braun, D. C.; Wagner, E. L.
2014shin.confE.171L    Altcode:
  Forecasting solar flares is a challenge from various scientific
  perspectives; major solar flares are inherently rare events, and all
  observations available with which to evaluate the flare-readiness of the
  Sun are remote, with inferences about the physical state rather than
  direct measurements. We report on efforts to improve forecasts, using
  data from the Helioseismic and Magnetic Imager on the Solar Dynamics
  Observatory using magnetic field and helioseismic parametrization,
  magnetic charge topology and Discriminant Analysis. We report on
  preliminary results of the performance, including the temporal
  variations of the parametrizations. <P />This work is supported by
  NASA contract NNH12CG10C and NOAA Contract WC-133R-13-CN-0079

---------------------------------------------------------
Title: Using Synthetic Data From Convection Simulations To Test
    Helioseismic Holography Inversions For Three-Dimensional Vector Flows
Authors: Crouch, Ashley D.; Birch, Aaron; Braun, Douglas; Javornik,
   Brenda; Rempel, Matthias D.
2014AAS...22421807C    Altcode:
  We investigate the efficacy of helioseismic holography for inferring
  the three-dimensional vector flows in the near-surface layers of the
  solar interior. Synthetic helioseismic data are taken from compressible
  convection simulations. Travel times are measured from the synthetic
  data using helioseismic holography. Kernels for the sensitivity
  of travel times to subsurface flows are calculated using the Born
  approximation. Inversions for subsurface flows are then performed
  using subtractive optimally localized averaging. This provides an
  opportunity to evaluate the accuracy of the inversion technique. We
  compare the actual flows present in the convection simulations to the
  flows retrieved by the inversion. We discuss the influence of the
  regularization used by the inversion, and the effects of noise and
  spatial resolution. This work is supported by the NASA SDO Science
  Center program (NNH09CE41C), the NASA Heliophysics Guest Investigator
  program (NNH12CF68C), and the NASA LWS TR&amp;T tools and methods
  program (NNH09CF68C). The National Center for Atmospheric Research is
  sponsored by the National Science Foundation.

---------------------------------------------------------
Title: Helioseismology of Pre-emerging Active
    Regions. III. Statistical Analysis
Authors: Barnes, G.; Birch, A. C.; Leka, K. D.; Braun, D. C.
2014ApJ...786...19B    Altcode: 2013arXiv1307.1938B
  The subsurface properties of active regions (ARs) prior to their
  appearance at the solar surface may shed light on the process of
  AR formation. Helioseismic holography has been applied to samples
  taken from two populations of regions on the Sun (pre-emergence and
  without emergence), each sample having over 100 members, that were
  selected to minimize systematic bias, as described in Paper I. Paper
  II showed that there are statistically significant signatures in
  the average helioseismic properties that precede the formation of
  an AR. This paper describes a more detailed analysis of the samples
  of pre-emergence regions and regions without emergence based on
  discriminant analysis. The property that is best able to distinguish
  the populations is found to be the surface magnetic field, even
  a day before the emergence time. However, after accounting for the
  correlations between the surface field and the quantities derived from
  helioseismology, there is still evidence of a helioseismic precursor
  to AR emergence that is present for at least a day prior to emergence,
  although the analysis presented cannot definitively determine the
  subsurface properties prior to emergence due to the small sample sizes.

---------------------------------------------------------
Title: Helioseismic Holography of an Artificial Submerged Sound Speed
    Perturbation and Implications for the Detection of Pre-emergence
    Signatures of Active Regions
Authors: Braun, D. C.
2014SoPh..289..459B    Altcode: 2012SoPh..tmp..306B; 2012arXiv1210.7504B
  We use a publicly available numerical wave-propagation simulation
  of Hartlep et al. (Solar Phys.268, 321, 2011) to test the ability
  of helioseismic holography to detect signatures of a compact,
  fully submerged, 5 % sound-speed perturbation placed at a depth of
  50 Mm within a solar model. We find that helioseismic holography
  employed in a nominal "lateral-vantage" or "deep-focus" geometry
  employing quadrants of an annular pupil can detect and characterize
  the perturbation. A number of tests of the methodology, including the
  use of a plane-parallel approximation, the definition of travel-time
  shifts, the use of different phase-speed filters, and changes to
  the pupils, are also performed. It is found that travel-time shifts
  made using Gabor-wavelet fitting are essentially identical to those
  derived from the phase of the Fourier transform of the cross-covariance
  functions. The errors in travel-time shifts caused by the plane-parallel
  approximation can be minimized to less than a second for the depths and
  fields of view considered here. Based on the measured strength of the
  mean travel-time signal of the perturbation, no substantial improvement
  in sensitivity is produced by varying the analysis procedure from the
  nominal methodology in conformance with expectations. The measured
  travel-time shifts are essentially unchanged by varying the profile
  of the phase-speed filter or omitting the filter entirely. The method
  remains maximally sensitive when applied with pupils that are wide
  quadrants, as opposed to narrower quadrants or with pupils composed
  of smaller arcs. We discuss the significance of these results for the
  recent controversy regarding suspected pre-emergence signatures of
  active regions.

---------------------------------------------------------
Title: A Full-Sun Magnetic Index from Helioseismology Inferences
Authors: González Hernández, I.; Díaz Alfaro, M.; Jain, K.; Tobiska,
   W. K.; Braun, D. C.; Hill, F.; Pérez Hernández, F.
2014SoPh..289..503G    Altcode:
  Solar magnetic indices are used to model the solar irradiance and
  ultimately to forecast it. However, the observation of such indices is
  generally limited to the Earth-facing hemisphere of the Sun. Seismic
  maps of the far side of the Sun have proven their capability to locate
  and track medium-large active regions at the non-visible hemisphere. We
  present here the possibility of using the average signal from these
  seismic far-side maps, combined with similarly calculated near-side
  maps, as a proxy to the full-Sun magnetic activity.

---------------------------------------------------------
Title: The Relativistic Electron-Proton Telescope (REPT) Instrument
on Board the Radiation Belt Storm Probes (RBSP) Spacecraft:
    Characterization of Earth's Radiation Belt High-Energy Particle
    Populations
Authors: Baker, D. N.; Kanekal, S. G.; Hoxie, V. C.; Batiste, S.;
   Bolton, M.; Li, X.; Elkington, S. R.; Monk, S.; Reukauf, R.; Steg,
   S.; Westfall, J.; Belting, C.; Bolton, B.; Braun, D.; Cervelli, B.;
   Hubbell, K.; Kien, M.; Knappmiller, S.; Wade, S.; Lamprecht, B.;
   Stevens, K.; Wallace, J.; Yehle, A.; Spence, H. E.; Friedel, R.
2013SSRv..179..337B    Altcode: 2012SSRv..tmp..101B
  Particle acceleration and loss in the million electron Volt (MeV)
  energy range (and above) is the least understood aspect of radiation
  belt science. In order to measure cleanly and separately both the
  energetic electron and energetic proton components, there is a need for
  a carefully designed detector system. The Relativistic Electron-Proton
  Telescope (REPT) on board the Radiation Belt Storm Probe (RBSP)
  pair of spacecraft consists of a stack of high-performance silicon
  solid-state detectors in a telescope configuration, a collimation
  aperture, and a thick case surrounding the detector stack to shield the
  sensors from penetrating radiation and bremsstrahlung. The instrument
  points perpendicular to the spin axis of the spacecraft and measures
  high-energy electrons (up to ∼20 MeV) with excellent sensitivity
  and also measures magnetospheric and solar protons to energies well
  above E=100 MeV. The instrument has a large geometric factor ( g=0.2
  cm<SUP>2</SUP> sr) to get reasonable count rates (above background)
  at the higher energies and yet will not saturate at the lower energy
  ranges. There must be fast enough electronics to avert undue dead-time
  limitations and chance coincidence effects. The key goal for the REPT
  design is to measure the directional electron intensities (in the range
  10<SUP>-2</SUP>-10<SUP>6</SUP> particles/cm<SUP>2</SUP> s sr MeV)
  and energy spectra (Δ E/ E∼25 %) throughout the slot and outer
  radiation belt region. Present simulations and detailed laboratory
  calibrations show that an excellent design has been attained for the
  RBSP needs. We describe the engineering design, operational approaches,
  science objectives, and planned data products for REPT.

---------------------------------------------------------
Title: A Search for Pre-Emergence Helioseismic Signatures of Active
Regions: Study Design and some Average Results
Authors: Leka, K. D.; Birch, A.; Barnes, G.; Braun, D.; Javornik,
   B.; Gonzalez-Hernandez, I.; Dunn, T.
2013SPD....44...91L    Altcode:
  Helioseismology can be an important tool for understanding the
  formation of active regions. This poster describes the design of a
  recently completed study, testing whether pre-appearance signatures
  of solar magnetic active regions were detectable using various tools
  of local helioseismology. We provide details of the data selection
  and preparation of samples, each containing over 100 members, of
  two populations: regions on the Sun which produced a numbered NOAA
  active region, and a "control" sample of areas which did not. The
  seismology is performed on data from the GONG network; accompanying
  magnetic data from the Michelson Doppler Imager aboard SoHO are used
  for co-temporal analysis of the surface magnetic field. Samples are
  drawn from 2001--2007, and each target is analyzed for 27.7hr prior
  to an objectively determined time of emergence. We describe known
  sources of bias and the approaches used to mitigate them. Examining the
  average ensemble differences between the two populations, we describe
  significant and surprising differences between our samples in both
  quantities determined from helioseismology and from surface magnetic
  fields. This work was supported by NASA contract NNH07CD25C.

---------------------------------------------------------
Title: Far-side helioseismic maps: the next generation
Authors: González Hernández, Irene; Lindsey, Charles; Braun,
   Douglas C.; Bogart, Richard S.; Scherrer, Philip H.; Hill, Frank
2013JPhCS.440a2029G    Altcode:
  For more than a decade, far-side seismic maps of medium-to-large active
  regions have proven their capability as a space weather forecasting
  tool. In the last few years, these maps have started to serve another
  purpose: complementing the front side observations that are input to
  different solar models. Photospheric flux transport as well as solar
  spectral irradiance models have been shown to produce improved results
  when incorporating the far-side seismic maps as well as providing
  better forecasting. The challenge for the future is twofold: Far-side
  seismic monitoring needs to be more sensitive, and it needs to offer
  more information. We present here initial steps towards fulfilling
  these goals using higher resolution input images, adding extra skips
  to the analysis and changing the presentation of the maps.

---------------------------------------------------------
Title: The Helioseismic Search for Emerging Flux
Authors: Braun, D. C.
2013enss.confE..64B    Altcode:
  Arguably considered the holy grail of local helioseismology
  is the detection of emerging flux before its appearance as a
  sunspot or magnetic region on the photosphere. After almost two
  decades of searching, this goal remains elusive and, at best,
  controversial. Helioseismic exploration is increasingly assisted
  by numerical simulations of rising flux which offer predictions of
  the magnitude and type of signatures, and also by computational wave
  propagation models which can validate and help improve the methods. We
  discuss some of these developments as well as results of a recent
  survey, carried out at NWRA, of approximately one hundred emerging
  active regions observed with the GONG network. A new survey, carried
  out in collaboration with colleagues at the Max Planck Institute for
  Solar System Research and made using the observations obtained by the
  HMI instrument on SDO is under way. This talk reviews work at NWRA
  which has been funded through the NASA Living with a Star program
  and currently though the NASA Solar and Heliospheric SR&amp;T program
  (contract NNH12CF23C) and Heliophysics GI program (contract NNH12CF68C).

---------------------------------------------------------
Title: Testing Helioseismic-Holography Inversions for Supergranular
    Flows Using Synthetic Data
Authors: Dombroski, D. E.; Birch, A. C.; Braun, D. C.; Hanasoge, S. M.
2013SoPh..282..361D    Altcode: 2012arXiv1211.6886D
  Supergranulation is one of the most visible length scales of solar
  convection and has been studied extensively by local helioseismology. We
  use synthetic data computed with the Seismic Propagation through
  Active Regions and Convection (SPARC) code to test regularized-least
  squares (RLS) inversions of helioseismic-holography measurements
  for a supergranulation-like flow. The code simulates the acoustic
  wavefield by solving the linearized three-dimensional Euler equations
  in Cartesian geometry. We model a single supergranulation cell with
  a simple, axisymmetric, mass-conserving flow.

---------------------------------------------------------
Title: Helioseismology of Pre-emerging Active Regions. II. Average
    Emergence Properties
Authors: Birch, A. C.; Braun, D. C.; Leka, K. D.; Barnes, G.;
   Javornik, B.
2013ApJ...762..131B    Altcode: 2013arXiv1303.1391B
  We report on average subsurface properties of pre-emerging active
  regions as compared to areas where no active region emergence was
  detected. Helioseismic holography is applied to samples of the two
  populations (pre-emergence and without emergence), each sample having
  over 100 members, which were selected to minimize systematic bias,
  as described in Leka et al. We find that there are statistically
  significant signatures (i.e., difference in the means of more than a few
  standard errors) in the average subsurface flows and the apparent wave
  speed that precede the formation of an active region. The measurements
  here rule out spatially extended flows of more than about 15 m
  s<SUP>-1</SUP> in the top 20 Mm below the photosphere over the course
  of the day preceding the start of visible emergence. These measurements
  place strong constraints on models of active region formation.

---------------------------------------------------------
Title: Helioseismology of Pre-emerging Active Regions. I. Overview,
    Data, and Target Selection Criteria
Authors: Leka, K. D.; Barnes, G.; Birch, A. C.; Gonzalez-Hernandez,
   I.; Dunn, T.; Javornik, B.; Braun, D. C.
2013ApJ...762..130L    Altcode: 2013arXiv1303.1433L
  This first paper in a series describes the design of a study testing
  whether pre-appearance signatures of solar magnetic active regions
  were detectable using various tools of local helioseismology. The
  ultimate goal is to understand flux-emergence mechanisms by setting
  observational constraints on pre-appearance subsurface changes, for
  comparison with results from simulation efforts. This first paper
  provides details of the data selection and preparation of the samples,
  each containing over 100 members, of two populations: regions on
  the Sun that produced a numbered NOAA active region, and a "control"
  sample of areas that did not. The seismology is performed on data from
  the GONG network; accompanying magnetic data from SOHO/MDI are used
  for co-temporal analysis of the surface magnetic field. Samples are
  drawn from 2001-2007, and each target is analyzed for 27.7 hr prior
  to an objectively determined time of emergence. The results of two
  analysis approaches are published separately: one based on averages of
  the seismology- and magnetic-derived signals over the samples, another
  based on Discriminant Analysis of these signals, for a statistical test
  of detectable differences between the two populations. We include
  here descriptions of a new potential-field calculation approach
  and the algorithm for matching sample distributions over multiple
  variables. We describe known sources of bias and the approaches used
  to mitigate them. We also describe unexpected bias sources uncovered
  during the course of the study and include a discussion of refinements
  that should be included in future work on this topic.

---------------------------------------------------------
Title: X-Spec: A Multi-Object Wideband Survey Spectrograph for CCAT
Authors: Bradford, Charles; Hailey-Dunsheath, S.; Shirokoff, E.;
   Hollister, M.; Kovacs, A.; Zmuidzinas, J.; Padin, S.; Seiffert, M. D.;
   Braun, D.; Banales, G.; LeDuc, H.; Stacey, G. J.; Nikola, T.; Glenn,
   J.; Chapman, S.
2013AAS...22115009B    Altcode:
  We are developing a multi-object dispersive survey spectrograph
  for CCAT. X-Spec is optimized for rest-frame far-IR / submm atomic
  and molecular transitions in high-z galaxies, and it will conduct
  multi-galaxy spectral survey up to 10x faster than ALMA. Detected lines
  will provide redshifts for and interstellar gas conditions in tens of
  thousands of galaxies ranging from the early universe (z &gt; 6) to the
  present day. X-Spec will be particularly sensitive to the 158-micron
  ionized carbon fine-structure transition [CII], and the initial
  instrument will target the 650-um, 850-um, and 1-mm atmospheric windows,
  corresponding to 3.5 to 9 for [CII]. By following up high-z candidate
  objects, X-Spec surveys of [CII] will reveal the early evolution of
  galaxies' energy sources and interstellar gas conditions. CCAT/X-Spec
  can also probe below individually-detected sources by using fluctuation
  analyses; the spatial-spectral fluctuations mm and submm bands are
  dominated by [CII], and can be used to measure the growth of large-scale
  structure and the global properties of galaxies in the reionization
  epoch. X-Spec will have at least 15 independent spectrometer backend
  'pixels', each covering 195-520 GHz instantaneously at R=400-700,
  in both polarizations with photon-background-limited sensitivity. It
  will use lithographically-patterned filterbank chips formed with
  superconducting transmission line. The detectors are titanium-nitride
  kinetic inductance detectors (KIDs), and each spectrometer chip
  will have ~500 KIDs integrated with the filterbank in a package a
  few square cm in size. Each chip has a bandwidth of ~ 1:1.6 and is
  single-polarization, so coverage of the full 195-520 GHz range in
  dual-pol requires 4 chips and ~2000 detectors. With the compact size
  and inexpensive mass production, much larger spectrometer formats
  (100-300 pixels) will be possible as detector readout technology
  progresses. To optimize on-source observation efficiency, a 2-axis
  rotary positioning system for each pixel will steer to an arbitrary
  position in a circular patch of sky; this system will steer to target
  galaxies, compensate for field rotation, and enable beam modulation
  (chopping) at ~1-2 Hz for sky subtraction.

---------------------------------------------------------
Title: Scattering of the f-mode by Small Magnetic Flux Elements from
    Observations and Numerical Simulations
Authors: Felipe, T.; Braun, D.; Crouch, A.; Birch, A.
2012ApJ...757..148F    Altcode: 2012arXiv1208.4024F
  The scattering of f-modes by magnetic tubes is analyzed using
  three-dimensional numerical simulations. An f-mode wave packet is
  propagated through a solar atmosphere embedded with three different
  flux tube models that differ in radius and total magnetic flux. A
  quiet-Sun simulation without a tube present is also performed as a
  reference. Waves are excited inside the flux tube and propagate along
  the field lines, and jacket modes are generated in the surroundings
  of the flux tube, carrying 40% as much energy as the tube modes. The
  resulting scattered wave is mainly an f-mode composed of a mixture of m
  = 0 and m = ±1 modes. The amplitude of the scattered wave approximately
  scales with the magnetic flux. A small amount of power is scattered
  into the p <SUB>1</SUB>-mode. We have evaluated the absorption and
  phase shift from a Fourier-Hankel decomposition of the photospheric
  vertical velocities. They are compared with the results obtained
  from the ensemble average of 3400 small magnetic elements observed in
  high-resolution MDI Doppler datacubes. The comparison shows that the
  observed dependence of the phase shift with wavenumber can be matched
  reasonably well with the simulated flux tube model. The observed
  variation of the phase shifts with the azimuthal order m appears to
  depend on details of the ensemble averaging, including possible motions
  of the magnetic elements and asymmetrically shaped elements.

---------------------------------------------------------
Title: A Search for Pre-Emergence Helioseismic Signatures of Active
    Regions
Authors: Barnes, Graham; Birch, A.; Leka, K.; Braun, D.; Dunn, T.;
   Javornik, B.; Gonzalez Hernandez, I.
2012AAS...22020510B    Altcode:
  Helioseismology can be an important tool for understanding the formation
  of active regions. As a first step towards this goal, we have carried
  out a search for statistically significant helioseismic precursors
  of active region emergence. We used an automatic method to determine
  the time of emergence based on the NOAA/NGDC active region catalog
  and MDI/SOHO 96 minute magnetograms. Using GONG data, we applied
  helioseismic holography to 107 pre-emergence active regions and a
  control sample of 107 regions where no active region was present. We
  found some significant and surprising differences between our samples
  in both quantities determined from helioseismology and from surface
  magnetic fields. However, we do not see a clear signature of emergence
  when considering individual active regions. The results of this
  investigation may shed some light on the mechanism responsible for
  flux emergence, and certainly illustrate the care which must be taken
  in conducting such an investigation. <P />This work was supported by
  NASA contract NNH07CD25C.

---------------------------------------------------------
Title: Comparison of Numerical and Observational Scattering of the
    f-mode by Small Magnetic Elements
Authors: Felipe, Tobias; Braun, D. C.; Crouch, A. D.; Birch, A. C.
2012AAS...22010906F    Altcode:
  The observed scattering of the f-mode by small magnetic elements
  is studied through Fourier-Hankel analysis and compared with
  three-dimensional numerical simulations of the scattering produced by
  magnetic flux tube models. The numerical setup consists of an f-mode
  wave packet which is propagated through a realistic solar atmosphere
  embedded with a flux tube model. A quiet Sun simulation without a
  tube present is also performed as a reference. Sausage (m=0) and kink
  (m=±1) modes are excited in the flux tube and propagate along the field
  lines, and jacket modes are generated in the surroundings of the flux
  tube, carrying 40% as much energy as the tube modes. The resulting
  scattered wave is mainly an f-mode composed of a mixture of m=0 and
  m=±1 modes. We find the observed dependence of the phase shift with
  wavenumber for an ensemble average of about 3400 magnetic elements
  can be matched reasonably well with the simulated flux tube model. The
  observed variation with azimuthal order m of the phase-shifts appears
  to depend on details of the ensemble averaging, including possible
  motions of the magnetic elements and asymmetrically shaped elements. <P
  />This research has been funded by NASA through projects NNH09CE43C,
  NNH09CF68C, and NNH07CD25C.

---------------------------------------------------------
Title: Comment on “Detection of Emerging Sunspot Regions in the
    Solar Interior”
Authors: Braun, Douglas C.
2012Sci...336..296B    Altcode:
  Ilonidis et al. (Reports, 19 August 2011, p. 993) report acoustic
  travel-time decreases associated with emerging sunspot regions before
  their appearance on the solar surface. An independent analysis using
  helioseismic holography does not confirm these travel-time anomalies for
  the four regions illustrated by Ilonidis et al. This negative finding
  is consistent with expectations based on current emerging flux models.

---------------------------------------------------------
Title: Helioseismology of a Realistic Magnetoconvective Sunspot
    Simulation
Authors: Braun, D. C.; Birch, A. C.; Rempel, M.; Duvall, T. L.
2012ApJ...744...77B    Altcode:
  We compare helioseismic travel-time shifts measured from a realistic
  magnetoconvective sunspot simulation using both helioseismic holography
  and time-distance helioseismology, and measured from real sunspots
  observed with the Helioseismic and Magnetic Imager instrument on
  board the Solar Dynamics Observatory and the Michelson Doppler Imager
  instrument on board the Solar and Heliospheric Observatory. We
  find remarkable similarities in the travel-time shifts measured
  between the methodologies applied and between the simulated and real
  sunspots. Forward modeling of the travel-time shifts using either Born
  or ray approximation kernels and the sound-speed perturbations present
  in the simulation indicates major disagreements with the measured
  travel-time shifts. These findings do not substantially change with
  the application of a correction for the reduction of wave amplitudes
  in the simulated and real sunspots. Overall, our findings demonstrate
  the need for new methods for inferring the subsurface structure of
  sunspots through helioseismic inversions.

---------------------------------------------------------
Title: Numerical simulations of the subsurface structure of sunspots
Authors: Rempel, M.; Cheung, M.; Birch, A. C.; Braun, D. C.
2011AGUFMSH52B..02R    Altcode:
  Knowledge of the subsurface magnetic field and flow structure of
  sunspots is essential for understanding the processes involved in their
  formation, dynamic evolution and decay. Information on the subsurface
  structure can be obtained by either direct numerical modeling or
  helioseismic inversions. Numerical simulations have reached only
  in recent years the point at which entire sunspots or even active
  regions can be modeled including all relevant physical processes
  such as 3D radiative transfer and a realistic equation of state. We
  present in this talk results from a series of different models: from
  simulations of individual sunspots (with and without penumbrae) in
  differently sized computational domains to simulations of the active
  region formation process (flux emergence). It is found in all models
  that the subsurface magnetic field fragments on an intermediate scale
  (larger than the scale of sunspot fine structure such as umbral dots);
  most of these fragmentations become visible as light bridges or flux
  separation events in the photosphere. The subsurface field strength is
  found to be in the 5-10 kG range. The simulated sunspots are surrounded
  by large scale flows, the most dominant and robust flow component is
  a deep reaching outflow with an amplitude reaching about 50% of the
  convective RMS velocity at the respective depth. The simulated sunspots
  show helioseismic signatures (frequency dependent travel time shifts)
  similar to those in observed sunspots. On the other hand it is clear
  from the simulations that these signatures originate in the upper
  most 2-3 Mm of the convection zone, since only there substantial
  perturbations of the wave speed are present. The contributions from
  deeper layers are insignificant, in particular a direct comparison
  between an 8 Mm and 16 Mm deep simulation leads to indiscernible
  helioseismic differences. The National Center for Atmospheric Research
  is sponsored by the National Science Foundation. This work is in part
  supported through the NASA SDO Science Center.

---------------------------------------------------------
Title: Numerical simulations of scattering of f-modes by magnetic
    flux tubes
Authors: Felipe, Tobias; Birch, Aaron C.; Crouch, Ashley D.; Braun,
   Douglas C.
2011sdmi.confE..80F    Altcode:
  The scattering of the f-mode by a magnetic flux tube is analyzed
  using three-dimensional numerical simulations. An f-mode wave packet
  is propagated through a realistic solar atmosphere embedded with a
  flux tube of 200 km radius and 1600 G field strength. A quiet Sun
  simulation without the tube being present is also performed as a
  reference. Sausage (m=0) and kink (m=± 1) modes are excited in the
  magnetic tube and propagate downward along the field lines, while the
  resulting scattered wave is mainly an f-mode composed of a mixture
  of m=0 and m=± 1 modes. Low power is also scattered into high-order
  acoustic p-modes. We have evaluated the absorption and phase shift
  from a Fourier-Hankel decomposition of the vertical velocities.

---------------------------------------------------------
Title: "Hare and Hounds" Tests of Helioseismic Holography
Authors: Birch, A. C.; Parchevsky, K. V.; Braun, D. C.; Kosovichev,
   A. G.
2011SoPh..272...11B    Altcode: 2011SoPh..tmp..315B; 2011SoPh..tmp..290B; 2011SoPh..tmp..257B;
   2011SoPh..tmp..188B
  We use the output of numerical wave-propagation simulations as synthetic
  data for "hare and hounds" tests of helioseismic holography. In
  the simple non-magnetic models examined here, we show that when the
  inversion method includes a consistent treatment of the filtering
  applied during the data analysis the inversions for the subsurface
  sound speed are qualitatively correct.

---------------------------------------------------------
Title: Towards physics-based helioseismic inversions of subsurface
    sunspot structure
Authors: Braun, D. C.; Birch, A. C.; Crouch, A. D.; Rempel, M.
2011IAUS..273..379B    Altcode:
  Numerical computations of wave propagation through sunspot-like magnetic
  field structures are critical to developing and testing methods to
  deduce the subsurface structure of sunspots and active regions. We
  show that helioseismic analysis applied to the MHD sunspot simulations
  of Rempel and collaborators, as well as to translation-invariant
  models of umbral-like fields, yield wave travel-time measurements in
  qualitative agreement with those obtained in real sunspots. However,
  standard inversion methods applied to these data fail to reproduce the
  true wave-speed structure beneath the surface of the model. Inversion
  methods which incorporate direct effects of the magnetic field,
  including mode conversion, may be required.

---------------------------------------------------------
Title: Helioseismic probing of the subsurface structure of sunspots
Authors: Crouch, A. D.; Birch, A. C.; Braun, D. C.; Clack, C. T. M.
2011IAUS..273..384C    Altcode:
  We discuss recent progress in the helioseismic probing of the subsurface
  structure of solar magnetic regions. To simulate the interaction of
  helioseismic waves with magnetic fields and thermal perturbations we
  use a simple model that is translation invariant in the horizontal
  directions, has a realistic stratification in the vertical direction,
  and has physically consistent boundary conditions for the waves at
  the upper and lower boundaries of the computational domain. Using
  this model we generate synthetic helioseismic data and subsequently
  measure time-distance travel times. We evaluate a model for the
  wave-speed perturbation below sunspots that replaces the sound speed
  in a non-magnetic model by the fast-mode speed from a magnetic model;
  our results indicate that this approach is unlikely to be useful in
  modeling wave-speed perturbations in sunspots. We develop and test
  an inversion algorithm for inferring the sound-speed perturbation in
  magnetic regions. We show that this algorithm retrieves the correct
  sound-speed perturbation only when the sensitivity kernels employed
  account for the effects of the magnetic field on the waves and the
  subsurface structure.

---------------------------------------------------------
Title: Helioseismic Inversions For Magnetic Field And Sound-speed
    Perturbations
Authors: Clack, Christopher; Crouch, A. D.; Birch, A. C.; Braun, D. C.
2011SPD....42.1602C    Altcode: 2011BAAS..43S.1602C
  In local helioseismology, inversion methods that can separate magnetic
  and thermal perturbations are needed, especially for probing the
  subsurface structure of sunspots. We present a method for performing
  linear helioseismic inversions that can infer small-amplitude
  perturbations to both the magnetic field strength and the sound-speed
  profile in translation-invariant background models permeated by a 3
  kG vertical magnetic field, consistent with expectations for sunspot
  umbrae. We introduce a novel inversion routine that consists of
  two parts: first; a traditional regularized least squares inversion
  is utilized to search regularization-parameter space for inversion
  coefficients and second; an analysis of these inversion coefficients
  identifies the sets of coefficients that have the required attributes
  for a pair of inferred sound-speed and magnetic fields models. We show a
  case study in which this inversion method is able to accurately recover
  a sound-speed perturbation and a perturbation in the magnetic field
  strength simultaneously. We will discuss how these results relate to
  the local helioseismology of sunspots. This work is supported by NASA
  contracts NNH09CE41C and NNG07EI51C.

---------------------------------------------------------
Title: F-mode Seismology Of Solar Simulations
Authors: DeGrave, Kyle; Jackiewicz, J.; Braun, D.; Birch, A. C.;
   Research Associates, NorthWest
2011SPD....42.1613D    Altcode: 2011BAAS..43S.1613D
  Time-distance helioseismology using f-mode travel times is used to
  study near-surface regions of realistic numerical magnetohydrodynamic
  simulations. A fully-consistent inversion procedure is used to analyze
  the simulation flow field outside of a sunspot. This approach is carried
  out to validate the time-distance technique, as well as the sensitivity
  kernels and the inversion algorithm. This work is supported by NASA
  under the SDO Science Center project (contract NNH09CE41C) as well as
  well as a NASA EPSCoR award.

---------------------------------------------------------
Title: Local Helioseismology of Small-Scale Magnetic Elements
Authors: Crouch, Ashley D.; Braun, D. C.; Felipe, T.; Birch, A. C.;
   Duvall, T. L.
2011SPD....42.1604C    Altcode: 2011BAAS..43S.1604C
  We will discuss recent progress in the measurement and modeling of the
  interaction of helioseismic waves with small-scale magnetic elements. We
  will present measurements of the Hankel analysis phase shifts
  and absorption coefficients associated with an average small-scale
  magnetic element, measured using ensemble-averaging techniques. We
  will show results from theoretical calculations and the numerical
  simulations of wave interactions with thin magnetic flux tubes. We
  will compare the Hankel analysis measurements with the predictions
  from these theoretical models, and discuss how these results pertain
  to the local helioseismology of magnetic flux concentrations. This
  work is supported by NASA contract NNH09CE43C.

---------------------------------------------------------
Title: Towards Reliable Physics-based Helioseismic Inversions of
    Sunspot Structure
Authors: Braun, Douglas; Birch, A.; Crouch, A.; Clack, C.; Dombroski,
   D.; Rempel, M.; Duvall, T., Jr.
2011SPD....42.1603B    Altcode: 2011BAAS..43S.1603B
  Inversion methods capable of reliably probing the subsurface structure
  beneath regions of strong magnetic fields, such as sunspots,
  remain elusive. We will review progress of a SDO Science Center
  project, funded to (among other goals) develop and evaluate new
  methods for this problem. Progress to date has included extensive
  production of magneto-convective sunspot models for the testing and
  validation of existing methods, for which a 27 hour run of artificial
  photospheric Dopplergrams is available online to the community. We
  will also summarize progress on the use of magnetostatic models for
  the development and testing of novel inversion methods designed to
  distinguish between magnetic field and thermal perturbations. <P />This
  work is supported by NASA contracts NNH09CE41C and NNG07EI51C.

---------------------------------------------------------
Title: Local Helioseismology of Magnetoconvective Sunspot Simulations
    and the Reliability of Standard Inversion Methods
Authors: Braun, Douglas; Birch, A.; Rempel, M.; Duvall, T.; J.
2011SPD....42.1607B    Altcode: 2011BAAS..43S.1607B
  Controversy exists in the interpretation and modeling of helioseismic
  signals in and around magnetic regions like sunspots. We show the
  results of applying local helioseismic inversions to travel-time shift
  measurements from realistic magnetoconvective sunspot simulations. We
  compare travel-time maps made from several simulations, using
  different measurements (helioseismic holography and center-annulus
  time distance helioseismology), and made on real sunspots observed
  with the HMI instrument onboard the Solar Dynamics Observatory. We
  find remarkable similarities in the travel-time perturbations
  measured between: 1) simulations extending both 8 and 16 Mm deep,
  2) the methodology (holography or time-distance) applied, and 3)
  the simulated and real sunspots. The application of RLS inversions,
  using Born approximation kernels, to narrow frequency-band travel-time
  shifts from the simulations demonstrates that standard methods fail
  to reliably reproduce the true wave speed structure. These findings
  emphasize the need for new methods for inferring the subsurface
  structure of active regions. Artificial Dopplergrams from our
  simulations are available to the community at www.hao.ucar.edu under
  "Data" and "Sunspot Models." This work is supported by NASA under the
  SDO Science Center project (contract NNH09CE41C).

---------------------------------------------------------
Title: Newly Identified Properties of Surface Acoustic Power
Authors: Schunker, H.; Braun, D. C.
2011SoPh..268..349S    Altcode: 2010SoPh..tmp..146S; 2010SoPh..tmp...76S; 2009arXiv0911.3042S
  The cause of enhanced acoustic power surrounding active regions,
  known as the acoustic halo, is not as yet understood. We explore the
  properties of the enhanced acoustic power observed near disk center
  from 21 to 27 January 2002, including AR 9787. We find that i) there
  exists a strong correlation of the enhanced high-frequency power with
  magnetic-field inclination, with greater power in more horizontal
  fields, ii) the frequency of the maximum enhancement increases along
  with magnetic-field strength, and iii) the oscillations contributing
  to the halos show modal ridges that are shifted to higher wavenumber
  at constant frequency in comparison to the ridges of modes in the
  quiet Sun.

---------------------------------------------------------
Title: The Need for Physics-based Inversions of Sunspot Structure
    and Flows
Authors: Braun, D. C.; Birch, A. C.; Crouch, A. D.; Rempel, M.
2011JPhCS.271a2010B    Altcode:
  Current controversy exists in the interpretation and modeling
  of helioseismic signals in and around magnetic regions like
  sunspots. Unresolved issues include the dependence of the sign of
  both the inferred flows and wave speed on the type of filtering used,
  and the discrepancy between the relatively deep two-layer wave-speed
  models derived from standard time-distance methods and shallow, positive
  wave-speed models derived using forward models which include effects of
  mode conversion To make full use of the year-round, almost limb-to-limb,
  coverage provided by the Solar Dynamics Observatory, an efficient and
  reliable inversion method incorporating possible magnetic effects and
  the currently unexplained sensitivity to methodology is critical.

---------------------------------------------------------
Title: Properties of Near-surface Flows around Active Regions from
    Helioseismic Holography
Authors: Braun, D. C.; Wan, K.
2011JPhCS.271a2007B    Altcode:
  A variety of local-helioseismic analyses have shown ~50 m/s flows
  converging on active regions (ARs). We have examined the average
  properties of both the 75 strongest converging and 75 strongest
  diverging flows present in Carrington rotation CR1988 within the
  uppermost 3 Mm of the Sun. The flows, averaged over 5 days, were deduced
  from calibrated helioseismic holography measurements applied to MDI
  observations of CR1988. Inflows associated with ARs typically have
  maximum speed of between 20 and 60 m/s at about 3 heliocentric degrees
  from their centers and fall to zero by a radius of 7 degrees. Similar
  converging flows, however, are prevalent in the quiet Sun. Outflows
  of similar spatial extent, but signficantly larger speeds, are present
  diverging from sunspots (i.e. the moat flows). Many of the converging
  flows in ARs appear to simply mark the boundaries of the moats while
  others converge on plage regions. In general, large ARs containing
  sunspots contain a complex mixture of both inflows and outflows which,
  aside from sunspot moats, also appear similar in property to convective
  components of the quiet Sun.

---------------------------------------------------------
Title: Sunspot Seismology with the Solar Dynamics Observatory
    Helioseismic and Magnetic Imager
Authors: Braun, D. C.; Birch, A. C.; Crouch, A. D.; Clack, C.;
   Dombroski, D.; Rempel, M.
2010AGUFMSH14A..05B    Altcode:
  The Helioseismic and Magnetic Imager (HMI) onboard the Solar Dynamics
  Observatory (SDO) promises to yield detailed information about the
  subsurface dynamics and structure of solar active regions. A SDO Science
  Center was recently funded and initiated by NASA to (among other goals)
  enable the reliable measurements of subsurface flow, magnetic field,
  and sound speed in regions of strong magnetic fields. Using analyses
  of sunspots observed with HMI/SDO, we illustrate the challenges of
  this goal and suggest a plan for the development and implementation of
  new physics-based modeling of the subsurface structure of sunspots. Key
  components of this effort will be discussed, including numerical forward
  modeling of the wave propagation through model sunspots. These efforts
  incorporate both magnetostatic and magneto-convective models. This
  work is supported by the NASA SDO Science Center and Heliophysics GI
  programs through contracts NNH09CE41C and NNG07EI51C.

---------------------------------------------------------
Title: An Estimate of the Detectability of Rising Flux Tubes
Authors: Birch, A. C.; Braun, D. C.; Fan, Y.
2010ApJ...723L.190B    Altcode:
  The physics of the formation of magnetic active regions (ARs) is one
  of the most important problems in solar physics. One main class of
  theories suggests that ARs are the result of magnetic flux that rises
  from the tachocline. Time-distance helioseismology, which is based on
  measurements of wave propagation, promises to allow the study of the
  subsurface behavior of this magnetic flux. Here, we use a model for a
  buoyant magnetic flux concentration together with the ray approximation
  to show that the dominant effect on the wave propagation is expected
  to be from the roughly 100 m s<SUP>-1</SUP> retrograde flow associated
  with the rising flux. Using a B-spline-based method for carrying out
  inversions of wave travel times for flows in spherical geometry, we
  show that at 3 days before emergence the detection of this retrograde
  flow at a depth of 30 Mm should be possible with a signal-to-noise
  level of about 8 with a sample of 150 emerging ARs.

---------------------------------------------------------
Title: Modeling the Subsurface Structure of Sunspots
Authors: Moradi, H.; Baldner, C.; Birch, A. C.; Braun, D. C.; Cameron,
   R. H.; Duvall, T. L.; Gizon, L.; Haber, D.; Hanasoge, S. M.; Hindman,
   B. W.; Jackiewicz, J.; Khomenko, E.; Komm, R.; Rajaguru, P.; Rempel,
   M.; Roth, M.; Schlichenmaier, R.; Schunker, H.; Spruit, H. C.;
   Strassmeier, K. G.; Thompson, M. J.; Zharkov, S.
2010SoPh..267....1M    Altcode: 2009arXiv0912.4982M; 2010SoPh..tmp..171M
  While sunspots are easily observed at the solar surface, determining
  their subsurface structure is not trivial. There are two main
  hypotheses for the subsurface structure of sunspots: the monolithic
  model and the cluster model. Local helioseismology is the only means
  by which we can investigate subphotospheric structure. However, as
  current linear inversion techniques do not yet allow helioseismology to
  probe the internal structure with sufficient confidence to distinguish
  between the monolith and cluster models, the development of physically
  realistic sunspot models are a priority for helioseismologists. This
  is because they are not only important indicators of the variety of
  physical effects that may influence helioseismic inferences in active
  regions, but they also enable detailed assessments of the validity of
  helioseismic interpretations through numerical forward modeling. In
  this article, we provide a critical review of the existing sunspot
  models and an overview of numerical methods employed to model wave
  propagation through model sunspots. We then carry out a helioseismic
  analysis of the sunspot in Active Region 9787 and address the serious
  inconsistencies uncovered by Gizon et al. (2009a, 2009b). We find that
  this sunspot is most probably associated with a shallow, positive
  wave-speed perturbation (unlike the traditional two-layer model)
  and that travel-time measurements are consistent with a horizontal
  outflow in the surrounding moat.

---------------------------------------------------------
Title: Erratum: Erratum to: Helioseismology of Sunspots: A Case
    Study of NOAA Region 9787
Authors: Gizon, L.; Schunker, H.; Baldner, C. S.; Basu, S.; Birch,
   A. C.; Bogart, R. S.; Braun, D. C.; Cameron, R.; Duvall, T. L.;
   Hanasoge, S. M.; Jackiewicz, J.; Roth, M.; Stahn, T.; Thompson, M. J.;
   Zharkov, S.
2010SSRv..156..257G    Altcode: 2010SSRv..tmp...99G
  No abstract at ADS

---------------------------------------------------------
Title: Modeling the Sensitivity of Helioseismic Measurements to
    Magnetic Fields and Thermal Perturbations
Authors: Crouch, Ashley D.; Birch, A.; Braun, D.
2010AAS...21631906C    Altcode: 2010BAAS...41Q.910C
  We will discuss recent progress in modeling the interaction of
  helioseismic waves with magnetic fields and thermal perturbations. We
  employ a background model that is translation-invariant in the
  horizontal directions, has a realistic stratification in the vertical
  direction, and includes uniform, inclined magnetic fields. Physically
  consistent boundary conditions for the waves are implemented at the
  upper and lower boundaries of the model. Using this model we generate
  synthetic data and subsequently measure time-distance travel times. We
  will show the sensitivity of these travel times to magnetic fields and
  changes in sound speed. We will show the effect of magnetic fields on
  inversions for wave speed. We will discuss how these results relate
  to the local heliseismology of sunspots. This work is supported by
  NASA contracts NNH09CE41C and NNG07EI51C.

---------------------------------------------------------
Title: Developing Physics-Based Procedures for Local Helioseismic
    Probing of Sunspots and Magnetic Regions
Authors: Birch, Aaron; Braun, D. C.; Crouch, A.; Rempel, M.; Fan,
   Y.; Centeno, R.; Toomre, J.; Haber, D.; Hindman, B.; Featherstone,
   N.; Duvall, T., Jr.; Jackiewicz, J.; Thompson, M.; Stein, R.; Gizon,
   L.; Cameron, R.; Saidi, Y.; Hanasoge, S.; Burston, R.; Schunker, H.;
   Moradi, H.
2010AAS...21630805B    Altcode:
  We have initiated a project to test and improve the local helioseismic
  techniques of time-distance and ring-diagram analysis. Our goals are
  to develop and implement physics-based methods that will (1) enable the
  reliable determinations of subsurface flow, magnetic field, and thermal
  structure in regions of strong magnetic fields and (2) be quantitatively
  tested with realistic solar magnetoconvection simulations in the
  presence of sunspot-like magnetic fields. We are proceeding through a
  combination of improvements in local helioseismic measurements, forward
  modeling of the helioseismic wavefield, kernel computations, inversions,
  and validation through numerical simulations. As improvements over
  existing techniques are made they will be applied to the SDO/HMI
  observations. This work is funded through the the NASA Heliophysics
  Science Division through the Solar Dynamics Observatory (SDO) Science
  Center program.

---------------------------------------------------------
Title: Tests of Helioseismic Holography Sound-Speed Inversions Using
    Synthetic Data
Authors: Birch, Aaron; Braun, D.; Crouch, A.; Parchevsky, K.;
   Kosovichev, A.
2010AAS...21640006B    Altcode: 2010BAAS...41..855B
  Helioseismic holography is an important method for measuring physical
  conditions in the solar interior. Synthetic data is a powerful tool
  for validating the methods of local helioseismology. Here we show
  some example inversions of surface-focusing holography measurements of
  synthetic data sets. We show that Born-approximation based inversions
  of phase-speed and ridge-filtered measurements yield models that
  are consistent with the true sound-speed structure in some simple
  test cases. This work is supported by NASA contracts NNH09CE41C and
  NNG07EI51C.

---------------------------------------------------------
Title: How Much Data Do We Need to Detect the Deep Solar Meridional
    Circulation?
Authors: Braun, D. C.; Birch, A. C.
2009ASPC..416..131B    Altcode:
  We assess the noise in p-mode travel-time shifts which would
  form the basis of inferences of large-scale flows throughout the
  solar convection zone. We derive the expected travel times from a
  parameterized return flow component of the meridional circulation. We
  show that a helioseismic detection of the return component may not be
  possible using data spanning an interval less than a solar cycle.

---------------------------------------------------------
Title: The Internal Dynamics and Magnetism of the Sun -- the
    Perspective from Local Helioseismology (Invited)
Authors: Braun, D. C.
2009AGUFMSH11B..03B    Altcode:
  The application of innovative local helioseismic methods to solar
  observations made with GONG, MDI, and other instruments over the past
  two decades has shed light on dynamical and magnetic processes in the
  solar interior. The community now stands poised for the onslaught
  of new data of unprecedented quality and quantity from the SDO
  mission. However, we are already substantially benefiting from the
  appearance of sophisticated numerical analyses and artificial data
  products. I will touch upon three problems in local helioseismology
  which are subject to substantive renewed efforts: the deep meridional
  circulation, the detection of magnetic flux prior to its appearance
  at the photosphere, and the subsurface nature of sunspots. All three
  problems pose major challenges, but there is considerable hope for
  breakthroughs within the next few years. DCB acknowledges support
  from NSF grant AST-0406225; NASA contracts NNH09CE41C, NNG07EI51C,
  and NNH07CD25C; and a subcontract from the NASA sponsored HMI project
  at Stanford University.

---------------------------------------------------------
Title: Numerical sunspot models - subsurface structure and
    helioseismic forward modeling (Invited)
Authors: Rempel, M.; Birch, A. C.; Braun, D. C.
2009AGUFMSH11B..02R    Altcode:
  The magnetic and thermal subsurface structure of sunspots has been
  debated for decades. While local helioseismic inversions allow in
  principle to constrain the subsurface structure of sunspots, a full
  inversion is still not possible due to the complicated interaction
  between waves and magnetic field. As an alternative it is possible to
  address this problem through forward modeling. Over the past few years
  numerical MHD models of entire sunspots including radiative transfer and
  a realistic equation of state have become possible. These simulations
  include p-modes excited by convection and the full interaction of these
  modes with the magnetic and thermal structure of the sunspot. In this
  talk I will present recent progress in MHD modeling of sunspots with
  special emphasis on the thermal and magnetic structure of numerical
  sunspot models. It turns out that modeled sunspots so far impose
  rather shallow perturbations to sound and fast mode speeds in the
  upper most 2 Mm. Nevertheless the seismic signatures are very similar
  to observed sunspots.

---------------------------------------------------------
Title: Improving the Prediction Capability of Seismic Far-Side Maps
Authors: González Hernández, I.; Scherrer, P.; Hill, F.; Lindsey,
   C.; Braun, D.
2009ASPC..416...87G    Altcode:
  Both the Michelson Doppler Imager (MDI) and the Global Oscillation
  Network Group (GONG) projects produce daily seismic maps of surface
  magnetic activity on the non-visible hemisphere of the Sun. The
  technique has proven useful to detect and follow large active regions
  before they appear to face the Earth. This work demonstrates an
  improvement in the detection capability of the technique by applying
  the results of new research. We calibrate the daily far-side maps in
  terms of characteristics of the active region, such as total area and
  magnetic flux strength, apply a relationship between the strength of
  the persistent signal and the success rate to automatically highlight
  possible candidates, and remove solar-cycle variations to stabilize
  the signal.

---------------------------------------------------------
Title: Absorption of p Modes by Magnetic Plage
Authors: Jain, R.; Hindman, B. W.; Braun, D. C.; Birch, A. C.
2009ASPC..416...55J    Altcode:
  The Sun's magnetic active regions, composed of sunspots and plage,
  are topologically complex. The magnetic field is highly structured,
  forming a tangle of fibrils within the plage and more compact,
  regimented bundles within sunspot umbrae. The fragmented nature
  of the field makes helioseismic observations within active regions
  rather difficult to interpret. We choose to study the propagation of
  acoustic waves through regions of plage, modeling the magnetic field
  therein as a collection of thin flux tubes. In this paper, we present
  the first results of this research; the computation of the absorption
  coefficient from an ensemble of many flux tubes. The incoming acoustic
  waves interact with the magnetic flux tube, exciting sausage and kink
  tube waves which propagate downward and upward carrying away energy,
  thereby producing absorption. We calculate the resulting theoretical
  absorption coefficients and compare with the most recent observations.

---------------------------------------------------------
Title: Detecting, Selecting, And Controlling For Emerging
    ActiveRegions In The Search For Helioseismic Pre-emergence Signatures.
Authors: Leka, K. D.; Dunn, T.; Gonzalez-Hernandez, I.; Barnes, G.;
   Braun, D.; Birch, A.
2009SPD....40.0708L    Altcode:
  Helioseismology is potentially capable of predicting the emergence of
  solaractive regions. As part of a search for statistically significant
  helioseismic predictors of active region emergence, we have developed
  methods for the automatic determination of emergence times based on the
  NOAA/NGDC active region catalog and MDI/SOHO 96 minute magnetograms. We
  demonstrate the application of this method and its sister task of
  selecting an appropriate control sample. We show first results from
  a statistical study investigating the pre-emergence signatures of
  Solar Active Regions using GONG data. This work was supported by NASA
  contract NNH07CD25C.

---------------------------------------------------------
Title: A Search for Pre-Emergence Signatures of Active Regions
Authors: Birch, Aaron; Braun, D. C.; Leka, K. D.; Barnes, G.; Dunn,
   T. L.; González Hernández, I.
2009SPD....40.0402B    Altcode:
  Prediction of solar active region emergence is an important goal
  for helioseismology. As a first step towards developing prediction
  methods, we are carrying out a search for helioseismic pre-emergence
  signatures. Using GONG data, we have applied helioseismic holography
  to about 150 pre-emergence active regions and a control sample of 450
  quiet-Sun regions. We will show preliminary results of this study. <P
  />This work was supported by NASA contract NNH07CD25C

---------------------------------------------------------
Title: Helioseismology of a Realistic MHD Sunspot Simulation
Authors: Braun, Douglas; Birch, A. C.; Rempel, M.
2009SPD....40.0303B    Altcode:
  We have recently measured travel times and absorption of p modes
  propagating through a realistic numerical model of solar convection in
  the presence of a sunspot-like structure. Both the mean travel-time
  perturbations and the absorption in the simulation are remarkably
  similar to those observed in typical sunspots. Therefore, simulations
  of this type provide both the means to understand the physics behind
  the helioseismic observations and the opportunity to validate existing
  and future models of the subsurface structure of sunspots. We will
  compare helioseismic measurements made with the simulation with
  those of a typical sunspot observed with MDI. We will discuss the
  implications of these comparisons for structural inversions of sunspots
  and understanding the role of MHD mode conversion in interpreting
  helioseismic observations. This work is supported by NASA contracts
  NNH09CE41C and NNG07EI51C.

---------------------------------------------------------
Title: Statistical Analysis of the Success Rate of the Far-Side
    Seismic Mapping of Active Regions.
Authors: Gonzalez-Hernandez, Irene; Scherrer, P.; Lindsey, C.; Hill,
   F.; Braun, D.
2009SPD....40.0707G    Altcode:
  Seismic maps of the non-visible side of the Sun (far side) have been
  used for almost a decade to follow large active regions before they
  rotate to face the Earth. Preliminary efforts to quantify the success
  rate of the used technique (seismic holography) have been published
  with limited data. However, a thorough study is needed to further
  understand the limitations of the technique in terms of size and
  strength of the active regions detected and to reveal clues as to how
  to improve it. <P />We have analyzed three complete years of far-side
  seismic maps calculated using both Global Oscillation Newtwork group
  (GONG) and Michelson Doppler Imager (MDI) data and matched the far-side
  candidates with associated active regions as recorded by the NOAA
  database. Here we present the results.

---------------------------------------------------------
Title: Helioseismic Inversions applied to a Realistic MHD Sunspot
    Simulation
Authors: Birch, Aaron; Braun, D. C.; Rempel, M.
2009SPD....40.0713B    Altcode:
  Local helioseismology applied to the realistic magneto-convection
  sunspot simulations of Rempel et al. produces solar-like wave travel
  times. We apply standard ray-theory based inversions to infer subsurface
  wave speed from these travel times. We find that the inferred wave-speed
  perturbations are similar to the wave-speed perturbations found from
  the analysis of typical sunspots observed with MDI. We show, however,
  that the ray theory inversions fail to retrieve the true time-averaged
  sound speed or fast-mode speed from the simulations. We propose some
  alternative strategies for inferring the subsurface structure of
  sunspots. <P />This work is supported by NASA contracts NNH09CE41C
  and NNG07EI51C.

---------------------------------------------------------
Title: Helioseismology of Sunspots: A Case Study of NOAA Region 9787
Authors: Gizon, L.; Schunker, H.; Baldner, C. S.; Basu, S.; Birch,
   A. C.; Bogart, R. S.; Braun, D. C.; Cameron, R.; Duvall, T. L.;
   Hanasoge, S. M.; Jackiewicz, J.; Roth, M.; Stahn, T.; Thompson, M. J.;
   Zharkov, S.
2009SSRv..144..249G    Altcode: 2008SSRv..tmp..188G; 2010arXiv1002.2369G
  Various methods of helioseismology are used to study the subsurface
  properties of the sunspot in NOAA Active Region 9787. This sunspot
  was chosen because it is axisymmetric, shows little evolution during
  20-28 January 2002, and was observed continuously by the MDI/SOHO
  instrument. AR 9787 is visible on helioseismic maps of the farside
  of the Sun from 15 January, i.e. days before it crossed the East
  limb. Oscillations have reduced amplitudes in the sunspot at all
  frequencies, whereas a region of enhanced acoustic power above 5.5 mHz
  (above the quiet-Sun acoustic cutoff) is seen outside the sunspot and
  the plage region. This enhanced acoustic power has been suggested to
  be caused by the conversion of acoustic waves into magneto-acoustic
  waves that are refracted back into the interior and re-emerge as
  acoustic waves in the quiet Sun. Observations show that the sunspot
  absorbs a significant fraction of the incoming p and f modes around 3
  mHz. A numerical simulation of MHD wave propagation through a simple
  model of AR 9787 confirmed that wave absorption is likely to be due
  to the partial conversion of incoming waves into magneto-acoustic
  waves that propagate down the sunspot. Wave travel times and mode
  frequencies are affected by the sunspot. In most cases, wave packets
  that propagate through the sunspot have reduced travel times. At
  short travel distances, however, the sign of the travel-time shifts
  appears to depend sensitively on how the data are processed and,
  in particular, on filtering in frequency-wavenumber space. We carry
  out two linear inversions for wave speed: one using travel-times
  and phase-speed filters and the other one using mode frequencies
  from ring analysis. These two inversions give subsurface wave-speed
  profiles with opposite signs and different amplitudes. The travel-time
  measurements also imply different subsurface flow patterns in the
  surface layer depending on the filtering procedure that is used. Current
  sensitivity kernels are unable to reconcile these measurements, perhaps
  because they rely on imperfect models of the power spectrum of solar
  oscillations. We present a linear inversion for flows of ridge-filtered
  travel times. This inversion shows a horizontal outflow in the upper
  4 Mm that is consistent with the moat flow deduced from the surface
  motion of moving magnetic features. From this study of AR 9787, we
  conclude that we are currently unable to provide a unified description
  of the subsurface structure and dynamics of the sunspot.

---------------------------------------------------------
Title: Surface-Focused Seismic Holography of Sunspots:
    II. Expectations from Numerical Simulations Using Sound-Speed
    Perturbations
Authors: Birch, A. C.; Braun, D. C.; Hanasoge, S. M.; Cameron, R.
2009SoPh..254...17B    Altcode: 2008SoPh..tmp..186B
  Helioseismic observations of sunspots show that wave travel times, at
  fixed horizontal phase speed, depend on the temporal frequency of the
  waves employed in the data analysis. This frequency variation has been
  suggested to be consistent with near-surface (vertical length scales
  of order one Mm or smaller) changes in wave propagation properties
  relative to the quiet Sun. We investigate this suggestion by employing
  numerical simulations of acoustic-wave propagation through models
  with horizontally and vertically inhomogeneous structure. Standard
  methods of surface-focused helioseismic holography are applied to the
  resulting simulated wave fields. We find that the travel-time shifts
  measured using holography from the simulations with deep sound-speed
  perturbations (relative to a plane-parallel quiet-Sun model) do not
  show a systematic frequency dependence at phase speeds above about
  20 km s<SUP>−1</SUP>. However, shallow sound-speed perturbations,
  similar to those proposed to model the acoustic scattering properties
  of sunspots observed with Hankel analysis, produce systematic frequency
  dependence at these phase speeds. In both cases, positive travel-time
  shifts can be caused by positive sound-speed perturbations. The details
  of the travel-time shifts are, however, model dependent.

---------------------------------------------------------
Title: Magnetic flux emergence on the Sun and Sun-like stars
Authors: Rempel, Matthias; Fan, Yuhong; Birch, Aaron; Braun, Douglas
2009astro2010S..74R    Altcode: 2009astro2010S..74F
  No abstract at ADS

---------------------------------------------------------
Title: Helioseismology of Sunspots: A Case Study of NOAA Region 9787
Authors: Gizon, L.; Schunker, H.; Baldner, C. S.; Basu, S.; Birch,
   A. C.; Bogart, R. S.; Braun, D. C.; Cameron, R.; Duvall, T. L.;
   Hanasoge, S. M.; Jackiewicz, J.; Roth, M.; Stahn, T.; Thompson, M. J.;
   Zharkov, S.
2009odsm.book..249G    Altcode:
  Various methods of helioseismology are used to study the subsurface
  properties of the sunspot in NOAA Active Region 9787. This sunspot
  was chosen because it is axisymmetric, shows little evolution during
  20-28 January 2002, and was observed continuously by the MDI/SOHO
  instrument. AR 9787 is visible on helioseismic maps of the farside of
  the Sun from 15 January, i.e. days before it crossed the East limb.

---------------------------------------------------------
Title: Prospects for the Detection of the Deep Solar Meridional
    Circulation
Authors: Braun, Douglas; Birch, A. C.
2009AAS...21349202B    Altcode: 2009BAAS...41..471B
  We perform helioseismic holography to assess the noise in p-mode
  travel-time shifts which would form the basis of inferences of
  large-scale flows throughout the solar convection zone. We also
  derive the expected travel times from a parameterized return
  (equatorward) flow component of the meridional circulation at the
  base of the convection zone from forward models under the assumption
  of the Born approximation. From estimations of the signal-to-noise
  ratio for measurements focused near the base of the convection zone,
  we conclude that the helioseismic detection of the deep meridional
  flow including the return component may not be possible using data
  spanning an interval less than a solar cycle.

---------------------------------------------------------
Title: Prospects for the Detection of the Deep Solar Meridional
    Circulation
Authors: Braun, D. C.; Birch, A. C.
2008ApJ...689L.161B    Altcode: 2008arXiv0810.0284B
  We perform helioseismic holography to assess the noise in p-mode
  travel-time shifts which would form the basis of inferences of
  large-scale flows throughout the solar convection zone. We also derive
  the expected travel times from a parameterized return (equatorward)
  flow component of the meridional circulation at the base of the
  convection zone from forward models under the assumptions of the ray
  and Born approximations. From estimates of the signal-to-noise ratio
  for measurements focused near the base of the convection zone, we
  conclude that the helioseismic detection of the deep meridional flow
  including the return component may not be possible using travel-time
  measurements spanning an interval less than a solar cycle. We speculate
  that this conclusion may be generally true for other helioseismic
  methods under the assumption that the underlying measurements are
  equivalently limited by solar realization noise.

---------------------------------------------------------
Title: Physical Properties of Wave Motion in Inclined Magnetic Fields
    within Sunspot Penumbrae
Authors: Schunker, H.; Braun, D. C.; Lindsey, C.; Cally, P. S.
2008SoPh..251..341S    Altcode: 2008arXiv0801.4448S; 2008SoPh..tmp...41S
  At the surface of the Sun, acoustic waves appear to be affected by the
  presence of strong magnetic fields in active regions. We explore the
  possibility that the inclined magnetic field in sunspot penumbrae may
  convert primarily vertically-propagating acoustic waves into elliptical
  motion. We use helioseismic holography to measure the modulus and phase
  of the correlation between incoming acoustic waves and the local surface
  motion within two sunspots. These correlations are modeled by assuming
  the surface motion to be elliptical, and we explore the properties
  of the elliptical motion on the magnetic-field inclination. We also
  demonstrate that the phase shift of the outward-propagating waves is
  opposite to the phase shift of the inward-propagating waves in stronger,
  more vertical fields, but similar to the inward phase shifts in weaker,
  more-inclined fields.

---------------------------------------------------------
Title: Surface-Focused Seismic Holography of Sunspots: I. Observations
Authors: Braun, D. C.; Birch, A. C.
2008SoPh..251..267B    Altcode: 2008arXiv0802.2652B; 2008SoPh..tmp...46B
  We present a comprehensive set of observations of the interaction
  of p-mode oscillations with sunspots using surface-focused seismic
  holography. Maps of travel-time shifts, relative to quiet-Sun travel
  times, are shown for incoming and outgoing p modes as well as their
  mean and difference. We compare results using phase-speed filters
  with results obtained with filters that isolate single p-mode ridges,
  and we further divide the data into multiple temporal frequency
  bandpasses. The f mode is removed from the data. The variations of the
  resulting travel-time shifts with magnetic-field strength and with the
  filter parameters are explored. We find that spatial averages of these
  shifts within sunspot umbrae, penumbrae, and surrounding plage often
  show strong frequency variations at fixed phase speed. In addition, we
  find that positive values of the mean and difference travel-time shifts
  appear exclusively in waves observed with phase-speed filters that
  are dominated by power in the low-frequency wing of the p<SUB>1</SUB>
  ridge. We assess the ratio of incoming to outgoing p-mode power using
  the ridge filters and compare surface-focused holography measurements
  with the results of earlier published p-mode scattering measurements
  using Fourier - Hankel decomposition.

---------------------------------------------------------
Title: Combining far-side maps from MDI and GONG to improve the
    prediction capability
Authors: Gonzalez Hernandez, I.; Scherrer, P.; Lindsey, C.; Braun,
   D.; Hill, F.
2008AGUSMSP41A..04G    Altcode:
  Both the Michaelson Doppler Imager (MDI) and the Global Oscillation
  Network Group (GONG) projects produce daily seismic maps of surface
  magnetic activity at the non-visible hemisphere the Sun. The technique
  has proven useful in order to detect and follow large active regions
  before they appear to face the Earth. This work explores the possibility
  of improving the detection capability of the technique by combining
  the results from both instruments. The research should lead to a better
  understanding of the spurious, non persistent seismic signal associated
  with the far-side images and better discrimination between solar and
  instrumental noise.

---------------------------------------------------------
Title: Helioseismic Holography of Simulated Solar Convection and
    Prospects for the Detection of Small-Scale Subsurface Flows
Authors: Braun, D. C.; Birch, A. C.; Benson, D.; Stein, R. F.;
   Nordlund, Å.
2007ApJ...669.1395B    Altcode: 2007arXiv0708.0214B
  We perform helioseismic holography on realistic solar convection
  simulations and compare the observed travel-time perturbations
  with the expected travel times from the horizontal flows in the
  simulations computed from forward models under the assumption of
  the Born approximation. We demonstrate reasonable agreement between
  the observed and model travel times, which reinforces the validity
  of helioseismic holography in the detection of subsurface horizontal
  flows. An assessment is made of the uncertainty of the measured p-mode
  travel times from the rms of the residuals. From the variation of the
  signal-to-noise ratio with depth we conclude that the helioseismic
  detection of individual flow structures with spatial scales of
  supergranulation or smaller is not possible for depths below about 5 Mm
  below the surface over timescales of less than a day. The travel-time
  noise estimated from these simulations appears to be similar to noise
  in measurements made using solar observations. We therefore suggest
  that similar limitations exist regarding the detection of analogous
  subsurface flows in the Sun. A study of the depth dependence of
  the contribution to the travel-time perturbations for focus depths
  between 3 and 7 Mm is made, showing that approximately half of the
  observed signal originates within the first 2 Mm below the surface. A
  consequence of this is a rapid decrease (and reversal in some cases)
  of the travel-time perturbations with depth due to the contribution to
  the measurements of oppositely directed surface flows in neighboring
  convective cells. This confirms an earlier interpretation of similar
  effects reported from observations of supergranulation.

---------------------------------------------------------
Title: Helioseismic Holography of Simulated Solar Convection and
    Prospects for the Detection of Small-Scale Subsurface Flows
Authors: Braun, Douglas; Birch, A. C.; Benson, D.; Stein, R. F.;
   Nordlund, A.
2007AAS...210.2201B    Altcode: 2007BAAS...39..124B
  We perform helioseismic holography on the solar convection simulations
  of Benson, Stein, and Nordlund and compare the observed acoustic
  travel-time perturbations with the expected travel times from the
  horizontal flows in the simulations computed from forward models under
  the assumption of the Born approximation. The agreement between the
  observed and model travel times reinforces the validity of helioseismic
  holography in the detection of subsurface horizontal flows. However,
  from the variation of the signal-to-noise ratio with depth, we conclude
  that the local helioseismic detection of individual supergranule-size
  (or smaller) flow patterns is not possible for depths below about
  5 Mm below the surface over time scales less than a day. We suggest
  that similar limitations exist regarding the detection of analogous
  subsurface flows in the Sun. We also study the depth dependence of
  the contribution to the travel-time perturbations for the simulated
  flows. For holography measurements focused down to 7 Mm, we find
  that approximately half of the observed signal originates within
  the first 2 Mm below the surface. A consequence of this is a a rapid
  decrease (and possible reversal) of the travel-time perturbations with
  increasing focus depth due to the contribution to the measurements of
  oppositely directed surface flows in neighboring convective cells. This
  confirms an earlier interpretation of similar effects reported from
  holographic analyses of observations of supergranulation. <P />This
  work is supported by NASA contracts NNH05CC76C and NNH04CC05C, NSF
  grant AST-0406225 , and a subcontract through the HMI project at
  Stanford University awarded to NWRA, and by NASA grant NNG04GB92G and
  NSF grant AST-0605738 to MSU.

---------------------------------------------------------
Title: Sunspot Seismology: Testing Surface Effects with Numerical
    Simulations
Authors: Braun, Douglas; Birch, A. C.; Hanasoge, S. M.
2007AAS...210.2206B    Altcode: 2007BAAS...39..125B
  The discovery that sunspots absorb acoustic waves was first announced
  twenty years ago at a previous SPD meeting in Honolulu. A considerable
  effort has been made to understand the physics of the interaction
  between acoustic waves and sunspots. However, the implications of this
  two-decade old discovery are still being explored in helioseismology. An
  ongoing controversy involves the role of surface effects, including
  absorption, in modeling the subsurface structure of sunspots. Braun
  and Birch recently suggested that observed frequency variations,
  at fixed phase speeds, of acoustic travel-time perturbations through
  sunspots offers evidence for a strong contribution to travel times
  from structures with vertical scales smaller than about one Mm
  near the solar surface. We test this suggestion with the numerical
  simulations of acoustic-wave propagation hrough specified sound-speed
  perturbations of a background solar model. An important finding is that
  travel times measured using helioseismic holography from simulations
  employing sound-speed perturbations typical of recent time-distance
  inversions do not predict the strong frequency variations observed in
  with solar data. We are in the process of evaluating whether shallow
  sound-speed perturbations, such as that proposed by Fan, Braun and
  Chou to explain the acoustic scattering propertis of sunspots observed
  with Hankel analysis, can reproduce the frequency variations observed
  in sunspots. <P />This work is supported by contracts NAS5-02139,
  NNH05CC76C and NNH04CC05C from NASA, and grant AST-0406225 from the NSF.

---------------------------------------------------------
Title: Surface magnetic field effects in local helioseismology
Authors: Schunker, H.; Braun, D. C.; Cally, P. S.
2007AN....328..292S    Altcode: 2010arXiv1002.2379S
  Using helioseismic holography strong evidence is presented that
  the phase (or equivalent travel-time) of helioseismic signatures in
  Dopplergrams within sunspots depend upon the line-of-sight angle in
  the plane containing the magnetic field and vertical directions. This
  is shown for the velocity signal in the penumbrae of two sunspots
  at 3, 4 and 5 mHz. Phase-sensitive holography demonstrates that they
  are significantly affected in a strong, moderately inclined magnetic
  field. This research indicates that the effects of the surface magnetic
  field are potentially very significant for local helioseismic analysis
  of active regions.

---------------------------------------------------------
Title: The Role of MHD Mode Conversion in Sunspot Seismology
Authors: Crouch, A. P.; Cally, P. S.; Charbonneau, P.; Braun, D. C.;
   Desjardins, M.
2006ASPC..354..161C    Altcode:
  Sunspots absorb energy from and shift the phase of f and p modes
  incident upon them. Understanding the mechanism causing each of these
  effects is vital to the local helioseismology of sunspots (and magnetic
  flux concentrations in general). Because the beta-equals-unity layer
  typically lies in the near surface layers below the photospheres
  of sunspot umbrae, MHD mode conversion can occur. Mode conversion
  provides a promising absorption mechanism because the slow
  magnetoacoustic-gravity waves and Alfvén waves guide energy along
  the magnetic field away from the acoustic cavity. Our previous mode
  conversion calculations have shown that simple sunspot models with
  non-vertical magnetic fields can produce ample absorption to explain the
  Hankel analysis measurements, along with phase shift predictions that
  agree well with the observations. Those calculations only considered
  the possibility of MHD waves propagating down the magnetic field into
  the interior. In this contribution, we consider a second additional
  possibility -- waves propagating up into the atmosphere overlying
  sunspots.

---------------------------------------------------------
Title: Behaviour of Acoustic Waves in Sunspots
Authors: Schunker, H.; Braun, D. C.; Cally, P. S.; Lindsey, C.
2006ASPC..354..244S    Altcode:
  Because helioseismology uses surface signals to calculate subsurface
  characteristics the behaviour of surface acoustic oscillations in
  sunspots is important in interpreting helioseismic results. SOHO-MDI
  Doppler velocity analysis of AR9026 and AR9033 at 3, 4, and 5 mHz,
  using helioseismic holography, show that the amplitude and the phase
  in the correlation of the acoustic ingression with the observed surface
  velocity are found to be sensitive to the relative line-of-sight angle
  in the penumbra of both sunspots. This is consistent with a conversion
  of vertically propagating acoustic waves into magneto-acoustic waves
  with motion described by ellipses.

---------------------------------------------------------
Title: Farside helioseismic holography: recent advances
Authors: González Hernández, I.; Hill, F.; Lindsey, C.; Braun, D.;
   Scherrer, P.; Hanasoge, S. M.
2006ESASP.624E...3G    Altcode: 2006soho...18E...3G
  No abstract at ADS

---------------------------------------------------------
Title: The interaction between acoustic waves and inclined magnetic
    fields near the β~1 layer
Authors: Schunker, H.; Braun, D. C.; Cally, P. S.; Lindsey, C.
2006IAUJD..17E..16S    Altcode:
  The acoustic showerglass effect may be hindering our helioseismic
  renditions of the solar subsurface. We present the results of near
  -surface wave conversion of acoustic waves in a model polytropic
  atmosphere by a uniform, inclined magnetic field. The upcoming fast,
  acoustic wave undergoes conversion to a slow, magnetic wave at the β
  ~ 1 layer where the sound speed and Alfven speed are comparable. The
  conversion is dependent upon the " attack angle" between the ray path
  and the magnetic field. The angle of the wave vectors at the polytropic
  " surface" is compared to observations of surface velocity vectors in
  sunspot penumbrae. AR9026 and AR9057 both have well- defined, static
  penumbrae and their Doppler velocities are viewed from different
  angles by SOHO-MDI as they cross the solar disk. The phase of the
  correlation between the ingression and surface velocity, determined by
  helioseismic holography, is used to assess the effect the penumbral
  magnetic field has on incoming acoustic waves. The phase is found to
  be dependent upon the line-of-sight of observation indicating that
  this is a surface phenomenon, which could otherwise be interpreted as
  subsurface travel-time perturbations of up to one minute. Furthermore,
  using vector magnetograms from the IVM at the Mees Observatory, the
  phase of the correlation is found to be dependent on the magnetic
  field tilt from vertical, and the dependence is consistent across the
  two sunspots. Comparing the results from the polytropic model with the
  observations show strong support for the near-surface wave conversion
  theory, although many questions still remain.

---------------------------------------------------------
Title: Observed Frequency Variations of Solar p-Mode Travel Times
    as Evidence for Surface Effects in Sunspot Seismology
Authors: Braun, D. C.; Birch, A. C.
2006ApJ...647L.187B    Altcode:
  Using helioseismic holography, we measure acoustic (p-mode) travel-time
  perturbations, observed within solar active regions, as functions of
  frequency and phase speed. We find evidence for a frequency variation,
  at fixed phase speed, of the travel times that has not previously been
  reported. This variation is not expected from typical sound-speed models
  of sunspots, which result from the inversion of travel times and may
  indicate a significant contribution to the travel times from structures
  with vertical scales smaller than about 1 Mm near the solar surface.

---------------------------------------------------------
Title: Farside Helioseismic Holography: Recent Advances
Authors: Gonzalez-Hernandez, Irene; Braun, D. C.; Hanasoge, S. M.;
   Hill, F.; Lindsey, C. A.; Scherrer, P. H.
2006SPD....37.0502G    Altcode: 2006BAAS...38Q.223G
  Both MDI and GONG have been calculating partial farside maps for some
  time, showing a high degree of agreement in detecting large active
  regions within approximately 45 degrees around the antipode of disk
  center.Recently, the full-hemisphere capability has been added to the
  farside pipelines of both instruments. We show here the capability of
  detecting large active regions and tracking them through out the full
  farside hemisphere by applying the technique to active region 10808.We
  also report on efforts underway to calibrate the farside signal in
  terms of equivalent magnetic field, including some preliminary maps
  obtained from artificial helioseismic data.

---------------------------------------------------------
Title: Genetic magnetohelioseismology with Hankel analysis data
Authors: Crouch, A. D.; Cally, P. S.; Charbonneau, P.; Braun, D. C.;
   Desjardins, M.
2005MNRAS.363.1188C    Altcode: 2005MNRAS.tmp..856C
  Hankel analysis determined that sunspots absorb energy from and
  shift the phase of f- and p-modes incident upon them. One promising
  mechanism that can explain the absorption is partial conversion
  to slow magnetoacoustic-gravity (MAG) waves and Alfvén waves,
  which guide energy along the magnetic field away from the acoustic
  cavity. Our recent mode conversion calculations demonstrated that
  simple sunspot models, which roughly account for the radial variation
  of the magnetic field strength and inclination, can produce ample
  absorption to explain the observations, along with phase shifts that
  agree remarkably well with the Hankel analysis data. In this paper,
  we follow the same approach, but adopt a more realistic model for the
  solar convection zone that includes the thermal perturbation associated
  with a sunspot's magnetic field. Consistent with our earlier findings,
  we show that a moderately inclined, uniform magnetic field exhibits
  significantly enhanced absorption (mode conversion) in comparison
  to a vertical field (depending on the frequency and radial order of
  the mode). A genetic algorithm is employed to adjust the parameters
  that control the radial structure of our sunspot models, in order
  to minimize the discrepancy between the theoretical predictions and
  the Hankel analysis measurements. For models that best fit the phase
  shifts, the agreement with the Hankel analysis data is excellent, and
  the corresponding absorption coefficients are generally in excess of the
  observed levels. On the other hand, for models that best fit the phase
  shift and absorption data simultaneously, the overall agreement is very
  good but the phase shifts agree less well. This is most likely caused
  by the different sizes of the regions responsible for the absorption and
  phase shift. Typically, the field strengths required by such models lie
  in the range 1-3kG, compatible with observations for sunspots and active
  regions. While there remain some uncertainties, our results provide
  further evidence that mode conversion is the predominant mechanism
  responsible for the observed absorption in sunspots; and that field
  inclination away from vertical is a necessary ingredient for any model
  that aims to simultaneously explain the phase shift and absorption data.

---------------------------------------------------------
Title: The GONG Farside Project
Authors: Leibacher, J. W.; Braun, D.; González Hernández, I.;
   Goodrich, J.; Kholikov, S.; Lindsey, C.; Malanushenko, A.; Scherrer, P.
2005AGUSMSP11B..14L    Altcode:
  The GONG program is currently providing near-real-time helioseismic
  images of the farside of the Sun. The continuous stream of low
  resolution images, obtained from the 6 earth based GONG stations, are
  merged into a single data series that are the input to the farside
  pipeline. In order to validate the farside images, it is crucial
  to compare the results obtained from different instruments. We show
  comparisons between the farside images provided by the MDI instrument
  and the GONG ones. New aditions to the pipeline will allow us to create
  full-hemisphere farside images, examples of the latest are shown in
  this poster. Our efforts are now concentrated in calibrating the
  farside signal so it became a reliable solar activity forecasting
  tool. We are also testing single-skip acoustic power holography
  at 5-7 mHz as a prospective means of reinforcing the signatures of
  active regions crossing the the east and west limb and monitoring
  acoustic emission in the neighborhoods of Sun's the poles. This work
  utilizes data obtained by the Global Oscillation Network Group (GONG)
  Program, managed by the National Solar Observatory, which is operated
  by AURA, Inc. under a cooperative agreement with the National Science
  Foundation. The data were acquired by instruments operated by the Big
  Bear Solar Observatory, High Altitude Observatory, Learmonth Solar
  Observatory, Udaipur Solar Observatory, Instituto de Astrofisico de
  Canarias, and Cerro Tololo Interamerican Observatory, as well as
  the Michaelson Doppler Imager on SoHO, a mission of international
  cooperation between ESA and NASA. This work has been supported by the
  NASA Living with a Star - Targeted Research and Technology program.

---------------------------------------------------------
Title: Flow Inversions for Phase-Sensitive Helioseismic Holography
Authors: Birch, A. C.; Braun, D. C.
2005AGUSMSP24A..05B    Altcode:
  Phase-sensitive holography has been used extensively to study solar
  subsurface mass flows. To date though, the ingression-egression
  correlation phases measured using phase-sensitive holography data
  have never been inverted. We present an inversion procedure, based
  on Born-approximation sensitivity functions and the MCD algorithm,
  for estimating subsurface flows from phase-sensitive holography
  measurements. We present some simple validation tests and example flow
  maps resulting from inversions of SOHO/MDI data.

---------------------------------------------------------
Title: Comparison of Solar Subsurface Velocities Using Small-Scale
    Ring Analysis, Time-Distance and Holography
Authors: Haber, D. A.; Featherstone, N. A.; Braun, D. C.; Hindman,
   B. W.; Bogart, R. S.
2005AGUSMSP24A..01H    Altcode:
  For the first time we compare subsurface horizontal velocity flows
  determined by all three common local helioseismic analysis methods
  on a very small scale (approximately 1-2 degrees). Holographic and
  time-distance techniques have been compared on small scales, however,
  ring analysis techniques have mainly been performed with 15 degree
  size tiles spaced 7.5 degrees apart. Here we use tiles approximately
  2 degrees in size with a spacing of 1 degree and compare the results
  with those of time-distance and holography. All three techniques have
  been applied to full-disc Doppler velocity data with 4" resolution (0.2
  deg at disc center) taken with the Michelson Doppler Imager instrument
  aboard SOHO during Carrington Rotation 1988 in March-April of 2002.

---------------------------------------------------------
Title: Towards Assessing, Understanding, and Correcting the Influence
    of Surface Magnetism in Local Helioseismology
Authors: Braun, D. C.; Schunker, H.; Lindsey, C.; Cally, P. S.
2005AGUSMSP23C..03B    Altcode:
  Efforts to probe subsurface wave-speed variations and mass flows
  near and under solar active regions are complicated and potentially
  compromised by strong phase and amplitude perturbations introduced in
  the photosphere by magnetic fields. Recently it has been shown that
  the phase distortions correlate with surface magnetic field strength
  and may be corrected to image wave-speed variations underlying active
  regions. A strong phase asymmetry between waves arriving into and
  departing from a magnetic region is also shown to produce spurious
  signatures of horizontal outflows below active regions. Further
  evidence of the photospheric origin of these phase distortions, as
  well as a key to their physical origin, is also presented. Using MDI
  observations, from the SOHO spacecraft, we perform ingression control
  correlations in the inclined magnetic fields of sunspot penumbra and
  demonstrate that incoming acoustic waves produce photospheric motion
  that describes an ellipse tilted towards the inclination of the magnetic
  field. A consequence is that the phase of the correlation varies with
  the viewing angle with respect to the field direction. Observations
  of the vector components of the photospheric fields could be used to
  correct these phase perturbations analogous to the procedures already
  developed using line-of-sight magnetograms. A physical understanding
  of surface distortions will come through MHD modeling, including
  simulations of the interaction of acoustic and magneto-acoustic-gravity
  waves with prescribed magnetic and sound-speed perturbations and flows
  (artificial data). The development of appropriate tools for assessing
  and correcting the effects of the surface magnetism will be vital for
  the interpretation of helioseismic data from the upcoming HMI mission
  on SDO. DCB and CL gratefully acknowledge support from the NSF (SAA/AST)
  and NASA (LWS, SR&amp;T).

---------------------------------------------------------
Title: The Local Helioseismology of Inclined Magnetic Fields and
    the Showerglass Effect
Authors: Schunker, H.; Braun, D. C.; Cally, P. S.; Lindsey, C.
2005ApJ...621L.149S    Altcode:
  We present evidence for the dependence of helioseismic Doppler
  signatures in active regions on the line-of-sight angle in inclined
  magnetic fields. Using data from the Michelson Doppler Imager
  (MDI) on board the Solar and Heliospheric Observatory, we performed
  phase-sensitive holography in the penumbrae of sunspots over the
  course of several days as the spots traversed the solar disk. Control
  correlations, which comprise a correlation of the surface wave amplitude
  with the incoming acoustic wave amplitude from a surrounding region,
  were mapped. There is a direct dependence of control-correlation phase
  signatures on the line-of-sight angle in the plane defined by the
  vertical and magnetic field vectors. The phase shift of waves observed
  along directions close to the orientation of the magnetic field is
  smaller than the phase shift observed when the line of sight is at a
  significant angle with respect to the field orientation. These findings
  have important implications for local helioseismology. The variation
  in phase shift (or the equivalent acoustic travel-time perturbations)
  with line-of-sight direction suggests that a substantial portion of the
  phase shift occurs in the photospheric magnetic field. Observations of
  the vector components of the field may be used to develop a proxy to
  correct these phase perturbations (known as the acoustic showerglass)
  that introduce uncertainties in the signatures of acoustic perturbations
  below the surface.

---------------------------------------------------------
Title: The Acoustic Showerglass. I. Seismic Diagnostics of
    Photospheric Magnetic Fields
Authors: Lindsey, Charles; Braun, D. C.
2005ApJ...620.1107L    Altcode:
  A problem of major interest in the helioseismology of active
  regions is the acoustics of magnetic photospheres and shallow
  subphotospheres. Magnetic fields suppress the photospheric signatures
  of acoustic waves impinging onto them from the underlying solar
  interior and shift their phases. The phase shifts function as a
  sort of acoustic showerglass that impairs the coherence of seismic
  waves arriving from below, degrading images of subsurface anomalies
  derived by mechanical reconstruction of phase-coherent waves. The
  purpose of this study is to characterize the “acoustic showerglass”
  in general optical terms and make a rough practical assessment of its
  impact on local seismic diagnostics of the shallow subphotospheres of
  active regions. We compile statistics comparing the acoustic field in
  magnetic photospheres with holographic projections of waves arriving
  from distant surrounding pupils. These “local control correlations”
  are consistent with an acoustic anomaly in the shallow subphotosphere
  of the active region that is strong but predominantly superficial;
  we call this the “acoustic Wilson depression.” The local control
  correlations also exhibit a phenomenon we call the “penumbral acoustic
  anomaly,” characterized by a conspicuous phase shift in regions of
  inclined magnetic field. This appears to be consistent with a fairly
  straightforward hydromechanical interpretation of the interaction of
  acoustic waves with photospheric magnetic forces. Detailed numerical
  simulations of the interaction of acoustic waves with magnetic forces
  can greatly facilitate our understanding of the acoustic showerglass
  and the thermal structure of the top few hundred kilometers of active
  region subphotospheres.

---------------------------------------------------------
Title: The Acoustic Showerglass. II. Imaging Active Region
    Subphotospheres
Authors: Lindsey, Charles; Braun, D. C.
2005ApJ...620.1118L    Altcode:
  Seismic diagnostics of the shallow subphotospheres of strong active
  regions are substantially impacted by large amplitude and phase
  perturbations introduced by overlying surface magnetic fields. These
  function as an “acoustic showerglass” that impairs the coherence
  of acoustic waves impinging onto the solar surface from below,
  degrading images of subsurface anomalies derived by phase-coherent
  seismic reconstruction. In an independent study we have developed a
  rough proxy to characterize showerglass phase errors based on maps of
  the square magnitude of the vector magnetic field at the surface. In
  this study we apply the proxy to correct helioseismic observations of
  active region photospheres from the Michelson Doppler Imager aboard the
  Solar and Heliospheric Observatory. We apply phase-correlation seismic
  holography to the corrected observations to image the underlying 5-10
  Mm subphotosphere. The corrected phase maps show no consistent evidence
  for sound-speed anomalies more than 5 Mm beneath a moderately large,
  isolated sunspot. Forward-modeling computations applied to simple
  models suggest sound-speed anomalies limited to approximately +/-250 m
  s<SUP>-1</SUP> for depths from 5 to 10 Mm, averaged over the horizontal
  extent of the sunspot. For complex active regions, uncertainties are
  considerably greater. However, results of this study suggest that more
  careful modeling of the acoustic showerglass will lead to substantially
  improved seismic diagnostics of active region subphotospheres. Detailed
  hydromechanical computations of acoustics models of active region
  photospheres and subphotospheres are needed to facilitate the
  interpretation of showerglass-corrected holographic signatures.

---------------------------------------------------------
Title: Principles of Seismic Holography for Diagnostics of the
    Shallow Subphotosphere
Authors: Lindsey, Charles; Braun, D. C.
2004ApJS..155..209L    Altcode:
  We develop the wave-mechanical formalism for phase-correlation
  computational seismic holography of the shallow subphotosphere under
  the plane-parallel approximation and apply it to helioseismic Doppler
  observations from the Michelson Doppler Imager on the SOHO spacecraft
  of both the quiet Sun and active regions. We compare holographic
  signatures computed wave-mechanically with similar signatures
  computed under the widely used eikonal approximation. The major
  difference between the hydromechanical and eikonal computations can
  be expressed in terms of acoustic dispersion effects within a few
  Mm of the solar surface. With an appropriate account for dispersion,
  the eikonal computations are remarkably accurate over a broad range
  of practical applications. A major imposition that confronts local
  diagnostics of the shallow subphotosphere is a phenomenon we call
  “ghost signatures,” artifacts introduced by a local ambiguity in
  the origin of the waves that give rise to the helioseismic signatures
  observed in the photosphere. Phase-correlation holographic signatures
  of the shallow subphotospheres of active regions are predominated by
  strong, stochastic phase shifts associated with magnetic fields at the
  solar surface. These introduce effects similar to those of an optical
  showerglass, significantly impairing the coherence of waves impinging
  into the magnetic photosphere from beneath, smearing the holographic
  signatures of possible subphotospheric anomalies.

---------------------------------------------------------
Title: Local Helioseismology of Inclined Magnetic Fields and the
    Showerglass Effect
Authors: Schunker, H.; Braun, D. C.; Lindsey, C.; Cally, P. S.
2004ESASP.559..227S    Altcode: 2004soho...14..227S
  No abstract at ADS

---------------------------------------------------------
Title: Local Helioseismology of Near-Surface Flows
Authors: Braun, D. C.; Birch, A. C.; Lindsey, C.
2004ESASP.559..337B    Altcode: 2004soho...14..337B
  No abstract at ADS

---------------------------------------------------------
Title: The Penumbral Acoustic Anomaly
Authors: Lindsey, C.; Braun, D. C.
2004ESASP.559..552L    Altcode: 2004soho...14..552L
  No abstract at ADS

---------------------------------------------------------
Title: Local Helioseismology of Solar Dynamics
Authors: Braun, D. C.; Lindsey, C.; Birch, A. C.
2004AAS...204.5309B    Altcode: 2004BAAS...36..757B
  We have initiated a systematic exploration of the dynamics of the
  solar interior, applying Doppler-sensitive seismic holography to data
  from the MDI instrument onboard the SOHO spacecraft and the Global
  Oscillations Network Group (GONG). Goals of this comprehensive project
  include understanding the nature of supergranulation, monitoring the
  subsurface variations of the meridional circulation, and understanding
  other subsurface flows and their relation to solar activity. We
  present initial results on our inference of subsurface flows due with
  an emphasis on control work, including comparisons between MDI and GONG
  datasets and other local seismic procedures such as ring diagrams. The
  project will develop and test data analysis tools and a forward
  (and inverse) modeling formalism based on the Born approximation,
  in preparation for their routine application to the next generation
  of helioseismic data from the Helioseismic and Magnetic Imager (HMI)
  on the Solar Dynamics Observer. This work is supported by funding
  from NASA SR&amp;T and Living With a Star programs and the NSF Stellar
  Astronomy and Astrophysics program.

---------------------------------------------------------
Title: The Acoustic Showerglass and Diagnostics of Active Region
    Subphotospheres
Authors: Lindsey, C.; Braun, D. C.
2004AAS...204.5310L    Altcode: 2004BAAS...36..757L
  Magnetic fields introduce large phase shifts into acoustic waves
  passing through the upper 400 km of an active region subphotosphere,
  impairing the phase coherence of time-distance correlation measurements,
  including seismic images of the underlying subphotosphere. We call
  this the "acoustic showerglass" effect. Reliable diagnostics of active
  region subphotospheres require a careful account of the interaction of
  acoustic waves with showerglass magnetic fields. A clear understanding
  of the acoustics of shallow magnetic fields offers the facility for
  detailed thermal modeling of the showerglass layer. It also opens the
  possibility of a high-quality magnetic proxy to correct showerglass
  phase errors, greatly improving our view of the underlying magnetic
  subphotosphere. The research reported in this poster is supported by
  grants from the National Aeronautics and Space Administration and the
  National Science Foundation.

---------------------------------------------------------
Title: Acoustic Holographic Studies of Solar Active Regions
Authors: Malanushenko, A.; Braun, D.; Kholikov, S.; Leibacher, J.;
   Lindsey, C.
2004IAUS..223..283M    Altcode: 2005IAUS..223..283M
  We present results of a study of the morphology and evolution of
  active regions using solar acoustic holography. These include acoustic
  signatures of large far-side active regions and their relationship to
  near-side activity indices a half rotation before and after the farside
  image, and the direct comparison of near-side acoustic signatures with
  the standard activity indicators, not only in their own right but also
  to calibrate the farside acoustic signature.

---------------------------------------------------------
Title: Microfluidic Experiments exploring Thermal Force approaches
    to the Origin of Life
Authors: Braun, D.
2004cosp...35..781B    Altcode: 2004cosp.meet..781B
  Microfluidic experiments are discussed where temperature gradients
  across mesoscopic pores provide essential boundary conditions for
  autonomous molecular evolution: (1) Laminar thermal convection can
  drive exponential DNA replication as the molecules are continuously
  cycled between hot and cold regions of a chamber. (2) Thermophoresis
  can induce strong accumulation of charged biopolymers such as DNA in the
  same convection settings. Combined, the experiments demonstrate a robust
  nonequilibrium boundary condition for the replication and accumulation
  of evolving molecules. The experimental conditions are comparable to
  conditions in porous rocks near submarine hydrothermal mounds. It is
  expected that further studies of microscopic open systems can reveal
  further unexpected connecting pieces in the fascinating puzzle on
  the origins of life. 1. D. Braun, N.L. Goddard and A. Libchaber,
  Exponential DNA Replication by Laminar Convection, Physical Review
  Letters 91:158103 (2003) 2. D. Braun &amp; A. Libchaber, Trapping of
  DNA by Thermophoretic Depletion and Convection, Physical Review Letters
  89:188103 (2002) 3. D. Braun &amp; A. Libchaber, Thermal force approach
  to molecular evolution, Physical Biology, accepted

---------------------------------------------------------
Title: Probing sunspot magnetic fields with p-mode absorption and
    phase shift data
Authors: Cally, P. S.; Crouch, A. D.; Braun, D. C.
2003MNRAS.346..381C    Altcode:
  Long-standing observations of incoming and outgoing f- and p-modes
  in annuli around sunspots reveal that the spots partially absorb
  and substantially shift the phase of waves incident upon them. The
  commonly favoured absorption mechanism is partial conversion to
  slow magneto-acoustic waves that disappear into the solar interior
  channelled by the magnetic field of the sunspot. However, up until
  now, only f-mode absorption could be accounted for quantitatively by
  this means. Based on vertical magnetic field models, the absorption of
  p-modes was insufficient. In this paper, we use the new calculations
  of Crouch &amp; Cally for inclined fields, and a simplified model of
  the interaction between spot interior and exterior. We find excellent
  agreement with phase shift data assuming field angles from the
  vertical in excess of 30° and Alfvén/acoustic equipartition depths
  of around 600-800 km. The absorption of f-modes produced by such
  models is considerably larger than is observed, but consistent with
  numerical simulations. On the other hand, p-mode absorption is generally
  consistent with observed values, up to some moderate frequency dependent
  on radial order. Thereafter, it is too large, assuming absorbing regions
  comparable in size to the inferred phase-shifting region. The excess
  absorption produced by the models is in stark contrast with previous
  calculations based on a vertical magnetic field, and is probably due
  to finite mode lifetimes and excess emission in acoustic glories. The
  excellent agreement of phase shift predictions with observational
  data allows some degree of probing of subsurface field strengths, and
  opens up the possibility of more accurate inversions using improved
  models. Most importantly, though, we have confirmed that slow mode
  conversion is a viable, and indeed the likely, cause of the observed
  absorption and phase shifts.

---------------------------------------------------------
Title: Computational Seismic Holography of Active Region
    Subphotospheres
Authors: Lindsey, C.; Braun, D. C.
2003SPD....34.0808L    Altcode: 2003BAAS...35Q.823L
  We apply phase-correlation seismic holography to SOHO/MDI observations
  of large sunspots to render signatures of local sound-speed anomalies
  in their shallow subphotospheres. In the computations reported
  here, a magnetic proxy we call the “showerglass correction” was
  applied to correct large phase errors introduced by surface magnetic
  fields. Preliminary results suggest a general sound speed enhancement
  in the range 1--4% up to depths of 10 Mm over horizontally extended
  regions surrounding large sunspots. These regions cover diameters
  roughly in the range 30--50 Mm. Phase maps of large active region
  complexes show signatures that tend to blanket most of the active
  region. The correlation between the phase shift and the magnetic
  field strength is generally high, but there are localized regions in
  which the phase signature departs significantly from the magnetic. The
  signature of the sunspot itself tends to be subtle with a maximum that
  may be significantly displaced towards the periphery of the active
  region. The research reported here is supported by funding from the
  Supporting Research and Technology and the Living with a Star Programs
  of the National Aeronautics and Space Administration, and from the
  Astronomical Sciences Division of the National Science Foundation.

---------------------------------------------------------
Title: The showerglass effect in seismic diagnostics of active
    region subphotospehres
Authors: Lindsey, Charles; Braun, D. C.
2003ESASP.517...23L    Altcode: 2003soho...12...23L
  A major obstacle that encumbers local seismic diagnostics of the shallow
  subphotospheres of strong active regions is phase errors introduced by
  overlying surface magnetic fields. These errors function as a sort of
  "acoustic showerglass" that obscures subphotospheric acoustic anomalies,
  scrambling computational images of these derived by phase-coherent
  seismic reconstruction. We develop a proxy based on the surface magnetic
  field to correct the showerglass phase errors and image acoustic
  scatterers beneath it. Preliminary applications of this correction give
  us signatures that appear to signify strong, sharply outlined acoustic
  anomalies 3-9 Mm beneath large growing active regions. Correction of
  the showerglass correction appears to be important, if not essential,
  for diffraction-limited diagnostics of acoustic anomalies in the
  shallow subphotospheres of strong active regions.

---------------------------------------------------------
Title: Helioseismic imaging of the farside and the interior
Authors: Braun, D. C.; Lindsey, C.
2003ESASP.517...15B    Altcode: 2003soho...12...15B
  Helioseismic holography is a highly efficient and flexible procedure
  with a wide range of utility, from mapping sound wave travel times over
  the entire far solar hemisphere to imaging small scale scatterers and
  flows beneath solar active regions. Seismic images covering the entire
  far hemisphere of the Sun have been constructed using data from the
  recently upgraded Global Oscillation Network Group (GONG+) network
  and compare favorably with those made using simultaneous data from
  the Michelson Doppler Imager (MDI) onboard the Solar and Heliospheric
  Observer (SOHO). We are also continuing our comprehensive exploration
  of diffraction-limited seismic imaging of active regions. We have
  recently extended our applications of helioseismic holography to include
  Doppler diagnostics of active regions and quiet Sun. A major finding
  presented here is that the horizontal velocity field in supergranules
  and sunspot moats appears to be concentrated at the surface. Another
  recent, but vital, contribution to local helioseismology has been a
  study of what is termed the "showerglass effect". Magnetic fields in
  the photosphere produce large, local amplitude and phase perturbations
  to the observed acoustic wave field which may be quantified and removed
  prior to the holographic computations. Removal of the showerglass from
  local helioseismic images of active regions is proving to be a crucial
  step in the detection of compact subsurface scatterers.

---------------------------------------------------------
Title: MDI and GONG inferences of the changing solar interior
Authors: Barban, C.; Howe, R.; Hill, F.; Komm, R. W.; Leibacher, J.;
   Toner, C.; Bogart, R.; Braun, D.; Haber, D.; Hindman, B.; Lindsey, C.
2002ESASP.508...55B    Altcode: 2002soho...11...55B
  The Global Oscillation Network Group (GONG) and the Solar Oscillations
  Investigation (SOI) using the Michelson Doppler Imager (MDI) instrument
  aboard the SOHO spacecraft provide combined data sets that now cover
  more than six years and allow us to probe the changing dynamics of the
  convection zone in unprecedented detail. Here we present the latest
  combined results from both projects, showing the evolution of the
  migrating zonal flows close to the surface and also changes close to
  and below the base of the convection zone, as well as changes in the
  mode parameters related to surface magnetic activity variation in time
  and latitude.

---------------------------------------------------------
Title: The First Seismic Images of the Solar Interior and Far Side
    from the GONG+ Network
Authors: Braun, D. C.; Lindsey, C.
2002AAS...200.8906B    Altcode: 2002BAAS...34..791B
  Since mid-2001, the upgraded GONG+ network has been providing
  high-resolution Doppler images of the Sun. We are now analyzing GONG+
  data as part of our program in local helioseismology and acoustic
  holography. The bulk of the results shown here are derived from data
  obtained during a 24-hour period in 2001 September, when simultaneous
  full-disk observations from the MDI instrument onboard the SOHO
  spacecraft were available for comparison. Images showing the acoustic
  travel-time perturbations over the entire far hemisphere obtained from
  GONG+ and MDI data are essentially identical. This demonstrates that
  the GONG+ network may be used as the basis of a synoptic far-side
  imaging program of comparable quality to that now provided by
  MDI. Holographic depth-diagnostics of travel-time perturbations below
  several active regions on the solar front side are also presented. These
  phase-sensitive holographic images from GONG+ and MDI have similar
  noise characteristics when computed using acoustic modes with degree
  (wavenumber) below about 300, which implies that the r.m.s. fluctuations
  in these images are solar in nature. At higher wavenumbers, atmospheric
  seeing introduces an excess r.m.s., which increases with mode degree,
  to the images derived from GONG+ data. However, acceptable images are
  possible using modes with degrees up to at least 700. We will discuss
  how GONG+ data may be advantageously utilized in detailed, continuous,
  and long-term local-helioseismic analyses of the far side and deep
  interior of the Sun. This work is supported by awards AST-9987286 from
  NSF, and awards NASW-01007 and NAG5-10984 from NASA.

---------------------------------------------------------
Title: Computational Seismic Holography of the Deep Interior and
    Far Surface of the Sun
Authors: Lindsey, C.; Braun, D. C.
2002AAS...200.7903L    Altcode: 2002BAAS...34..780L
  Computational seismic holography has given us a remarkably flexible and
  powerful new utility for local diagnostics of the solar interior. Major
  results to date include the following: - Seismic signatures
  surrounding sunspots up to 100 Mm in diameter, called “acoustic
  moats.” - Enhancements of locally stochastic seismic emission, called
  “acoustic glories,” surrounding complex active regions. - Chromatic
  siesmic emission maps of a solar flare. - Signatures suggesting compact
  thermal enhancements in the shallow subphotospheres of surface magnetic
  regions. - Synoptic phase-correlation maps of active regions on the
  far surface of the Sun. Prospects for deep interior diagnostics of the
  solar interior are highly encouraging. Seismic holography applied to the
  database we expect from the Solar Dynamics Observatory is nearly certain
  to give us a synoptic view of the local structure of flows and torsional
  oscillations down to the base of the convection zone. Cooperative
  seismic observations of both near and far surfaces of the Sun offer
  high quality holographic diagnostics of the solar core. Holographic
  diagnostics promise deep insight into the operation of the solar dynamo,
  and may give us indications of emerging magnetic fields significantly
  in advance of their appearance at the solar surface. This research
  has been supported by funding from the National Science Foundation
  and the National Aeronautics and Space Administration.

---------------------------------------------------------
Title: Helioseismological observations of active regions
Authors: Braun, Douglas
2002ocnd.confE...3B    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: Seismic forecasting of solar activity
Authors: Braun, D. C.; Lindsey, C.
2002HiA....12..378B    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: Seismic Imaging of the Far Hemisphere of the Sun
Authors: Braun, D. C.; Lindsey, C.
2001ApJ...560L.189B    Altcode:
  We apply phase-sensitive helioseismic holography to Solar and
  Heliospheric Observatory/Michelson Dopper Imager data to demonstrate
  how acoustic travel-time perturbations may be mapped over the entire
  portion of the Sun facing away from the Earth, including the polar
  regions. In addition to offering significant improvements to ongoing
  space weather forecasting efforts, the procedure offers the possibility
  of local seismic monitoring of both the temporal and spatial variations
  in the acoustic properties of the Sun over all of the far surface.

---------------------------------------------------------
Title: Helioseismic Holography and a Study of the Process of Magnetic
    Flux Disappearance in Canceling Bipoles
Authors: Lindsey, Charles; Harvey, Karen L.; Braun, D.; Jones, H. P.;
   Penn, M.; Hassler, D.
2001STIN...0156300L    Altcode:
  Project 1: We have developed and applied a technique of helioseismic
  holography along the lines of originally set out in our proposal. The
  result of the application of this diagnostic technique to solar activity
  and the quiet Sun has produced a number of important discoveries:
  (1) acoustic moats surrounding sunspots; (2) acoustic glories
  surround large active regions; (3) acoustic condensations beneath
  active regions; and (4) temporally-resolve acoustic images of a solar
  flare. These results have been published in a series of papers in the
  Astrophysical Journal. We think that helioseismic holography is now
  established as the most powerful and discriminating diagnostic in local
  helioseismology. Project 2: We conducted a collaborative observational
  program to define the physical character and magnetic geometry of
  canceling magnetic bipoles aimed at determining if the cancellation
  process is the result of submergence of magnetic fields. This assessment
  is based on ground-based observations combining photospheric and
  chromospheric magnetograms from NSO/KP, BBSO, and SOHO-MDI, and EUV
  and X-ray images from SOHO EIT/CDS, Yohkoh/SXT, and TRACE. Our study
  involves the analysis of data taken during three observing campaigns to
  define the height structure of canceling bipoles inferred from magnetic
  field and intensity images, and how this varies with time. We find
  that some canceling bipoles can be explained by the submerge of their
  magnetic flux. A paper on the results of this analysis will be presented
  at an upcoming scientific meeting and be written up for publication.

---------------------------------------------------------
Title: Progress in Helioseismic Holography
Authors: Braun, D. C.
2001AGUSM..SP21C07B    Altcode:
  Local Helioseismology uses acoustic waves to probe small-scale
  structures in the solar interior down to a spatial resolution
  imposed by wave diffraction. Although its practitioners, including
  this author, may sometimes employ measurements of the acoustic wave
  field made over a local area of the Sun's surface to examine its
  shallow layers, local helioseismology generally has a much broader
  utility. For example, some applications of helioseismic holography
  (and other local diagnostics) require global acoustic modes, observed
  over large portions of the surface, to produce diffraction-limited
  images of the far side or deep interior of the Sun. In this review,
  I will summarize recent progress achieved in seismic holography in
  collaboration with C. Lindsey (SPRC). With P. Scherrer and the SOI-MDI
  team at Stanford, we have helped to realize a daily synoptic monitor of
  far-side activity using medium-resolution MDI images obtained within
  24 hours of their acquisition by the SOHO spacecraft. In addition,
  we have laid out the basic theoretical groundwork for the application
  of computational seismic holography to the deep solar interior to
  image the tachocline and underlying radiative core of the Sun. Taking
  advantage of the substantial depth sensitivity of horizontal-flow
  diagnostics, we have recently adapted our holographic software to
  test the basic techniques on the shallow subphotospheres of active
  regions. The utility of both ground- and space-based instruments is
  usually enhanced by their combination and comparison. I will present
  the results of holographic analyses of simultaneous GONG+ prototype
  and SOI-MDI observations of a large flare-producing active region. The
  general similarity of the helioseismic images from both instruments is
  noteworthy. This demonstrates the feasibility of increasing the temporal
  and spatial coverage available to local analyses by combining SOHO data
  with that obtained from the GONG+ network. We gratefully acknowledge
  recent support from the National Science Foundation (AST-9987286)
  and a contract (PY-0184) from the NASA-funded SOI-MDI project at
  Stanford University.

---------------------------------------------------------
Title: Prospects for Helioseismic Holography in the Deep Solar
    Interior
Authors: Lindsey, C.; Braun, D. C.
2001AGUSM..SP21C08L    Altcode:
  Holographic seismic imaging of low-degree acoustic noise
  opens new prospects for solar interior diagnostics that are most
  encouraging. Seismic imaging of the near solar interior has given us the
  discoveries of “acoustic moats,” surrounding sunspots, of anomalous
  emission from “acoustic glories” surrounding large active regions,
  acoustic images of solar flares, and the signatures of apparent acoustic
  perturbations up to 20~Mm beneath active region photospheres. Low-degree
  seismic holography is now giving us images of large magnetic regions
  on the far surface of the Sun, a utility with valuable space-weather
  forecasting and general synoptic applications. Extensions of the
  foregoing applications promise insight into the deep solar interior,
  to the base of the convection zone and into the Sun's nuclear-burning
  core. Diffraction-limited imaging of low-degree noise over pupils
  covering most of the near solar hemisphere offer the most discriminating
  probe of the deep solar interior. Earth-based helioseismic observations
  coordinated with seismic observations of the far side of the Sun at
  frequencies in the range 6--7 mHz would allow us to resolve local
  thermal and Doppler structure in the solar core with a resolution of
  75~Mm. Coordinated seismic observations of both near and far sides
  of the Sun are essential to take advantage of the superior spatial
  resolution offered by high-frequency waves.

---------------------------------------------------------
Title: Seismic Holography of the Solar Interior and Far Side
Authors: Braun, D. C.; Lindsey, C.
2001IAUS..203..167B    Altcode:
  The development of solar acoustic holography has opened a major
  new diagnostic avenue in local helioseismology. Its application to
  SOI-MDI data from SOHO has revealed “acoustic moats” surrounding
  sunspots, “acoustic glories” surrounding complex active-regions,
  and “acoustic condensations” suggesting the existence of significant
  seismic anomalies up to 20 Mm beneath active-region photospheres. It has
  given us the first seismic images of a solar flare, and has uncovered a
  remarkable anomaly in the statistical distribution of seismic emission
  from acoustic glories. Phase-sensitive seismic holography is now
  producing high-resolution maps of sound travel-time anomalies caused
  by magnetic forces in the immediate subphotosphere, apparent thermal
  enhancements in acoustic moats, and Doppler signatures of subsurface
  flows. It has also produced the first seismic images of active regions
  on the far-side of the Sun, giving us a powerful tool for forecasting
  more than a week in advance their arrival at the east limb. This
  diagnostic now promises a new insight into the hydromechanical and
  thermal environments of the solar interior in the local perspective.

---------------------------------------------------------
Title: Seismic Holography of the Deep Solar Interior
Authors: Lindsey, C.; Braun, D. C.
2000SPD....31.0503L    Altcode: 2000BAAS...32R.836L
  The first images of magnetic regions on the far solar surface
  were recently secured by applying seismic holography to five-minute
  oscillations with spherical harmonic degrees roughly in the range 20 to
  40 in SOHO-MDI observations. These waves penetrate up to half way to the
  sun's center, and can therefore sample the base of the convection zone
  with a resolution similar to that of the aforementioned far-side images,
  approximately 10<SUP>o</SUP> in longitude at the solar equator. However,
  by far the best seismic diagnostics are invariably offered by the
  highest possible frequencies, 6 mHz and above, if possible. Because
  these waves are efficiently absorbed by the solar surface, helioseismic
  observations that can compare the far side of the sun with earth-based
  observations of the near side are needed for coherent phase-sensitive
  imaging of the deep solar interior. Coordinated near- and far-side
  seismic observations of the sun at frequencies in the range 6--7
  mHz would allow us to examine the thermal and Doppler profile of the
  solar core with a resolution of 75 Mm. This presentation is based on
  research supported by grants NAG5-7236 from NASA and AST-9528249 from
  NSF, and by a contract, PY-0184, with Stanford University.

---------------------------------------------------------
Title: Seismic Imaging of the Far Side and Interior of the Sun
Authors: Braun, D. C.; Lindsey, C.
2000SPD....3102112B    Altcode: 2000BAAS...32Q.831B
  Images of active regions on the far side of the Sun were derived
  by applying seismic holography to observations from the SOI-MDI
  instrument on the SOHO spacecraft. Synoptic seismic imaging of
  far-side solar activity will allow anticipation of the appearance of
  large active regions more than a week ahead of their arrival on the
  east limb. The technical requirements for a synoptic monitor appear
  to be quite modest, given real time access to observations from the
  Global Oscillations Network Group, for example. Currently, seismic
  images of the solar far side are easily computed in less than a day
  using a single-processor Pentium-based PC running Linux. In addition to
  providing new applications for space weather prediction, the development
  of solar acoustic holography is opening major new diagnostic avenues in
  the study of the solar interior. Phase-sensitive seismic holography is
  producing high-resolution maps of sound travel-time anomalies caused
  by magnetic forces in the immediate subphotosphere, apparent thermal
  enhancements in acoustic moats around sunspots, and Doppler signatures
  of subsurface flows. Seismic holography applied to global modes, such
  as those used to image the far side, has directly demonstrated the
  influence of active regions on these modes. This reinforces a growing
  consensus that reduced sound travel times in magnetic regions explain
  the entirety of the frequency shifts of global modes with the solar
  cycle. Phase-sensitive holography will also be used to probe thermal
  and Doppler perturbations deep in the solar convection zone and the
  tachocline. This work is supported by grants NAG5-7236 from NASA
  and AST-9528249 from NSF, and by a contract, PY-0184, from Stanford
  University.

---------------------------------------------------------
Title: Stochastic Seismic Emission from Acoustic Glories and the
    Quiet Sun
Authors: Donea, A. -C.; Lindsey, C.; Braun, D. C.
2000SoPh..192..321D    Altcode:
  Helioseismic images of multipolar active regions show enhanced seismic
  emission in 5-mHz oscillations in a halo surrounding the active region
  called the `acoustic glory'. The acoustic glories contain elements
  that sustain an average seismic emission 50% greater than similar
  elements in the quiet Sun. The most intense seismic emitters tend to
  form strings in non-magnetic regions, sometimes marking the borders of
  weak magnetic regions and the separation between weak magnetic regions
  of opposite polarity. This study compares the temporal character
  of seismic emission from acoustic glories with that from the quiet
  Sun. The power distribution of quiet-Sun seismic emission far from solar
  activity is exponential, as for random Gaussian noise, and therefore
  not perceivably episodic. The distribution of seismic power emanating
  from the most intense elements that comprise the acoustic glories is
  exponential out to approximately 4 times the average power emitted
  by the quiet Sun. Above this threshold the latter distribution shows
  significant saturation, suggesting the operation of a hydromechanical
  non-linearity that sets limits on the acoustic power generated by
  the convection zone. This could give us considerable insight into the
  physical mechanism of seismic emission from the near subphotosphere.

---------------------------------------------------------
Title: Helioseismic Holography of Active-Region Subphotospheres -
    (Invited Review)
Authors: Braun, D. C.; Lindsey, C.
2000SoPh..192..285B    Altcode:
  The development of solar acoustic holography has opened a major new
  diagnostic avenue in local helioseismology. It has revealed `acoustic
  moats' surrounding sunspots, `acoustic glories' surrounding complex
  active regions, and `acoustic condensations' suggesting the existence
  of significant seismic anomalies up to 20 Mm beneath active-region
  photospheres. Phase-sensitive seismic holography is now yielding
  high-resolution maps of sound travel-time anomalies caused by magnetic
  forces in the immediate subphotosphere, apparent thermal enhancements
  in acoustic moats, and Doppler signatures of subsurface flows. It has
  given us the first seismic images of a solar flare, and has uncovered a
  remarkable anomaly in the statistical distribution of seismic emission
  from acoustic glories. Seismic holography will probably give us the
  means for early detection of large active regions on the far-surface
  of the Sun, and possibly of deep subsurface activity as well. This
  powerful diagnostic now promises a new insight into the hydromechanical
  and thermal environments of the solar interior in the local perspective.

---------------------------------------------------------
Title: Seismic Images of the Far Side of the Sun
Authors: Lindsey, C.; Braun, D. C.
2000Sci...287.1799L    Altcode:
  Images of an active region on the far side of the sun were derived by
  applying seismic holography to recent helioseismic observations from
  space. Active regions are the centers of energetic phenomena such as
  solar flares and coronal mass ejections, whose resulting electromagnetic
  and particle radiation interfere with telecommunications and power
  transmissions on Earth and can pose significant hazards to astronauts
  and spacecraft. Synoptic seismic imaging of far-side solar activity
  will now allow anticipation of the appearance of large active regions
  more than a week ahead of their arrival on the east solar limb.

---------------------------------------------------------
Title: Phase-sensitive Holography of Solar Activity
Authors: Braun, D. C.; Lindsey, C.
2000SoPh..192..307B    Altcode:
  Phase-correlation statistics comparing acoustic radiation coming
  out of a particular point on the solar photosphere with acoustic
  radiation going into it show considerably reduced sound travel times
  through the subphotospheres of active regions. We have now applied
  techniques in phase-sensitive seismic holography to data from the Solar
  Oscillations Investigation - Michelson Doppler Imager (SOI-MDI) on the
  Solar and Heliospheric Observatory (SOHO) spacecraft to obtain high
  resolution phase-correlation maps of a large, complex active region
  and the `acoustic moat' which surrounds it. We report the following
  new results: First, the reduced sound travel-time perturbations in
  sunspots, acoustic moats, and isolated plages increase approximately in
  proportion to the logarithm of the surface magnetic flux density, for
  flux densities above 10 G. This is consistent with an interpretation
  of the travel-time anomalies, observed with holographic and other
  local-helioseismic procedures, as caused by acoustic Wilson-like
  depressions in photospheres of magnetic regions. Second, we find that,
  compared with isolated plages, the acoustic moats have an additional
  sound travel-time reduction on the order of 3-5 s which may be
  explained by a thermal excess due to the blockage of convective
  transport by the sunspot photosphere. Third, the combined effect of
  the Wilson depression in plages, acoustic moats, and sunspots may
  explain the observed variation of global p-mode frequencies with the
  solar cycle. Fourth, we find that active regions, including sunspots,
  acoustic moats, and plages, significantly reflect p modes above the
  acoustic cut-off frequency, where the surface of the quiet Sun acts
  as a nearly perfect absorber of incident acoustic radiation.

---------------------------------------------------------
Title: Basic Principles of Solar Acoustic Holography - (Invited
    Review)
Authors: Lindsey, C.; Braun, D. C.
2000SoPh..192..261L    Altcode:
  We summarize the basic principles of holographic seismic imaging of
  the solar interior, drawing on familiar principles in optics and
  parallels with standard optical holography. Computational seismic
  holography is accomplished by the phase-coherent wave-mechanical
  reconstruction of the p-mode acoustic field into the solar interior
  based on helioseismic observations at the solar surface. It treats the
  acoustic field at the solar surface in a way broadly analogous to how
  the eye treats electromagnetic radiation at the surface of the cornea,
  wave-mechanically refocusing radiation from submerged sources to render
  stigmatic images that can be sampled over focal surfaces at any desired
  depth. Holographic diagnostics offer a straight-forward assessment of
  the informational content of the observed p-mode spectrum independent
  of prospective physical models of the local interior anomalies that
  it represents. Computational holography was proposed as the optimum
  approach whereby to address the severe diffraction effects that
  confront standard tomography in the solar p-mode environment. It has
  given us a number of remarkable discoveries in the last two years
  and now promises a new insight into solar interior structure and
  dynamics in the local perspective. We compare the diagnostic roles of
  simple acoustic-power holography and phase-sensitive holography, and
  anticipate approaches to solar interior modeling based on holographic
  signatures. We identify simple computational principles that, applied to
  high-quality helioseismic observations, make it easy for prospective
  analysts to produce high-quality holographic images for practical
  applications in local helioseismology.

---------------------------------------------------------
Title: Seismic Forecasting of Solar Activity
Authors: Lindsey, C.; Braun, D. C.
2000IAUJD...7E...4L    Altcode:
  from SOHO, has recently given us the first images of an active region on
  the far side of the Sun. The advent of phase-coherent seismic imaging is
  now allowing us quite literally to look into the solar interior from a
  local perspective, indeed to see through the solar interior acoustically
  to its far surface. Space and ground-based helioseismic observatories
  will soon have the capability for “real-time helioseismology,” and
  will be routinely monitoring the far surface of the Sun. This will
  greatly facilitate medium-range forecasts important to space weather,
  allowing us to anticipate more than a week in advance the arrival
  of large far-side active regions at the Sun's east limb to within a
  few hours.

---------------------------------------------------------
Title: The MVACS soil temperature probe.
Authors: Wood, S. E.; Paige, D. A.; Nguyen, A.; Crisp, D.; Alleruzzo,
   R.; Labaw, C.; Mahoney, C.; Vargas, R.; Gunderson, H.; Braun, D.;
   Slostad, J.; Manvi, R.; Brown, K.; Oakes, E.
1999BAAS...31.1146W    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: The MVACS Soil Temperature Probe
Authors: Wood, S. E.; Paige, D. A.; Nguyen, A.; Crisp, D.; Alleruzzo,
   R.; Labaw, C.; Mahoney, C.; Vargas, R.; Gunderson, H.; Braun, D.;
   Slostad, J.; Manvi, R.; Brown, K.; Oakes, E.
1999DPS....31.4711W    Altcode:
  As part of the Mars Volatiles and Climate Surveyor (MVACS) payload
  on Mars Polar Lander, currently on its way to a Dec. 3, 1999 landing
  on the south polar layered deposits, the Soil Temperature Probe (STP)
  will make direct measurements of the temperatures and thermophysical
  properties of soils and/or ices accessible by the Robotic Arm (RA). The
  STP consists of a thin, rigid fiberglass tube 15 cm long containing 2
  platinum resistance temperature sensors; one in the metal tip which can
  be heated (PRT-1), and another inside the tube (PRT-2). It is mounted
  on the side of the scoop at the end of the RA. To make measurements,
  the RA places the STP in the desired location on or beneath the surface,
  and Robotic Arm Camera (RAC) image(s) are taken to verify its position,
  using ruler markings on the STP to measure its depth. The temperatures
  of both PRT's are recorded every 3 seconds. Data and commanding
  are handled through the meteorology instruments (MET) electronics
  package. Measurement of thermophysical properties can be done actively
  or passively. In active mode, PRT-1 is heated at a constant rate ( 10
  mW). The thermal conductivity of the surrounding soil can be derived
  from the asymptotic temperature rise. The thermal diffusivity (alpha )
  can be derived from the transient response. In passive mode alpha can
  also be determined by measuring the change in the amplitude and phase
  of the diurnal thermal wave at different depths. The temperature and
  thermophysical property measurements obtained with the STP will be
  very useful for interpreting other MVACS observations including air
  temperature and humidity, the presence or absence of subsurface ice,
  the identity of any surface frosts (CO_2 or H_2O), and Thermal Evolved
  Gas Analyzer soil sample analysis. These STP measurements will also
  provide invaluable "ground truth" for comparison with data from orbiting
  spacecraft such as Mars Global Surveyor and Mars Climate Orbiter.

---------------------------------------------------------
Title: New Results from Helioseismic Holography
Authors: Braun, D. C.
1999AAS...194.4202B    Altcode: 1999BAAS...31..882B
  The application of helioseismic holography (also called seismic
  imaging) to solar data is among the latest developments in local
  helioseismology. This procedure applies helioseismic observations at
  the solar surface in time-reverse to a model of the solar interior,
  coherently regressing the surface disturbances downward to render
  acoustic images of subsurface structure. I will describe the basic
  concept, first developed ten years ago by C. Lindsey and D. Braun
  (1990 Solar Physics, 126, 101), and present new results from our
  recent application of the method to SOHO/MDI data. Notable discoveries
  include the “acoustic moat” (extended 3-mHz absorption surrounding
  all active regions), “acoustic glories” (high frequency halos of
  emission around complex active regions), acoustic condensations up to
  20 Mm beneath active regions, and the 6-mHz acoustic reflectivity of
  active regions. Recent results obtained with phase-sensitive seismic
  holography demonstrate a wave-speed perturbation beneath acoustic moats,
  which may be a manifestation of a localized convection cell predicted
  by theoretical models of sunspot convection and energy transport. The
  development of seismic-imaging procedures sensitive to Doppler and
  thermal perturbations promises to provide considerable insight into
  the physical conditions underlying active regions. This research is
  supported by NSF Grants AST 9521637 and AST 9528249, and NASA Grants
  NAGW-97029 and NAG5-7236.

---------------------------------------------------------
Title: Phase-Sensitive Holography of Acoustic Moats
Authors: Braun, D. C.; Lindsey, C.
1999AAS...194.5610B    Altcode: 1999BAAS...31..913B
  Phase-correlation statistics comparing acoustic radiation coming out
  of a particular point on the solar photosphere with acoustic radiation
  going into it show considerably reduced sound travel times through the
  subphotospheres of active regions. This is already well established by
  time-distance correlations measured by Duvall et al., and is consistent
  with earlier measurements of scattering phase shifts of single sunspots
  by Braun and Fan. We have now applied techniques in phase-sensitive
  seismic holography to obtain high resolution phase-correlation maps
  of active regions and the “acoustic moats” that surround them. The
  important new result which the holographic correlation maps give us
  is that the seismic perturbation manifested by the acoustic moats
  is generally quite significant and in large active-region complexes
  predominant. Indeed, the acoustic moat surrounding the large active
  region complex NOAA AR 8179 (1998 March 16) manifests a one-way
  travel-time reduction of ~ 30s over an area of some 10(4) Mm(2) ,
  encompassing all of the significant sunspots in the region. Onto
  this phase perturbation the major sunspots impose an additional
  localized contribution of ~ 30s. These results strongly reinforce an
  interpretation of the acoustic moat as a well integrated convection
  cell driven by the thermal perturbation that results from the local
  blockage of convective heat transport by the sunspot photosphere. The
  remarkable lateral extent of the acoustic moat, some 100 Mm in latitude
  and more than 150 Mm in longitude, suggests a convective flow that
  undertakes to spread the thermal perturbation into a relatively thin
  layer, such that the excess heat contained therein can access the
  solar surface through normal supergranular and granular diffusion. We
  expect holographic Doppler diagnostics, now under development, to shed
  considerable light very soon on the flows that are needed to explain
  the extended dimensions of the thermal perturbations that surround
  large active regions. This research is supported by NSF Grants AST
  9521637 and AST 9528249, and NASA Grants NAGW-97029 and NAG5-7236.

---------------------------------------------------------
Title: Seismic Images of a Solar Flare
Authors: Donea, A. -C.; Braun, D. C.; Lindsey, C.
1999ApJ...513L.143D    Altcode:
  We have used helioseismic holography to render seismic images of
  the solar flare of 1996 July 9, whose helioseismic signature was
  recently reported by Kosovichev &amp; Zharkova. We computed time
  series of “egression power maps” in 2 mHz bands centered at 3.5 and
  6 mHz. These images suggest an oblong acoustic source associated with
  the flare some 18 Mm in the north-south direction and approximately 15
  Mm in the east-west direction. The considerable preponderance of the
  flare acoustic power emanates in the 3.5 mHz band. However, because
  the ambient noise in the 6 mHz band is much lower and the diffraction
  limit for 6 mHz waves is much finer, the flare is rendered far more
  clearly in the 6 mHz band. The 6 mHz flare signature lags the 3.5 mHz
  by approximately 4 minutes.

---------------------------------------------------------
Title: Helioseismic Images of an Active Region Complex
Authors: Braun, D. C.; Lindsey, C.
1999ApJ...513L..79B    Altcode:
  Helioseismic images of a large active region complex at a frequency
  of 5 mHz show a prominent halo of acoustic emission, which we
  call the “acoustic glory,” surrounding the active region. This
  feature is remarkably intense and contains small-scale elements of
  concentrated seismic emission which cluster in strings in nonmagnetic
  regions. Subsurface images show condensations of acoustic deficit
  that appear to represent acoustic perturbations located in excess of
  10 Mm beneath the photosphere. The analysis of this complex active
  region suggests that these features are common in the neighborhoods of
  large active regions and can appear tens of megameters horizontally
  separated from sunspots. We propose that acoustic condensations are
  the result of refraction or scattering by subsurface thermal or Doppler
  perturbations below active regions. The appearance of acoustic glories
  and condensations strongly suggests that complex active regions have
  acoustic properties that are fundamentally different from those of
  single isolated sunspots.

---------------------------------------------------------
Title: Chromatic Holography of the Sunspot Acoustic Environment
Authors: Lindsey, C.; Braun, D. C.
1999ApJ...510..494L    Altcode:
  We use helioseismic holography to obtain seismic images of a sunspot
  and its local environment over the 3-8 mHz acoustic spectrum. We
  are particularly interested in the acoustic deficit brought about by
  strong acoustic absorption by the sunspot itself in the 3-4 mHz range
  and in the helioseismic character of the “acoustic moat” recently
  discovered by Braun et al. The holographic images computed here clearly
  show that over a broad range in frequency the sunspot replaces the
  acoustic radiation impinging into it from the ambient solar interior
  with an outgoing acoustic flux that is only a fraction of that which
  it receives. This acoustic deficit persists uniformly over the 3-7
  mHz spectrum, even as the reflectivity of the quiet-Sun photosphere
  goes from being an almost perfect, specular reflector at 4 mHz to an
  almost perfect absorber at 5 mHz. As far as we can judge, the acoustic
  moat surrounding the sunspot need not require a helioseismic absorption
  mechanism of its own. Its signature in 3-4 mHz images could arise from
  simple scattering of an acoustic deficit that originates in the nearby
  sunspot. Such scattering may be the result of a thermal perturbation
  resulting from the blockage of convective heat transport through the
  sunspot photosphere. Alternatively, it could be the signature of a
  Doppler perturbation attendant to the rapid convective outflow that
  might be driven by such a thermal accumulation. While the results
  presented here do not rule out the possibility that the acoustic moat
  has its own absorption mechanism, they show little independent evidence
  to indicate that the acoustic moat otherwise behaves very differently
  from the quiet Sun where absorption and reemission of acoustic flux
  are concerned. <P />Helioseismic images of conspicuous halos that
  appear in 6 mHz acoustic power maps show no significant enhancement of
  acoustic emission from these regions. A fairly broad region surrounding
  the sunspot appears to render a weak enhancement, ~2.5%, in the local
  generation of 5 mHz acoustic power. This seems to explain peculiarities
  in the spectrum of acoustic flux balance measurements based on Hankel
  analysis. The distribution of the 5 mHz “acoustic egression” excess
  is fairly diffuse and does not seem to be spatially correlated with
  the strong acoustic power halos seen in 6 mHz acoustic power maps.

---------------------------------------------------------
Title: Erratum: Helioseismic Measurements of the Subsurface
    Meridional Flow
Authors: Braun, D. C.; Fan, Y.
1999ApJ...510L..81B    Altcode:
  In the Letter “Helioseismic Measurements of the Subsurface Meridional
  Flow” by D. C. Braun and Y. Fan (<A href="/abs/1998ApJ...508L.105">ApJ,
  508, L105 [1998]</A>), equation (4) was misprinted and should appear as
  follows:&lt;U<SUB>θ</SUB>&gt;≡-(θ<SUB>max</SUB>-θ<SUB>min</SUB>)<SUP>-1</SUP>θ<SUB>min</SUB>θ<SUB>max</SUB>U\b.dot
  θ̂dθ. (4)

---------------------------------------------------------
Title: Comparative Results from Seismic Imaging and Hankel Analysis
Authors: Braun, D. C.
1999soho....9E..27B    Altcode:
  Studies of solar active regions using Hankel-decomposition techniques
  have clearly demonstrated over the past decade that sunspots and plage
  are efficient absorbers of acoustic waves, and that the wave speeds
  below sunspots are generally greater than that of the surrounding quiet
  Sun. These results have been consistently confirmed by more recent
  applications of both seismic-imaging and time-distance correlation
  analyses. The development of seismic imaging (or helioseismic
  holography), originally conceived ten years ago by C. Lindsey and
  D. Braun, and recently applied to SOHO/MDI data, has additionally
  provided important insights regarding the spatial (horizontal and
  vertical) structure of the acoustic perturbations first detected
  with Hankel analysis. Moreover, holography has enabled a number of
  remarkable new discoveries including the "acoustic moat," "acoustic
  glories," acoustic condensations up to 20 Mm beneath active regions,
  and the reflectivity of active regions above the quiet-Sun acoustic
  cut-off frequency. Recent application of phase-sensitive holographic
  procedures have also revealed a subsurface wave-speed perturbation
  extending tens of Mm beyond the sunspots, possibly associated with
  a convection cell driven by the local blockage of heat transport
  by the spots. A significant controversy still remains regarding the
  depth of the primary acoustic perturbation below sunspots. Modeling of
  scattering phase-shifts and seismic-imaging observations suggests that
  the perturbations are strongly concentrated within depths of a few Mm
  or less, in contrast to the deeper signatures implied by inversions of
  time-distance correlation measurements. Simple, but straightforward
  theoretical considerations, imply that the burden of proof rests
  with proponents of the latter scenario. Complexities introduced by
  the use of the photospheric signals within sunspots themselves also
  contribute to uncertainties in the interpretations. Careful control
  work and comparisons among diverse techniques, coupled with a continued
  theory-based effort in understanding and modeling local-helioseismic
  techniques and results, are crucial in providing a full understanding
  of the physics of solar active regions and their interaction with
  acoustic radiation.

---------------------------------------------------------
Title: Seismic images of the solar flare of July 9, 1996.
Authors: Donea, A. -C.; Braun, D. C.; Lindsey, C.
1999joso.proc..124D    Altcode:
  The helioseismic holography is a new method useful for rendering
  seismic images of the solar flare of July 9, 1996. Time series of the
  "egression power map" are computed in 2 mHz bands centered at 3.5
  mHz and 6 mHz. The images show an acoustic source associated with the
  flare some 18 mm in the N-S direction and approximately 15 mm in the
  E-W. The flare is rendered far more clearly in the 6 mHz band. The 6
  mHz flare signature lags the 3.5 mHz by approximately 6 minutes.

---------------------------------------------------------
Title: Phase-Sensitive Seismic Holography of the Photospheres and
    Near Subphotospheres of Active Regions
Authors: Lindsey, C.; Braun, D. C.
1999soho....9E..71L    Altcode:
  The discovery of acoustic power halos surrounding active regions by
  Braun, et al., Brown et al., and Toner and LaBonte, suggested that
  surface regions with weak magnetic fields were enhanced emitters of
  high-frequency seismic noise. Seismic holography of these regions
  by Lindsey and Braun showed clearly that this was not generally the
  case. Phase-sensitive holography of these features shows that these are
  regions in which the Doppler signatures of seismic waves from distant
  sources are locally enhanced, but the local seismic emission is not
  enhanced. On the other hand, acoustic glories are regions of strongly
  enhanced seismic emission from the quiet Sun just outside of magnetic
  regions. Moreover, regions of strong magnetic field show suppressed
  seismic emission. We examine the phase relation between the acoustic
  ingressions, acoustic egressions, and local acoustic amplitudes of
  these regions and consider how these can be treated as diagnostic of
  the photospheres and near subphotospheres of active regions.

---------------------------------------------------------
Title: Helioseismic Holography - a Technique for Understanding
    Solar Flares
Authors: Donea, A. C.; Lindsey, C.; Braun, D.
1999RoAJ....9S..71D    Altcode:
  The helioseismic holography is a technique which allows the analysis of
  the photosphere of the Sun from the point of view of the acoustics. In
  this paper we shall discuss mainly the seismic image of the flare of
  July 9, 1996 which produced the largest sunquake observed by MDI-SOHO
  instrument. We emphasize the fact that the kernel-like structure
  observed in the seismic signature at both 3.5 mHz and 6 mHz egression
  power maps are not side lobes effect. The seismic signature reveals
  the presence of an extended acoustic source, much larger than the
  Doppler redshift motion observed in the MDI-SOHO Dopplergrams.

---------------------------------------------------------
Title: Seismic Imaging of Acoustic Moats around Active Regions
Authors: Braun, D. C.; Lindsey, C.
1999soho....9E..46B    Altcode:
  Phase-correlation statistics comparing acoustic radiation coming out
  of a particular point on the solar photosphere with acoustic radiation
  going into it show considerably reduced sound travel times through the
  subphotospheres of active regions. This is already well established
  by scattering phase shifts of single sunspots by Braun and Fan, and
  by time-distance correlations measured by Duvall et al. We have now
  applied techniques in phase-sensitive seismic holography to obtain high
  resolution phase-correlation maps of active regions and the "acoustic
  moats" that surround them. Correlation maps obtained for several active
  regions show that the seismic perturbation manifested by the acoustic
  moats extends 30 Mm or so beyond the visible sunspots, and in large
  active-region complexes is quite predominate. Indeed, the acoustic moat
  surrounding the large active region complex NOAA AR 8179 (1998 March 15)
  manifests a one-way travel-time reduction of approximately 30s over an
  area of some 10,000 sq. Mm, encompassing all of the significant sunspots
  in the region. Onto this phase perturbation the major sunspots impose an
  additional localized contribution of about 30s. These results strongly
  reinforce an interpretation of the acoustic moat as a well integrated
  convection cell driven by the thermal perturbation that results from the
  local blockage of convective heat transport by the sunspot photosphere.

---------------------------------------------------------
Title: Acoustic Signatures of Subphotospheric Structure Underlying
    Sunspots
Authors: Lindsey, C.; Braun, D. C.
1998ApJ...509L.129L    Altcode:
  Helioseismic holography of active regions at frequencies in the
  range of 5-6 mHz renders acoustic signatures that we think signify
  acoustic perturbations several megameters beneath the photosphere. The
  application of holographic diagnostics at 5-6 mHz gives us images
  with considerably finer horizontal spatial resolution, and likewise
  much finer depth resolution with respect to focus, than the 3 mHz
  diagnostics we have recently published. This Letter reports comparative
  results of standard focus-defocus diagnostics of a single sunspot at 3
  and 6 mHz. Images of the “acoustic egression power” at 6 mHz show a
  remarkable, compact acoustic deficit that persists in acoustic focal
  planes submerged up to 11.2 Mm beneath the solar surface. We propose
  that this and other similar features associated with other active
  regions are the result of refraction or scattering by submerged thermal
  or Doppler perturbations of an acoustic deficit that is caused by strong
  wave absorption in the overlying photosphere of the active region.

---------------------------------------------------------
Title: Helioseismic Measurements of the Subsurface Meridional Flow
Authors: Braun, D. C.; Fan, Y.
1998ApJ...508L.105B    Altcode:
  We measure the mean frequencies of acoustic (p-mode) waves propagating
  toward and away from the poles of the Sun from observations made with
  the Solar Oscillations Investigation-Michelson Doppler Imager on board
  the Solar and Heliospheric Observatory and the ground-based Global
  Oscillations Network Group. We demonstrate that there is a significant
  frequency shift between poleward- and equatorward-traveling waves
  measured over solar latitudes 20°-60°, which is consistent with
  the Doppler effect of a poleward meridional flow on the order of 10 m
  s<SUP>-1</SUP>. From the variation of the frequency shifts of p-modes
  with degree l between 72 and 882 as a function of the lower turning
  point depth, we infer the speed of the meridional flow, averaged over
  these latitudes, over a range in depth extending over the top half
  of the solar convection zone. We find no evidence for a significant
  equatorward return flow within this depth range.

---------------------------------------------------------
Title: Seismic Holography of Solar Activity
Authors: Braun, D. C.; Lindsey, C.; Fan, Y.; Fagan, M.
1998ApJ...502..968B    Altcode:
  Helioseismic images of sunspots show a remarkable acoustic anomaly
  surrounding the sunspot. We applied the computational formalism of
  “helioseismic holography” to SOHO-MDI observations to render
  acoustic images of NOAA AR 7973, an active region containing a
  moderately large sunspot. The results of this study are based on
  simple “acoustic power holography,” to image the absorption of
  p-mode waves by the sunspot. These images clearly show a strong,
  compact acoustic deficit representing the sunspot, as well as plages
  in the neighborhood of the sunspot, consistent with earlier results of
  “Hankel analysis.” However, they also show surrounding the sunspot
  a conspicuous acoustic halo extending out to a radius of approximately
  35,000 km. We propose that this “acoustic moat” is the helioseismic
  manifestation of a single convection eddy that is driven by the thermal
  disturbance resulting from the local blockage of convective transport
  in the sunspot subphotosphere. Depth diagnostics based on acoustic
  focus show a rapidly defocusing sunspot image as the focal plane is
  submerged. Acoustic noise models in which absorption by the sunspot
  is entirely superficial yield images that defocus significantly more
  slowly with increasing focal-plane depth than the SOHO-MDI images of
  NOAA AR 7973. Extending the absorption significantly beneath the model
  photosphere enhances the discrepancy. More recent tests tentatively
  suggest that this “focus anomaly” is the result of neglect of image
  smearing introduced into the MDI instrument to suppress aliasing,
  and that a proper account of the instrumental MTF will render
  defocus profiles roughly consistent with superficial absorption. Our
  holographic images roughly indicate that the sunspot in NOAA AR 7973
  absorbs low-l waves with approximately the same efficiency as it does
  high-l waves. Contrary to widely held opinion, this result is entirely
  consistent with that of the Hankel analysis, given that the absorption
  of waves by magnetic regions is indeed superficial. We expect that the
  efficient absorption of low-l waves will make it possible to image large
  active regions on the far side of the Sun by the acoustic-absorption
  signatures they render at their antipodes.

---------------------------------------------------------
Title: The Acoustic Moat and Thermal Transport in the Neighborhoods
    of Sunspots
Authors: Lindsey, C.; Braun, D. C.
1998ApJ...499L..99L    Altcode:
  Helioseismic holography of sunspots shows a remarkable acoustic anomaly
  surrounding the sunspot, which we call an “acoustic moat.” We used
  Solar and Heliospheric Observatory (SOHO) Michelson Doppler Imager
  observations of NOAA Active Region 7973 to render acoustic images
  of a typical sunspot. These images show a conspicuous halo, 70,000
  km in diameter, surrounding the sunspot, in which there appears a
  predominant acoustic deficit. This “acoustic moat” may be terminated
  by a sharp outer boundary, which appears to circumscribe the sunspot
  completely in some instances. The outer boundary of the acoustic
  moat coincides conspicuously with plages in the neighborhood of the
  sunspot. Depth diagnostics based on acoustic focus suggest that the
  acoustic perturbations characterizing both the sunspot and the acoustic
  are predominantly superficial, within a few thousand kilometers of
  the solar surface. Following work by Meyer et al., we propose that
  the acoustic moat is the helioseismic manifestation of a single,
  integrated convection eddy that is driven by heat accumulation
  resulting from the local blockage of convective transport from the
  solar interior into the sunspot subphotosphere. We propose that the
  acoustic deficit predominantly characterizing the halo is the result
  of thermal refraction or Doppler scattering by the eddy outflow of an
  acoustic deficit originating in the helioseismic absorption by the
  nearby sunspot and possibly neighboring plages. With the advent of
  SOHO and the Global Oscillation Network Group, helioseismic holography
  promises considerable insight into the general subject of convective
  flows surrounding sunspots, an issue that is certain to be critical
  to the long-standing problem of thermal transport in the neighborhoods
  of sunspots.

---------------------------------------------------------
Title: The Seismology of Sunspots: A Comparison of Time-Distance
    and Frequency-Wavenumber Methods
Authors: Bogdan, T. J.; Braun, D. C.; Lites, B. W.; Thomas, John H.
1998ApJ...492..379B    Altcode:
  A pair of formulae are developed that relate the absorption coefficient
  and partial-wave phase shift concepts of frequency-wavenumber local
  helioseismology to the center-annulus cross-correlation function
  of time-distance helioseismology, under the general circumstances
  that both induced and spontaneous sunspot oscillations may be
  present. These formulae show that spontaneous emission of p-modes
  by magnetic and Reynolds stresses within the spot and the mode
  mixing between incoming and outgoing p-modes affect only the
  outgoing center-annulus cross-correlation time τ<SUP>+</SUP>,
  and they caution that real or spurious phase lags of the umbral
  oscillation signal lead to differences in the incoming and outgoing
  correlation times, resulting in τ<SUP>-</SUP> ≠ τ<SUP>+</SUP>. The
  application of these methods to actual helioseismic data obtained
  by the Global Oscillation Network Group (GONG) project is carried
  out in order to provide a tangible illustration of how time-distance
  and frequency-wavenumber ideas can profitably be combined to yield
  deeper insight into the seismic probing of sunspots. <P />By using the
  helioseismic GONG data in conjunction with concurrent observations of
  Doppler velocities and vector magnetic fields obtained by the High
  Altitude Observatory/National Solar Observatory (HAO/NSO) Advanced
  Stokes Polarimeter (ASP) for the 1995 October disk passage of active
  region NOAA 7912, we demonstrate that the inferred GONG umbral
  signal actually originates from the umbra-penumbra boundary about 6
  Mm distant from the center of the spot. Further, the ASP observations
  show that the 5 minute oscillations at the umbra-penumbra boundary lag
  behind those in the center of the umbra by approximately 1 minute,
  which is precisely the difference between the incoming and outgoing
  correlation times for NOAA 7912 recently determined by Braun. This
  remarkable result underscores the perils of using umbral oscillations
  in time-distance helioseismology, and it calls into question previous
  claims that correlation time differences constitute direct evidence
  for the existence of a steady downflow in and around sunspots. Taken
  together, the observational and theoretical evidence suggest that
  the p-mode forcing of the spot leads to the generation of upwardly
  propagating slow magnetoatmospheric waves. These waves are in turn
  responsible for the decreased amplitudes of the outwardly propagating
  p-modes in the surrounding quiet Sun, and the dispersion in their travel
  times between the hidden subsurface layer where they are forced and
  the overlying level where the Doppler signals originate leads to the
  observed phase lag between the umbral and penumbral oscillations and
  the corresponding correlation time differences. <P />This work utilizes
  data obtained by the Global Oscillations Network Group (GONG) project,
  managed by the National Solar Observatory, a Division of the National
  Optical Astronomy Observatories, which is operated by AURA, Inc.,
  under a cooperative agreement with the National Science Foundation.

---------------------------------------------------------
Title: Helioseismic Signatures of Subphotospheric Structure Beneath
    Active Regions
Authors: Lindsey, C.; Braun, D. C.
1998ESASP.418..641L    Altcode: 1998soho....6..641L
  No abstract at ADS

---------------------------------------------------------
Title: Time-Distance Sunspot Seismology with GONG Data
Authors: Braun, D. C.
1997ApJ...487..447B    Altcode:
  We present time-distance analyses of several active regions and a
  region of quiet Sun observed with the Global Oscillation Network Group
  (GONG). Analyzing temporal correlations between the p-mode oscillation
  signal observed within the sunspots with the signals integrated within
  surrounding annuli, we confirm the recent finding of Duvall and his
  colleagues that travel times (τ<SUP>+</SUP>) for outward propagating
  p-modes are smaller by approximately 1 minute than corresponding inward
  travel times (τ<SUP>-</SUP>). We also analyze correlations of the
  oscillation signal integrated within annuli of different radii. By
  varying the radius of the inner annulus (that which is closer to the
  target) we show that the radial extent of the region giving rise to
  the travel time perturbations is coincident with the outer boundary
  of the sunspot penumbrae. <P />A comparison of independent methods
  designed to determine the mean travel time perturbations of p-modes
  passing through the sunspots is made. We find the surprising result that
  time-distance correlations that do not utilize the signal within the
  sunspot itself (employing “two-skip” trajectories) yield mean travel
  times that differ substantially from the average of τ<SUP>+</SUP>
  and τ<SUP>-</SUP> and that are significantly closer in agreement
  with times predicted from scattering phase shifts measured by Hankel
  decomposition techniques. These observations suggest that it unlikely
  that Doppler shifts caused by subsurface flows are responsible for the
  travel time differences determined from center-annuli correlations
  targeted on sunspots. <P />This work utilizes data obtained by
  the Global Oscillation Network Group (GONG) project, managed by
  the National Solar Observatory, a Division of the National Optical
  Astronomy Observatories, which is operated by AURA, Inc., under a
  cooperative agreement with the National Science Foundation.

---------------------------------------------------------
Title: Helioseismic Holography
Authors: Lindsey, C.; Braun, D. C.
1997ApJ...485..895L    Altcode:
  We describe the basic principles of “helioseismic holography,” an
  analytic technique intended for local helioseismology of subsurface
  structure. The purpose of this technique is to provide depth
  discrimination of subsurface structure that manifests a surface
  signature in acoustic waves. It is based on the computational
  application of spatially resolved helioseismic observations to the
  surface of an acoustic model of the solar interior that contains no
  local structure. The observed surface oscillations are applied to
  the model in time reverse, and the model is then computationally
  sampled at various depths in its interior. This technique takes
  advantage of the coherence retained by waves in a smooth acoustic
  medium following an interaction with subsurface structure, allowing
  us to extrapolate the acoustic field with high accuracy to the depth
  where the structure lies. Depth discrimination is then accomplished by
  focus-defocus diagnostics. <P />We describe computational approaches
  to the technique from two different perspectives, the “spectral”
  and the “spatial.” For rigorous models of the solar interior,
  the computational demands of the spectral and spatial approaches are
  approximately the same. For diagnostics of relatively shallow structure,
  the plane-parallel approximation of the model is useful. In this case
  the spectral approach reduces computational holography essentially to
  Fourier transforms, which can be performed rapidly with very modest
  hardware. We illustrate the technique in this case, using artificial
  data characterizing waves in an idealized plane-parallel medium
  with acoustic absorbers located at various depths. <P />At present,
  we prefer to maintain a secure distinction between holography and
  modeling. While we do not discuss modeling in this paper, we think
  that it is important to develop an approach to modeling that takes
  advantage of holographic reconstruction. The prospect of viewing local
  subsurface magnetic regions and flows opens an entirely new dimension
  to helioseismology and to solar and stellar physics in general. It may
  make it possible to anticipate solar activity far in advance of its
  emergence to the surface. Local acoustic diagnostics could revolutionize
  our understanding of the solar dynamo and the 22 yr activity cycle.

---------------------------------------------------------
Title: The Seismology of Sunspots: A Comparison of Time-Distance
    and Frequency-Wavenumber Methods
Authors: Bogdan, T. J.; Braun, D. C.; Lites, B. W.; Thomas, J. H.
1997SPD....28.0210B    Altcode: 1997BAAS...29..894B
  A pair of formulae are developed which relate the absorption coefficient
  and partial wave phase-shift concepts of frequency-wavenumber local
  helioseismology to the center- annulus cross correlation function
  of time-distance helioseismology, under the general circumstances
  that both induced and spontaneous sunspot oscillations may be
  present. These formulae caution that real or spurious phase lags of
  the umbral oscillation signal lead to differences in the incoming and
  outgoing correlation times for sunspots, as first observed by Duvall
  et al. (1996, Nature, 379, 430) and recently confirmed by Braun (1997,
  ApJ, submitted). By using helioseismic data obtained by the GONG project
  in conjunction with concurrent observations of Doppler velocities and
  magnetic fields obtained by the HAO/NSO Advanced Stokes Polarimeter
  for the October 1995 disk passage of active region NOAA 7912, we
  demonstrate that the inferred GONG umbral oscillation signal actually
  originates from the umbra-penumbra boundary some 6 Mm distant from the
  center of the spot. Further, the ASP observations show that the 5-min
  oscillations at the umbra-penumbra boundary lag those in the center of
  the umbra by approximately 1 min, which is precisely the difference
  between the incoming and outgoing cross correlation times for NOAA
  7912 recently determined by Braun. The evidence suggests that p-mode
  forcing of the spot results in the generation of upward propagating
  slow MAG waves. These waves are responsible for the absorption of
  the p-modes, and the dispersion in their travel times between the
  subsurface layer where they are forced and the overlying level where
  the Doppler signals originate leads to the observed phase lag between
  the umbral and penumbral oscillations, and the corresponding correlation
  time differences.

---------------------------------------------------------
Title: Doppler Acoustic Diagnostics of Subsurface Solar Magnetic
    Structure
Authors: Lindsey, C.; Braun, D. C.; Jefferies, S. M.; Woodard, M. F.;
   Fan, Y.; Gu, Y.; Redfield, S.
1996ApJ...470..636L    Altcode:
  We used the Bartol-NSO-NASA South Pole helioseismic observations of 1991
  January to probe the subsurface structure of active regions to depths
  of ∼15,000 km. The helioseismic signature we particularly examine is
  intended to register acoustic Doppler effects caused by horizontal flows
  associated with the active region. We propose to show that the Doppler
  acoustic signature of horizontal flows is particularly well suited
  for deep subsurface diagnostics in terms of vertical discrimination
  of the structure. This study is based primarily on observations of
  NOAA Active Regions 6431, 6432, 6440, and 6442 between 1991 January
  1 and January 8. We interpret the acoustic signatures we find in
  terms of a general outflow of the solar medium surrounding the active
  region. The acoustic signatures are strongly dependent on wavenumber,
  which suggests an outflow that is quite weak near the surface, the upper
  4000 km of the subphotosphere, but which increases strongly with depth
  to velocities of several hundred meters per second at 15,000 km. This
  depth profile evolves rapidly as the active region matures. Young
  active regions show a strong outflow signature for waves that explore
  depths between 4000 and 8000 km. As the active region matures, the
  outflow vacates these intermediate layers and submerges to depths
  mostly below 8000 km. <P />We examine the location of AR 6442 for a
  possible preemergence signature. We also show evidence for extended,
  relatively superficial flows in the quiet Sun between the active region
  bands directed roughly into the active region bands.

---------------------------------------------------------
Title: Helioseismic Measurements of Subsurface Outflows From Sunspots
Authors: Braun, D. C.; Fan, Y.; Lindsey, C.; Jefferies, S. M.
1996AAS...188.6911B    Altcode: 1996BAAS...28Q.937B
  We measure the mean frequencies of acoustic waves propagating toward
  and away from sunspots employing a spot-centered Fourier-Hankel
  decomposition of p-mode amplitudes as measured from observations made at
  the South Pole in 1988 and 1991. There is a significant frequency shift
  between the inward and outward traveling waves which is consistent with
  the Doppler effect of a radial outflow from the sunspots. For p-modes
  of temporal frequencies of 3 mHz it is observed that the frequency
  shift decreases slightly with spatial frequency, for modes with degree
  l between 160 to 600. From the l dependence of the frequency shift, we
  infer that the mean radial outflow within the observed annular region
  (which extends between 30 and 137 Mm from the spots) increases nearly
  linearly with depth, reaching a magnitude of about 200 m/s at a depth
  of 20 Mm. This outflow exhibits properties similar to flows recently
  reported by Lindsey, et al. (1996 ApJ submitted) using spatially
  sensitive local helioseismic techniques. This work is supported by
  NSF Grant AST 9496171 and NASA Grant NAGW-4143.

---------------------------------------------------------
Title: Doppler Acoustic Diagnostics of Subsurface Solar Magnetic
    Structure
Authors: Lindsey, C.; Braun, D.; Jefferies, S.; Fan, Y.; Gu, Y.;
   Redfield, S.
1996AAS...188.7903L    Altcode: 1996BAAS...28R.955L
  We used the Bartol-NSO-NASA South Pole helioseismic observations of 1991
  January to study the subsurface structure of active regions to depths of
  ~ 15,000 km. The helioseismic signature we particularly examine is based
  on acoustic Doppler effects caused by horizontal flows associated with
  the active region. We demonstrate that the Doppler-acoustic signature
  of horizontal flows is particularly well suited for deep subsurface
  diagnostics in terms of vertical discrimination of the structure. This
  study is based primarily on observations of NOAA active regions 6431,
  6432, 6440 and 6442 between 1991 January 1 and January 8. We interpret
  the Doppler signatures we find in terms of a general outflow of the
  solar medium surrounding the active region. The existence of deep
  subsurface structure is indicated by the strong dependence of the
  Doppler signature on horizontal wavelength. The outflows in surface
  layers, the upper 4,000 km of the subphotosphere, are quite weak but
  increase strongly with depth to velocities of several hundred m/s at
  15,000 km. This depth profile evolves rapidly as the active region
  matures. Young active regions show strong outflows at depths between
  4,000 and 8,000 km. As the active region matures, the outflow vacates
  these intermediate layers and submerges to depths mostly below 8,000
  km. We examine the location of Region 6442 for a possible pre-emergence
  signature. We also show strong evidence for extended, relatively
  superficial flows in the quiet Sun between the active-region bands
  directed roughly into the active region bands.

---------------------------------------------------------
Title: Diagnostics of a Subsurface Radial Outflow From a Sunspot
Authors: Braun, D. C.; Fan, Y.; Lindsey, C.; Jefferies, S. M.
1996astro.ph..3078B    Altcode:
  We measure the mean frequencies of acoustic waves propagating toward
  and away from a sunspot employing a spot-centered Fourier-Hankel
  decomposition of p-mode amplitudes as measured from a set of
  observations made at the South Pole in 1991. We demonstrate that
  there is a significant frequency shift between the inward and outward
  traveling waves which is consistent with the Doppler effect of a radial
  outflow from the sunspot. For p-modes of temporal frequencies of 3
  mHz it is observed that the frequency shift decreases slightly with
  spatial frequency, for modes with degree l between 160 to 600. From
  the l dependence of the frequency shift, we infer that the mean radial
  outflow within the observed annular region (which extends between 30 and
  137 Mm from the spot) increases nearly linearly with depth, reaching a
  magnitude of about 200 m/s at a depth of 20 Mm. This outflow exhibits
  properties similar to flows recently reported by Lindsey, et al. (1996)
  using spatially sensitive local helioseismic techniques.

---------------------------------------------------------
Title: Scattering of p-Modes by Sunspots. II. Calculations of Phase
    Shifts from a Phenomenological Model
Authors: Fan, Y.; Braun, D. C.; Chou, D. -Y.
1995ApJ...451..877F    Altcode:
  We model the scattering of p-mode waves in a polytropic atmosphere
  by localized inhomogeneities in wave speed, pressure, and density
  of the medium. The effect of the inhomogeneities is attributed to
  a source term in the pressure wave equation. The inhomogeneous wave
  equation for the scattered waves is solved under the simplification
  of the Born approximation. From the solution for the scattered waves,
  we compute the phase shifts between the incoming and outgoing waves of
  individual modes. <P />We find that the variations of the computed
  phase shifts with degree l and radial order n of the modes show
  different behavior for inhomogeneities with different characteristic
  depths. Depths significantly shallower than the depth of the modes
  seem to show a phase shift dependence on l and n that is similar to
  the qualitative behavior of the observed phase shifts produced by
  sunspots. Direct quantitative comparison of the computed phase shifts
  with observations is limited to modes with lower degree (l &lt; 200)
  in which the observed phase shifts are reasonably small so that the
  Born approximation is applicable. We find that for inhomogeneities
  with a wave speed contrast reasonable for sunspots, occupying a volume
  described by a characteristic depth D 108 cm and horizontal radius R ≍
  2.5 × 10<SUP>9</SUP> cm, the computed phase shifts at lower l range
  are in agreement with the observed phase shifts from sunspots in both
  their magnitudes as well as their variation with l and frequency (or n).

---------------------------------------------------------
Title: Scattering of p-Modes by Sunspots. I. Observations
Authors: Braun, D. C.
1995ApJ...451..859B    Altcode:
  The acoustic scattering properties of two large sunspots and a plage are
  determined from a Fourier-Hankel decomposition of p-mode amplitudes as
  measured from 68 hr subsets of a larger set of observations made at the
  South Pole in 1988. We present measurements of p-mode absorption and
  scattering phase shifts as functions of the incident mode properties
  (degree, radial order, and azimuthal order). <P />In the two sunspots
  we observe a distinct modulation of the absorption with temporal
  frequency in a fashion that is very nearly independent of the degree
  of the mode. In particular, the absorption exhibits a broad peak at 3
  mHz, an absence of absorption at 5 mHz, and a rise in absorption at
  higher temporal frequencies. This variation is in good qualitative
  agreement with a prediction of a model of p-mode absorption by slow
  mode conversion described recently by Spruit &amp; Bogdan (see also
  the recent work of Cally &amp; Bogdan). The spotless plage also shows
  significant p-mode absorption, at a level of 20% of the value seen in
  the spots. Control tests made by repeating the analysis in a region of
  quiet Sun have confirmed the recent observation by Bogdan et al. that
  the quiet Sun shows an apparent acoustic emission. In particular, we
  find a significant anticorrelation between the absorption coefficient
  in the quiet Sun and the values measured in a nearby sunspot. <P />The
  scattering phase shifts are shown to increase with the degree of the
  modes with an increase that is faster than a linear relation. At
  constant degree the phase shifts increase with temporal frequency
  (radial order) before leveling off at a roughly constant value. We
  suggest that this behavior is consistent with a relatively shallow
  sound-speed perturbation produced by the spots. The variation of
  the phase shift and the absorption with azimuthal order suggest
  that the phase shifts are largely produced within the area of the
  sunspot, while significant absorption is occurring in a more extended
  region. Related to this observation is the finding that the plage,
  while absorbing p-modes, produces no measurable phase shifts. Upper
  limits place any phase shifts caused by the plage to be less than
  about 5 % of that observed in the spots. <P />Finally, we find strong
  evidence of mode mixing in the two sunspots, as demonstrated by a
  significant correlation of the phases of incident p-modes of a given
  radial order with the phases of outgoing modes of adjacent orders at
  the same temporal frequency.

---------------------------------------------------------
Title: Observations and Models of p-Mode Scattering by Sunspots
Authors: Braun, D. C.; Fan, Y.
1995SPD....26..403B    Altcode: 1995BAAS...27..954B
  No abstract at ADS

---------------------------------------------------------
Title: Active Region Seismology
Authors: Bogdan, T. J.; Braun, D. C.
1995ESASP.376a..31B    Altcode: 1995heli.conf...31B; 1995soho....1...31B
  Active region seismology is concerned with the determination and
  interpretation of the interaction of the solar acoustic oscillations
  with near-surface target structures, such as magnetic flux
  concentrations, sunspots, and plages. Observations with high spatial
  resolution and long temporal duration have enabled the measurement
  of the scattering matrix for sunspots and solar active regions as a
  function of the mode properties (wavenumber, frequency and azimuthal
  order). From this information one may determine the amount of p-mode
  absorption, partial-wave phase shift, and mode mixing introduced by
  the sunspot. In addition, the possibility of detecting the presence of
  completely submerged magnetic fields has been raised and new procedures
  for performing acoustic holography of the solar interior are being
  developed. The accumulating evidence points to the mode conversion of
  p-modes to various magneto-atmospheric waves within the magnetic flux
  concentration as the unifying physical mechanism responsible for these
  diverse phenomena.

---------------------------------------------------------
Title: Sunspot Seismology: New Observations and Prospects
Authors: Braun, D. C.
1995ASPC...76..250B    Altcode: 1995gong.conf..250B
  No abstract at ADS

---------------------------------------------------------
Title: A Model of P-mode Scattering by Sunspots
Authors: Fan, Y.; Braun, D. C.
1994AAS...185.4406F    Altcode: 1994BAAS...26.1377F
  It has recently been discovered that sunspots scatter intermediate and
  high-degree p-modes. The scattering may be characterized by a shift
  in phase between modes travelling toward and away from the spot. These
  observations offer the hope that suitable models of the scattering may
  yield important clues about the subsurface evolution and structure
  of magnetic regions. We model the scattering of p-mode waves in a
  polytropic atmosphere by localized inhomogeneities in compressibility
  (the wave speed), density and pressure of the media. The effect of the
  inhomogeneities is to introduce a source term in the pressure wave
  equation. We solve this inhomogeneous equation for the scattered
  wave amplitudes using standard Green's function techniques under
  the simplification of the Born approximation. We found that with
  reasonable strength (or contrast) of the inhomogeneities we can
  obtain phase shifts between the outgoing and the in-going waves
  similar to observations of p-modes in both the magnitude and degree
  (l) dependence. We discuss how the strength of the scattered waves may
  depend on the depth distribution of the inhomogeneities. This work is
  supported by a NSF grant AST-9496171 and NASA grant NAGW-4143 awarded
  to DCB. YF is supported by ONR grant N00014-91-J-1040.

---------------------------------------------------------
Title: An active solar prominence in 1.3 MM radiation
Authors: Harrison, R. A.; Carter, M. K.; Clark, T. A.; Lindsey, C.;
   Jefferies, J. T.; Sime, D. G.; Watt, G.; Roellig, T. L.; Becklin,
   E. E.; Naylor, D. A.; Tompkins, G. J.; Braun, D.
1993A&A...274L...9H    Altcode:
  We present new millimetre-wavelength observations of an active solar
  prominence. Observations made over a two-day period with the James
  Clerk Maxwell Telescope on Manna Kea, Hawaii, give a unique view in
  1.3 mm radiation of the spectacular prominence that appeared on the
  west solar limb in the total solar eclipse of 11 July 1991.

---------------------------------------------------------
Title: Prospects in Helioseismic Holography
Authors: Lindsey, C. A.; Braun, D. C.; Jefferies, S. M.
1993BAAS...25.1220L    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: The P-Mode Scattering Properties of a Sunspot
Authors: Braun, D. C.; Labonte, B. J.; Duvall, T. L., Jr.; Jefferies,
   S. M.; Harvey, M. A.; Pomerantz, J. W.
1993ASPC...42...77B    Altcode: 1993gong.conf...77B
  No abstract at ADS

---------------------------------------------------------
Title: Local Helioseismology of Subsurface Structure
Authors: Lindsey, C.; Braun, D. C.; Jefferies, S. M.
1993ASPC...42...81L    Altcode: 1993gong.conf...81L
  No abstract at ADS

---------------------------------------------------------
Title: Measurement of the Height of the Solar CO Layer During the
    11 July 1991 Eclipse
Authors: Clark, T. A.; Naylor, D. A.; Tompkins, G. J.; Lindsey, C. A.;
   Becklin, E. E.; Jefferies, J. T.; Harrison, R. A.; Roellig, T. L.;
   Carter, M.; Braun, D. C.; Watt, G.
1992AAS...181.8108C    Altcode: 1992BAAS...24.1253C
  No abstract at ADS

---------------------------------------------------------
Title: Extreme-infrared brightness profile of the solar chromosphere
    obtained during the total eclipse of 1991
Authors: Lindsey, C.; Jefferies, J. T.; Clark, T. A.; Harrison, R. A.;
   Carter, M. K.; Watt, G.; Becklin, E. E.; Roellig, T. L.; Braun, D. C.;
   Naylor, D. A.
1992Natur.358..308L    Altcode:
  THE solar chromosphere is a thin layer of gas that is several thousand
  degrees hotter than the underlying photosphere, and responsible for
  most of the Sun's ultraviolet emission. The mechanism by which it is
  heated to temperatures exceeding 10,000 K is not understood. Millimetre
  and submillimetre radiometry can be used to obtain the chromospheric
  temperature profile, but the diffraction-limited resolution for the
  largest telescopes is at best 17 arcsec, or ~12,500 km at the Sun's
  distance. This is greater than the thickness of the quiet chromosphere
  itself. The total eclipse of July 1991, which passed over the Mauna
  Kea Observatory in Hawaii, provided a rare opportunity to make limb
  occultation observations with a large submillimetrewavelength telescope,
  the 15-m James Clerk Maxwell Telescope, and in this way we obtained a
  temperature profile in 1.3-mm radiation with ~300 km resolution at the
  Sun. Our observations indicate that spicules (magnetically entrained
  funnels of gas) reach a temperature of 8,000 K at 3,000-4,000 km above
  the photosphere, a temperature lower than those of many spicule models.

---------------------------------------------------------
Title: Local Acoustic Diagnostics of the Solar Interior
Authors: Braun, D. C.; Lindsey, C.; Fan, Y.; Jefferies, S. M.
1992ApJ...392..739B    Altcode:
  Two diagnostic utilities, acoustic power maps, and surface acoustic
  flux maps are used to explore the local diagnostics of magnetic field
  structure in the solar interior. The acoustic power maps, constructed
  from 50 hr of continuous K-line intensity images, show three general
  features: acoustic power deficits at 3 mHz corresponding to surface
  magnetic flux, acoustic power enhancements at 6 mHz surrounding the
  exterior of magnetic regions, and occasional power deficits at 3 mHz
  which extend beyond magnetic regions visible on the surface to regions
  of quiet-sun. Surface acoustic flux vector maps of two active regions
  were constructed for two 6-hr time-series of Dopplergrams. Both maps
  show the divergence of 3-mHz acoustic flux into surface magnetic
  structures and also sources and sinks of wave energy which are not
  associated with surface features.

---------------------------------------------------------
Title: Scattering of p-Modes by a Sunspot
Authors: Braun, D. C.; Duvall, T. L., Jr.; Labonte, B. J.; Jefferies,
   S. M.; Harvey, J. W.; Pomerantz, M. A.
1992ApJ...391L.113B    Altcode:
  The acoustic scattering properties of a large sunspot are determined
  from a Fourier-Hankel decomposition of p-mode amplitudes as measured
  from a 68-hr subset of a larger set of observations made at the
  South Pole in 1988. It is shown that significant improvement in the
  measurement of p-mode scattering amplitudes results from the increased
  temporal frequency resolution provided by these data. Scattering
  phase shifts are unambiguously determined for the first time, and the
  dependence of the p-mode phase shift and absorption with wavenumber
  and frequency is presented.

---------------------------------------------------------
Title: Prospects in Acoustic Holography of the Solar Interior
Authors: Lindsey, C.; Braun, D. C.; Fan, Y.; Jefferies, S. M.
1992AAS...180.1703L    Altcode: 1992BAAS...24..753L
  Acoustic power maps of the solar surface show strong evidence
  of magnetic structure crossing the solar equator not far beneath
  the photosphere to connect the active latitude bands. These maps,
  generated using the Bartol-NSO-NASA South Pole Observations show long
  finger-like acoustic shadows we think are caused by absorption of
  acoustic energy by the submerged magnetic structure. These features
  suggest a solar interior magnetic structure quite different from any
  previously expected. These new results open the prospect of a new and
  powerful solar interior diagnostic based on acoustic holography.

---------------------------------------------------------
Title: Scattering of p-Modes by a Sunspot
Authors: Braun, D. C.; Duvall, T. L., Jr.; Labonte, B. J.; Jefferies,
   S. M.; Harvey, J. W.; Pomerantz, M. A.
1992AAS...180.0604B    Altcode: 1992BAAS...24..737B
  For the first time the scattering phase shifts of solar p-modes
  from a sunspot have been unambiguously determined. This is made
  possible by the recent availability of long duration, high duty
  cycle observations. The results presented here are determined from a
  Fourier-Hankel decomposition of p-mode amplitudes as measured from a
  68 hr subset of a larger set of observations made at the South Pole in
  1988. In addition to the detection of the phase shifts, the quality of
  the data allows the dependence of the p-mode scattering and absorption
  with azimuthal order, spatial wavenumber and temporal frequency to
  be independently determined. Thus, unlike previous observations, our
  measurements of absorption and phase shifts do not represent averages
  over a range of p-modes. With this information we have for the first
  time a complete description of the acoustic scattering amplitudes
  from a large sunspot. Interpretation of these observations requires a
  suitable theory of the interaction of p-modes and sunspots. However,
  with the complete scattering amplitudes now available one may apply
  inverse scattering algorithms, based on a few simplifying assumptions,
  to deduce a 3-dimensional map of the scattering strength of the active
  region. This offers the hope that general information about subsurface
  morphology of active regions might be gained even without a detailed
  understanding of the physical scattering processes involved. DCB is
  supported by Air Force URI grant AFOSR-90-0116. The South Pole program
  is supported in part by National Science Foundation grants DPP87-15791
  and 89-17626, and by the Solar Physics Branch of the Space Physics
  Division of NASA.

---------------------------------------------------------
Title: Power Spectra of Solar Convection
Authors: Chou, D. -Y.; Labonte, B. J.; Braun, D. C.; Duvall, T. L., Jr.
1991ApJ...372..314C    Altcode:
  The properties of convective motions on the sun are studied using
  Kitt Peak Doppler images and power spectra of convection. The
  power peaks at a scale of about 29,000 km and drops off smoothly
  with wavenumber. There is no evidence of apparent energy excess at
  the scale of the mesogranulation proposed by other authors. The
  vertical and horizontal power for each wavenumber are obtained
  and used to calculate the vertical and horizontal velocities of the
  supergranulation. The amplitude of vertical and horizontal velocities
  of the supergranulation are 0.034 (+ or - 0.002) km/s and 0.38 (+ or -
  0.01) km/s, respectively. The corresponding rms values are 0.024 (+
  or - 0.002) km/s and 0.27 (+ or - 0.01) km/s.

---------------------------------------------------------
Title: An Acoustic Poynting Vector for Solar p-mode Oscillations
Authors: Braun, D. C.; Lindsey, C.
1991BAAS...23.1049B    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: p-mode absorption in the giant active region of 10 March, 1989
Authors: Braun, D. C.; Duvall, T. L., Jr.
1990SoPh..129...83B    Altcode:
  A time series of velocity oscillations is observed in the vicinity of
  NOAA region 5395 with the Kitt Peak vacuum telescope for 6.8 hours on
  1989 March 10 as part of a program to study the interaction of solar
  p-mode oscillations with solar active regions. The data is transformed
  in a cylindrical coordinate system centered on the visible sunspot,
  then Hankel- and Fourier-transformed to produce the power spectra of in-
  and outgoing acoustic waves. It is observed that a maximum of nearly 70%
  of the power of incident high-degree modes is absorbed by this unusually
  large sunspot group. The absorptive properties of this active region
  are compared with those of more typical regions studied previously.

---------------------------------------------------------
Title: The Spatial Distribution of p-Mode Absorption in Active Regions
Authors: Braun, D. C.; Labonte, B. J.; Duvall, T. L., Jr.
1990ApJ...354..372B    Altcode:
  The interaction of solar p-mode waves and active regions
  has been the subject of recent observational and theoretical
  investigations. Observations show that up to one-half of the power
  of incident high-degree acoustic may be absorbed in and around
  sunspots. In this paper the horizontal spatial distribution of
  high-degree p-mode absorption in solar active regions is explored. An
  appropriate Fourier-Hankel transform can be used to detect the mean
  absorption of waves passing through any given point on the solar
  surface. By repeating the analysis at multiple positions a map of the
  absorption can be constructed. A technique for optimal computation of
  absorption maps is developed and applied to observations of several
  active regions and an area of quiet sun near disk center. By comparing
  the distribution of p-mode absorption with magnetograms and line-wing
  intensity images, it is directly observed that the absorption is not
  limited to the location of the visible sunspots but is also associated
  with magnetic fields in the surrounding plage. It is estimated that the
  absorption efficiency scales roughly with the magnetic flux density,
  although the absorption appears to saturate inside the strongest fields.

---------------------------------------------------------
Title: Helioseismic Imaging of Sunspots at Their Antipodes
Authors: Lindsey, Charles; Braun, Douglas C.
1990SoPh..126..101L    Altcode:
  Recent work by Braun, Duvall, and LaBonte has shown that sunspots absorb
  helioseismic waves. We propose that sunspot absorption causes a seismic
  deficit that should be imaged at the antipode of the sunspot. If these
  images are observable, it should be possible to produce seismic maps
  of magnetic regions on the far side of the Sun. This possibility opens
  a broad range of synoptic and diagnostic applications. Diagnostic
  applications would include lifetimes of higher-frequency modes, and
  possibly rotation of the solar interior and detection of subsurface
  magnetic structure. We outline elements of the theory of seismic
  imaging and consider some applications. We propose the extention of
  acoustic holography to solar interior diagnostics in the context of
  antipodal imaging.

---------------------------------------------------------
Title: Far-Infrared Intensity Variations Caused by 5 Minute
    Oscillations
Authors: Lindsey, C.; Kopp, G.; Becklin, E. E.; Roellig, T.; Werner,
   M. W.; Jefferies, J. T.; Orrall, F. Q.; Braun, D.; Mickey, D. L.
1990ApJ...350..475L    Altcode:
  Observations of solar IR intensity variations at 50, 100, and
  200 microns were made simultaneously and cospatially with Doppler
  measurements in the sodium D1 line at 5896 A. Brightness temperature
  variations of several K in amplitude are highly correlated with five
  minute Doppler oscillations. The brightness variations are attributed
  to work done on the chromospheric medium by compression, driven by the
  five minute oscillations. The Doppler oscillations lead the brightness
  variations by about 47 deg in phase at 50 and 100 microns and by about
  72 deg in phase at 200 microns.

---------------------------------------------------------
Title: Observations of p-Mode Absorption in Active Regions
Authors: Braun, D. C.; Duvall, T. L., Jr.; Jefferies, S. M.
1990LNP...367..181B    Altcode: 1990psss.conf..181B
  We present here a summary of results on the interaction of p-modes with
  solar active regions based on observations made at the Kitt Peak Solar
  Vacuum Telescope and the geographic South Pole. A travelling wave
  decomposition of p-modes is performed in a cylindrical coordinate
  system centered on the active regions. Significant absorption of
  p-mode wave power is observed to occur in all of the regions and
  is a function of horizontal wavenumber () - increasing linearly
  with k up to some maximum value and remaining constant for higher
  wavenumbers. The maximum fractional absorption of incident power
  is about 0.2 for small pores and 0.4 for typical isolated sunspots
  (radius = 15 Mm). A maximum of 70% absorption is seen in the large
  sunspot group of March 1989 (radius = 60 Mm). No convincing variation
  of the absorption with temporal frequency (i.e. radial order) is seen,
  although not entirely ruled out considering the relative errors involved
  with the power measurements. No significant difference in the amount
  of p-mode absorption is detected between equal 3-hour time intervals
  before and after a class X4 flare in the March 1989 region. No excess
  of outgoing waves following the time of the flare is detected. These
  observations do not support the suggestion that large flares may excite
  observable acoustic waves in the photosphere.

---------------------------------------------------------
Title: The interaction of high-degree p-mode oscillations with solar
    active regions
Authors: Braun, Douglas C Doug
1988PhDT.......201B    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: The Absorption of High-Degree p-Mode Oscillations in and
    around Sunspots
Authors: Braun, D. C.; Duvall, T. L., Jr.; Labonte, B. J.
1988ApJ...335.1015B    Altcode:
  The direct interaction of p-modes and sunspots is investigated in
  four observed active regions using a partial wave analysis in a
  cylindrical coordinate system centered on the spots. Up to half the
  power of incident p-modes is absorbed by the sunspots. By measuring
  the magnitude of absorption as a function of horizontal wavenumber
  and azimuthal order the authors have determined that the absorption is
  not only from the umbrae of the spots but is also significant within
  the penumbrae, and in some cases it appears to be associated with the
  presence of extended magnetic fields surrounding the sunspots. The
  amount of p-mode energy removed by magnetic fields is estimated for
  each of the regions observed.

---------------------------------------------------------
Title: Tomography of Solar Active Regions
Authors: Braun, D. C.; Labonte, B. J.; Duvall, T. L., Jr.
1988BAAS...20..701B    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: A Solar Chromosphere and Spicule Model Based on Far-Infrared
    Limb Observations
Authors: Braun, D.; Lindsey, C.
1987ApJ...320..898B    Altcode:
  Techniques developed for LTE radiative transfer problems in a rough
  atmosphere were used to compute a model chromosphere containing spicules
  consistent with high-resolution solar limb observations from 100 microns
  to 2.6 mm. The model consists of a smooth, plane-parallel temperature
  minimum region extending from the photosphere to a height of 1000 km
  and randomly distributed cylindrical spicules above this height. It
  is found that the observed limb brightness profiles are well fitted
  by spicules with electron temperatures on the order of 7000 K.

---------------------------------------------------------
Title: Acoustic Absorption by Sunspots
Authors: Braun, D. C.; Duvall, T. L., Jr.; Labonte, B. J.
1987ApJ...319L..27B    Altcode:
  The paper presents the initial results of a series of observations
  designed to probe the nature of sunspots by detecting their influence
  on high-degree p-mode oscillations in the surrounding photosphere. The
  analysis decomposes the observed oscillations into radially propagating
  waves described by Hankel functions in a cylindrical coordinate system
  centered on the sunspot. From measurements of the differences in power
  between waves traveling outward and inward, it is demonstrated that
  sunspots appear to absorb as much as 50 percent of the incoming acoustic
  waves. It is found that for all three sunspots observed, the amount of
  absorption increases linearly with horizontal wavenumber. The effect
  is present in p-mode oscillations with wavelengths both significantly
  larger and smaller than the diameter of the sunspot umbrae. Actual
  absorption of acoustic energy of the magnitude observed may produce
  measurable decreases in the power and lifetimes of high-degree p-mode
  oscillations during periods of high solar activity.

---------------------------------------------------------
Title: The Absorption of 5-Minute Oscillations by Sunspots
Authors: Braun, D. C.; Labonte, B. J.; Duvall, T. L., Jr.
1987BAAS...19..936B    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: Sunspots as Sinks of P-Mode Wave Energy
Authors: Duvall, T. L., Jr.; Harvey, J. W.; Braun, D. C.; Labonte,
   B. J.; Pomerantz, M. A.
1987BAAS...19R.934D    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: The Solar Irradiance From January to February, 1981
Authors: Braun, D. C.; Labonte, B. J.
1985BAAS...17..756B    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: Observations of the Ca II K spectral line in He 10830 Å
    dark points.
Authors: Holt, R.; Fortune, N.; Braun, D.; Mullan, D.
1985BAAS...17..760H    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: Observations of the Ca II K spectral line in He 10830 Å
    dark points.
Authors: Holt, R.; Fortune, N.; Braun, D.; Mullan, D.
1985BAAS...17..933H    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: Planet Size Stars or Star Size Planets
Authors: McCarthy, D.; Low, F.; Kleinmann, S.; Lippincott, S. L.;
   Braun, D.
1983S&T....66..114M    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: Astrometric and infrared speckle analysis of the visually
    unresolved binary BD +41 328.
Authors: Lippincott, S. L.; Braun, D.; McCarthy, D. W., Jr.
1983PASP...95..271L    Altcode:
  BD +41°328 (PCC 372), a solar-type 5th magnitude star at a distance of
  14 parsecs was discovered to have an unseen companion from proper-motion
  analysis of astrometric plates taken with the Sproul 61-cm refractor,
  thus excluding it as a candidate for a solar planetary-type system. The
  combination of an improved photocentric orbit from recent astrometry and
  measurement of the companion's separation and brightness by infrared
  speckle interferometry at 2.2 microns indicates that the companion is
  a red dwarf with a mass of 0.38 ± 0.07M<SUB>sun</SUB>. It revolves
  around the primary with a period of 19.5 years and a semimajor axis
  of 8.9 ± 0.5 AU.