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Author name code: getling
ADS astronomy entries on 2022-09-14
author:"Getling, Alexander" 

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Title: Spatial Scales and Time Variation of Solar Subsurface
    Convection
Authors: Getling, Alexander V.; Kosovichev, Alexander G.
2022arXiv220804642G    Altcode:
  Spectral analysis of the spatial structure of solar subphotospheric
  convection is carried out for subsurface flow maps constructed
  using the time--distance helioseismological technique. The source
  data are obtained from the Helioseismic and Magnetic Imager
  (HMI) onboard Solar Dynamics Observatory (SDO) from 2010 May to
  2020 September. A spherical-harmonic transform is applied to the
  horizontal-velocity-divergence field at depths from 0 to 19~Mm. The
  range of flow scales is fairly broad in shallow layers and narrows
  as the depth increases. The horizontal flow scales rapidly increase
  with depth, from supergranulation to giant-cell values, and indicate
  the existence of large-scale convective motions in the near-surface
  shear layer. The results can naturally be interpreted in terms of
  a superposition of differently scaled flows localized in different
  depth intervals. There is some tendency toward the emergence of
  meridionally elongated (banana-shaped) convection structures in the
  deep layers. The total power of convective flows is anticorrelated
  with the sunspot-number variation over the solar activity cycle in
  shallow subsurface layers and positively correlated at larger depths,
  which is suggestive of the depth redistribution of the convective-flow
  energy due to the action of magnetic fields.

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Title: Helioseismic Monitoring of Solar Subsurface Dynamics and
    Activity
Authors: Kosovichev, Alexander; Pipin, Valery; Getling, Alexander;
   Stejko, Andrey; Stefan, John; Guerrero, Gustavo
2022cosp...44.3215K    Altcode:
  Uninterrupted helioseismic data from Michelson Doppler Imager (MDI)
  onboard Solar and Heliospheric Observatory (SoHO) and from Helioseismic
  and Magnetic Imager (HMI) onboard Solar Dynamics Observatory (SDO)
  have provided unique information about flows and structures evolving
  on various temporal and spatial scales inside the Sun. The data
  cover the past two solar cycles and the rising phase of the current
  solar cycle. In particular, our analysis of variations of the internal
  differential rotation reveals "extended" cyclic variations of migrating
  zonal flows ("torsional oscillations") through the whole convection
  zone. The observed patterns of subsurface flow acceleration provide
  evidence of hydromagnetic dynamo waves, which control the strength
  of sunspot cycles, and potentially carry information about the future
  solar cycles. Similarly, "extended" cyclic variations of the subsurface
  meridional circulation, detected by local helioseismic techniques,
  reflect the evolution of subsurface magnetic fields and emerging
  magnetic flux. Furthermore, to monitor emerging active regions, we
  develop a "deep-focus" helioseismic diagnostics, which allows us to
  detect large emerging active regions before they become visible on
  the surface. We present recent advances in helioseismic monitoring
  of solar activity and discuss helioseismic constraints on models of
  global solar variability and space weather forecasting.

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Title: Advances and Challenges in Observations and Modeling of the
    Global-Sun Dynamics and Dynamo
Authors: Kosovichev, A. G.; Guerrero, G.; Stejko, A. M.; Pipin, V. V.;
   Getling, A. V.
2022arXiv220310721K    Altcode:
  Computational heliophysics has shed light on the fundamental physical
  processes inside the Sun, such as the differential rotation, meridional
  circulation, and dynamo-generation of magnetic fields. However,
  despite the substantial advances, the current results of 3D MHD
  simulations are still far from reproducing helioseismic inferences
  and surface observations. The reason is the multi-scale nature of
  the solar dynamics, covering a vast range of scales, which cannot be
  solved with the current computational resources. In such a situation,
  significant progress has been achieved by the mean-field approach,
  based on the separation of small-scale turbulence and large-scale
  dynamics. The mean-field simulations can reproduce solar observations,
  qualitatively and quantitatively, and uncover new phenomena. However,
  they do not reveal the complex physics of large-scale convection,
  solar magnetic cycles, and the magnetic self-organization that causes
  sunspots and solar eruptions. Thus, developing a synergy of these
  approaches seems to be a necessary but very challenging task.

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Title: Spatial Spectrum of Solar Convection from Helioseismic Data:
    Flow Scales and Time Variations
Authors: Getling, Alexander V.; Kosovichev, Alexander G.
2022arXiv220100638G    Altcode:
  We analyze spectral properties of solar convection in the range of
  depths from 0 to 19~Mm using subsurface flow maps obtained by the
  time-distance heiioseismology analysis of solar-oscillation data from
  the Helioseismic and Magnetic Imager (HMI) onboard Solar Dynamics
  Observatory (SDO) from May 2010 to September 2020. The results reveal
  a rapid increase of the horizontal flow scales with the depth, from
  supergranulation to giant-cell scales, and support the evidence of
  large-scale convection, previously detected by tracking the motion of
  supergranular cells on the surface. The total power of convective flows
  correlates with the solar activity cycle. During the solar maximum,
  the total power decreases in shallow subsurface layers and increases
  in the deeper layers.

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Title: Large-Scale Dynamics of Solar Subsurface Shear Layer:
    Theoretical Predictions and Helioseismic Inferences
Authors: Kosovichev, Alexander; Getling, Alexander; Guerrero, Gustavo;
   Pipin, Valery; Stejko, Andrey
2021AGUFMSH53C..03K    Altcode:
  Helioseismic observations show that the solar rotation rate sharply
  increases with depth in the outer 30 Mm-deep layers of the solar
  convection zone. This subsurface shear layer (SSL) plays a critical role
  in the formation of migrating activity belts (the butterfly diagram)
  and the emergence of active regions. Measurements of the rotation
  rate indicate that the magnetic field of sunspots and active regions
  is anchored in the subsurface shear layer. The magnetic structure of
  the SSL has not been directly measured by helioseismology, but it can
  be inferred by comparing variations of subsurface flows and sound-speed
  variations predicted by dynamo models with helioseismic measurements. To
  establish the connections between the flows and fields, we construct
  and analyze synoptic maps of subsurface flows in the SSL, obtained
  from time-distance helioseismic inversion during the whole Solar Cycle
  24 and the rising phase of Cycle 25. The results reveal the extended
  solar-cycle pattern of variations of the meridional circulation,
  predicted by the dynamo models and previously known from surface and
  subsurface observations of zonal flows. We discuss the origin of the
  observed variations and their links to the magnetism and dynamics of
  the subsurface shear layer.

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Title: Multiscale Organization of Turbulent Convection in Global-Sun
    Simulations
Authors: Guerrero, Gustavo; Stejko, Andrey; Kosovichev, Alexander;
   Getling, Alexander; Smolarkiewicz, Piotr
2021AGUFMSH55D1885G    Altcode:
  Solar convection is at the core of fundamental phenomena such as
  differential rotation and meridional circulation and, ultimately, the
  solar dynamo. The governing mechanisms, amplitude, and dominant scales
  of convection in the solar interior remain under debate. Furthermore,
  the large Reynolds and Rayleigh numbers involved make it implausible
  to resolve all relevant scales using direct numerical simulation. In
  this work, we study solar convection through global, non-rotating, and
  non-magnetic implicit large-eddy simulations (ILES), using the 3D global
  hydrodynamic code EULAG. Our simulations exhibit a pattern of multiscale
  convection, clearly visible on the domain surface (~0.96 R), generated
  by a solar-like density and entropy stratification. Scale-splitting
  is evident at various depths throughout the model, with the upper
  boundary of convective cells penetrating surface layers, resembling
  solar-like convection. A continuous and coherent multiscale structure
  of convective cells is observed throughout the convective interior. The
  power peak of convective scales continuously shrinks with height to a
  maximum spherical harmonic degree of l = 40-50 on the model surface,
  compatible with reports of giant cell observations. Simulations are
  performed from low to high resolution to explore whether integral
  properties of convection, such as the RMS velocity, temperature
  profiles, and turbulent spectra, become independent of the mesh
  size. Results are compared with current observations of surface and
  sub-surface solar convection.

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Title: 3D Helioseismic Forward-Modeling and Analysis of Meridional
    Circulation
Authors: Stejko, Andrey; Kosovichev, Alexander; Pipin, Valery;
   Guerrero, Gustavo; Getling, Alexander; Smolarkiewicz, Piotr
2021AGUFMSH55D1870S    Altcode:
  The 3D Global Acoustic Linearized Euler (GALE) code is used to explore
  the variance in helioseismic signatures that result from various
  profiles of meridional circulation. The structure of meridional
  circulation regulates the redistribution of angular momentum and
  magnetic flux that governs the solar cycle. Forward-modeling is a useful
  tool in exploring the structure of meridional circulation and its impact
  on global parameters and can help resolve the current controversy
  between single and double-cell circulation profiles. Profiles of
  meridional circulation are generated using mean-field dynamo models,
  which induce a reverse flow near the base of the convection zone,
  characteristic of double-cell meridional circulation, with the inclusion
  of turbulent pumping (-effect) resulting from a strong rotational
  gradient in the region. These models provide physics-based mechanisms
  for the low-end in potential differences between single- and double-cell
  meridional circulation profiles. The resulting flows are used as
  background velocities in the linearized acoustic GALE codesimulating the
  stochastic excitation of acoustic perturbations. Techniques in local
  helioseismology are then applied to measure flow signatures, showing
  that within the observational time-period of the HMI instrument onboard
  Solar Dynamics Observatory, it may not be possible to definitively
  distinguish between single-cell and double-cell meridional circulation
  structure. This analysis is extended to models of meridional circulation
  generated in convectively-driven non-linear 3D global-Sun simulations
  to explore the helioseismic differences generated by these models and
  compare them with observations.

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Title: The Origin Of The Extended Solar Cycle
Authors: Kosovichev, A.; Pipin, V.; Getling, A.
2021AAS...23830405K    Altcode:
  The extended 22-year solar cycle phenomenon, discovered in observations
  of the solar corona and variations of the solar differential rotation
  (torsional oscillations), represents a fundamental heliophysics problem
  linked to dynamo processes inside the Sun. As observed on the surface,
  the extended solar cycle starts during a sunspot maximum at high
  latitudes and consists of a relatively short polar branch (described
  as "rush to the poles") and a long equatorward branch that continues
  through the solar minimum and the next sunspot cycle. Helioseismic
  observations of the internal dynamics of the Sun during the last two
  solar activity cycles allow us to identify the dynamical processes
  associated with the extended solar cycle throughout the depth of the
  convective zone and to link them with dynamo models. Observational
  data obtained from the SoHO (1996-2010) and SDO (2010-2020) spacecraft
  represent measurements of the internal differential rotation, meridional
  circulation, and thermodynamic parameters. The data indicate that the
  development of a new extended solar cycle begins at about 60 degrees
  latitude at the base of the convective zone during the maximum of
  the previous cycle. Then, the process of magnetic field migration to
  the Sun's surface is divided into two branches: fast (in 1-2 years)
  migration to the poles in the high-latitude zone and slow migration to
  the equator at middle and low latitudes for ~ 10 years. The subsurface
  rotational shear layer (leptocline) plays a key role in the formation
  of the magnetic butterfly diagram. Both the zonal flows (torsional
  oscillations) and the meridional circulation reveal the 22-year
  pattern of the extended solar cycle. A self-consistent MHD model
  of the solar dynamo developed in the mean-field theory framework is
  in good qualitative and quantitative agreement with the helioseismic
  observations. The model shows that the extended solar-cycle phenomenon
  is caused by magnetic field quenching of the convective heat flux
  and modulation of the meridional circulation induced by the heat
  flux variations. The model explains why the solar minimum polar field
  predicts the next sunspot maximum and points to new possibilities for
  predicting solar cycles from helioseismological data.

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Title: Helioseismic Observations and Modeling of Solar Dynamo
Authors: Kosovichev, Alexander G.; Getling, Alexander V.; Pipin,
   Valery V.
2021csss.confE.115K    Altcode:
  Helioseismological observations of the internal dynamics of the
  Sun during the last two solar activity cycles make it possible
  to trace the development of solar dynamo processes throughout the
  depth of the convective zone and to link them with models of solar
  cycles. Observational data obtained from the SoHO (1996-2010) and
  SDO (2010-2020) spacecraft represent measurements of the internal
  differential rotation, meridional circulation, and thermodynamic
  parameters. The structure and dynamics of zonal and meridional
  plasma flows reveal the processes of generation and transfer of
  magnetic fields inside the Sun. The data analysis shows that active
  latitudes and regions of a strong polar field on the Sun's surface
  coincide with regions of deceleration of zonal currents ("torsional
  oscillations"). The observed structure of zonal flows and their
  latitudinal and radial migration in deep layers of the convective
  zone correspond to dynamo waves predicted by dynamo theories and
  numerical MHD models. The data indicate that the development of a new
  solar cycle begins at about 60 degrees latitude at the base of the
  convective zone during the maximum of the previous cycle. Then, the
  process of magnetic field migration to the Sun's surface is divided
  into two branches: fast (in 1-2 years) migration in the high-latitude
  zone and slow migration at middle and low latitudes for ~ 10 years. The
  subsurface rotational shear layer ("leptocline") plays a key role in
  the formation of the magnetic "butterfly diagram". Both the zonal
  flows ("torsional oscillations") and the meridional circulation
  reveal the 22-year pattern of the "extended" solar cycle, initially
  discovered from observations of Doppler velocities and the structure
  of the solar corona.A self-consistent MHD model of the solar dynamo
  developed in the mean-field theory framework is in good qualitative
  and quantitative agreement with the helioseismic observations. The
  model shows that the observed variations of the solar dynamics are
  associated with a magnetic field effect on convective heat transfer
  and the corresponding modulation of the meridional circulation. The
  model explains why the solar minimum polar field predicts the next
  sunspot maximum and points to new possibilities for predicting solar
  cycles from helioseismological data.

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Title: Evolution of Subsurface Zonal and Meridional Flows in Solar
    Cycle 24 from Helioseismological Data
Authors: Getling, Alexander V.; Kosovichev, Alexander G.; Zhao, Junwei
2021ApJ...908L..50G    Altcode: 2020arXiv201215555G
  The results of determinations of the azimuthal and meridional
  velocities by time-distance helioseismology from Helioseismic and
  Magnetic Imager on board Solar Dynamics Observatory from 2010 May to
  2020 September at latitudes and Stonyhurst longitudes from - 60° to
  + 60° and depths to about 19 Mm below the photosphere are used to
  analyze spatiotemporal variations of the solar differential rotation
  and meridional circulation. The pattern of torsional oscillations,
  or latitudinal belts of alternating "fast" and "slow" zonal flows
  migrating from high latitudes toward the equator, is found to extend in
  the time-latitude diagrams over the whole time interval. The oscillation
  period is comparable with a doubled solar-activity-cycle and can be
  described as an extended solar cycle. The zonal-velocity variations
  are related to the solar-activity level, the local-velocity increases
  corresponding to the sunspot-number increases and being localized at
  latitudes where the strongest magnetic fields are recorded. The dramatic
  growth of the zonal velocities in 2018 appears to be a precursor of
  the beginning of Solar Cycle 25. The strong symmetrization of the
  zonal-velocity field by 2020 can be considered another precursor. The
  general pattern of poleward meridional flows is modulated by latitudinal
  variations similar to the extended-solar-cycle behavior of the zonal
  flows. During the activity maximum, these variations are superposed
  with a higher harmonic corresponding to meridional flows converging to
  the spot-formation latitudes. Our results indicate that variations of
  both the zonal and meridional flows exhibit the extended-solar-cycle
  behavior, which is an intrinsic feature of the solar dynamo.

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Title: Peculiarities of the Dynamics of Solar NOAA Active Region 12673
Authors: Getling, A. V.
2019ApJ...878..127G    Altcode: 2019arXiv190408367G
  The dynamics of active region (AR) 12673 is qualitatively studied using
  observational data obtained with the Helioseismic and Magnetic Imager
  of the Solar Dynamics Observatory on 2017 August 31-September 8. This
  AR was remarkable for its complex structure and extraordinary flare
  productivity. The sunspot group in this AR consisted of (1) an old,
  well-developed and highly stable, coherent sunspot, which had also been
  observed two solar rotations earlier, and (2) a rapidly developing
  cluster of umbral and penumbral fragments. Cluster (2) formed two
  elongated, arc-shaped chains of spot elements, skirting around the
  major sunspot (1), with two chains of magnetic elements spatially
  coinciding with the arcs. AR components (1) and (2) were in relative
  motion, cluster (2) overtaking spot (1) in westward motion, and their
  relative velocity agrees in order of magnitude with the velocity jump
  over the near-surface shear layer, or leptocline. The pattern of motion
  of the features about the main spot bears amazing resemblance to the
  pattern of a fluid flow about a roundish body. This suggests that spot
  (1) was dynamically coupled with the surface layers, while cluster (2)
  developed in deeper layers of the convection zone. The magnetic-flux
  emergence in cluster (2) appeared to be associated with fluid motions
  similar to roll convection. The mutual approach of components (1)
  and (2) gave rise to light bridges in the umbrae of sunspots with the
  magnetic field having the same sign on both sides of the bridge.

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Title: The Origin and Early Evolution of a Bipolar Magnetic Region
    in the Solar Photosphere
Authors: Getling, A. V.; Buchnev, A. A.
2019ApJ...871..224G    Altcode: 2018arXiv180506486G
  Finding the formation mechanisms for bipolar configurations of a
  strong local magnetic field under control of the relatively weak
  global magnetic field of the Sun is a key problem of the physics of
  solar activity. This study is aimed at discriminating whether the
  magnetic field or fluid motion plays a primary, active role in this
  process. The very origin and early development stage of Active Region
  12548 are investigated based on Solar Dynamics Observatory/Helioseismic
  and Magnetic Imager observations of 2016 May 20-25. Full-vector
  magnetic and velocity fields are analyzed in parallel. The leading
  and trailing magnetic polarities are found to grow asymmetrically in
  terms of their amplitude, magnetic flux, and the time variation of
  these quantities. The leading-polarity magnetic element originates
  as a compact feature against the background of a distributed
  trailing-polarity field, with an already existing trailing-polarity
  magnetic element. No signs of strong horizontal magnetic fields
  are detected between the two magnetic poles. No predominant upflow
  between their future locations precedes the origin of this bipolar
  magnetic region (BMR); instead, upflows and downflows are mixed, with
  some prevalence of downflows. Any signs of a large-scale horizontal
  divergent flow from the area where the BMR develops are missing;
  in contrast, a normal supergranulation and mesogranulation pattern
  is preserved. This scenario of early BMR evolution is in strong
  contradiction with the expectations based on the model of a rising
  Ω-shaped loop of a flux tube of strong magnetic field, and an in
  situ mechanism of magnetic-field amplification and structuring should
  operate in this case.

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Title: Effects of variable thermal diffusivity on the structure
    of convection
Authors: Shcheritsa, O. V.; Getling, A. V.; Mazhorova, O. S.
2016arXiv160402543S    Altcode:
  The multiscale flow structure in the solar convection zone -
  the coexistence of such features as the granules, mesogranules,
  supergranules and giant cells - has not yet been properly
  understood. Here, the possible role of one physical factor - variations
  in the thermal diffusivity - in the formation of a multiscale convection
  structure is investigated. Thermal convection in a plane horizontal
  fluid layer is numerically simulated. The temperature dependence of
  thermal diffusivity is chosen so as to produce a sharp kink in the
  static temperature profile near the upper layer boundary. As a result,
  the magnitude of the (negative) static temperature gradient dTs/dz,
  being small over the most part of the layer thickness, reaches large
  values in a thin boundary sublayer. To identify the structures on
  different scales, we apply a smoothing procedure, computational-homology
  techniques and spectral processing to the temperature field. The flow
  is found to be a superposition of three cellular structures with three
  different characteristic scales. The largest (first-scale) convection
  cells, with central upflows, fill the whole layer thickness; most of
  these cells are divided by bridges, or isthmuses, into a few smaller
  (second-scale) ones, which are localised in the upper portion of the
  layer; finally, there are numerous tiny (third-scale) features that dot
  the horizontal sections of the layer located near its upper boundary
  and exhibit a tendency of gathering in the intercellular lanes of the
  first-scale cells. The third-scale cellular structures are advected
  by the first-scale and second-scale convective flows. The spatial
  spectrum of the flow does not directly indicate the presence of the
  second-scale and third-scale structures; however, they can be selected
  by using our processing techniques. On the whole, the simulated flow
  pattern qualitatively resembles that observed on the Sun.

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Title: Development of Active Regions: Flows, Magnetic-Field Patterns
    and Bordering Effect
Authors: Getling, A. V.; Ishikawa, R.; Buchnev, A. A.
2016SoPh..291..371G    Altcode: 2016SoPh..tmp....9G; 2015arXiv150601848G
  A qualitative analysis is given of the data on the full magnetic
  and velocity vector fields in a growing sunspot group, recorded
  nearly simultaneously with the Solar Optical Telescope on the Hinode
  satellite. Observations of a young bipolar subregion developing within
  AR 11313 were carried out on 9 - 10 October 2011. Our aim was to form an
  idea about the consistency of the observed pattern with the well-known
  rising-tube model of the formation of bipolar active regions and sunspot
  groups. We find from our magnetograms that the distributions of the
  vertical [B<SUB>v</SUB>] and the horizontal [B<SUB>h</SUB>] component
  of the magnetic field over the area of the magnetic subregion are
  spatially well correlated; in contrast, the rise of a flux-tube loop
  would result in a qualitatively different pattern, with the maxima of
  the two magnetic-field components spatially separated: the vertical
  field would be the strongest where either spot emerges, while the
  maximum horizontal-field strengths would be reached in between them. A
  specific feature, which we call the bordering effect, is revealed:
  some local extrema of B<SUB>v</SUB> are bordered with areas of locally
  enhanced B<SUB>h</SUB>. This effect suggests a fountainlike spatial
  structure of the magnetic field near the B<SUB>v</SUB> extrema, which
  is also hardly compatible with the emergence of a flux-tube loop. The
  vertical-velocity field in the area of the developing active subregion
  does not exhibit any upflow on the scale of the whole subregion, which
  should be related to the rising-tube process. Thus, our observational
  data can hardly be interpreted in the framework of the rising-tube
  model.

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Title: Stratification-induced scale splitting in convection
Authors: Shcheritsa, O. V.; Getling, A. V.; Mazhorova, O. S.
2015AdSpR..55..927S    Altcode: 2014arXiv1401.8137S
  The coexistence of motions on various scales is a remarkable feature of
  solar convection, which should be taken into account in analyses of the
  dynamics of magnetic fields. Therefore, it is important to investigate
  the factors responsible for the observed multiscale structure of solar
  convection. In this study, an attempt is made to understand how the
  scales of convective motions are affected by the particularities of
  the static temperature stratification of a fluid layer. To this end,
  simple models are considered. The equations of two-dimensional thermal
  convection are solved numerically for a plane horizontal fluid layer
  heated from below, in an extended Boussinesq approximation that
  admits thermal-diffusivity variations. These variations specify
  the stratification of the layer. The static temperature gradient
  in a thin sublayer near the upper surface of the layer is assumed
  to be many times larger than in the remainder of the layer. In
  some cases, distributed heat sinks are assumed to produce a stably
  stratified region overlying the convective layer. Manifestations of
  the scale-splitting effect are noted, which depend on the boundary
  conditions and stratification; it becomes more pronounced with the
  increase of the Rayleigh number. Small-scale convection cells are
  advected by larger-scale flows. In particular, the phase trajectories
  of fluid particles indicate the presence of complex attractors, which
  reflect the multiscale structure of the flow. The effect of the stably
  stratified upper sublayer on the flow scales is also considered.

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Title: Doubts about the crucial role of the rising-tube mechanism
    in the formation of sunspot groups
Authors: Getling, A. V.; Ishikawa, R.; Buchnev, A. A.
2015AdSpR..55..862G    Altcode: 2014arXiv1401.8077G
  Some preliminary processing results are presented for a dataset obtained
  with the Solar Optical Telescope on the Hinode satellite. The idea of
  the project is to record, nearly simultaneously, the full velocity and
  magnetic-field vectors in growing active regions and sunspot groups at
  a photospheric level. Our ultimate aim is to elaborate observational
  criteria to distinguish between the manifestations of two mechanisms
  of sunspot-group formation - the rising of an Ω -shaped flux tube of
  a strong magnetic field and the in situ amplification and structuring
  of magnetic field by convection (the convective mechanism is briefly
  described). <P />Observations of a young bipolar subregion developing
  within AR 11313 were carried out on 9-10 October 2011. During each
  2-h observational session, 5576-Å filtergrams and Dopplergrams
  were obtained at a time cadence of 2 min, and one or two 32-min-long
  spectropolarimetric fast-mode scans were done. Based on the series of
  filtergrams, the trajectories of corks are computed, using a technique
  similar to but more reliable than local correlation tracking (LCT),
  and compared with the magnetic maps. At this stage of the investigation,
  only the vertical magnetic field and the horizontal flows are used for
  a qualitative analysis. <P />According to our preliminary findings,
  the velocity pattern in the growing active region has nothing to do
  with a spreading flow on the scale of the entire bipolar region, which
  could be expected if a tube of strong magnetic field emerged. No violent
  spreading flows on the scale of the entire growing magnetic region can
  be identified. Instead, normal mesogranular and supergranular flows
  are preserved. Signs of small-scale structuring of the magnetic field
  can be detected in the area where new spots develop, and signs of
  the presence of separatrices between the magnetic polarities can be
  found, such that the surface flows converge to but not diverge from
  these separatrix curves. The observed scenario of evolution seems to
  agree with Bumba's inference that the development of an active region
  does not entail the destruction of the existing convective-velocity
  field. The convective mechanism appears to be better compatible with
  observations than the rising-tube mechanism. <P />In the umbras of
  the well-developed sunspots, flows converging to the umbra centres
  are revealed. Spreading streams are present around these spots.

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Title: Can subphotospheric magnetic fields be amplified and structured
    by a convective mechanism?
Authors: Getling, Alexander; Mazhorova, Olga; Kolmychkov, Vyacheslav
2014cosp...40E.975G    Altcode:
  Strong photospheric magnetic fields frequently originate at the knots
  of the network formed by intercellular lanes -- the peripheral parts
  of convection cells on various scales. This phenomenon is normally
  interpreted as a result of the “sweeping” of magnetic field lines by
  convective motions. On the other hand, magnetic elements can emerge in
  the inner parts of supergranules (Title, 2006), which may be an effect
  of the “winding” of magnetic field lines by circulating matter, as
  suggested by Tverskoi (1966) based on a simple kinematic model. In this
  study, magnetoconvection in a horizontal layer of incompressible fluid
  is simulated numerically. The initial magnetic field is assumed to be
  weak, uniform throughout the layer and horizontal. The interaction of
  quasi-ordered cellular convection with the magnetic field is shown to be
  able to produce bipolar (and also diverse more complex) configurations
  of a substantially amplified magnetic field. In some cases, bipolar
  magnetic structures change into unipolar ones. Such transitions are
  analysed. The formation of the magnetic features can be attributed to
  either the “winding” or “sweeping” of magnetic field lines. The
  operation of this mechanism is controlled by the very topology of the
  cellular flow and does not require strong initial fields. Under solar
  conditions, it should be manifest on various spatial scales. This
  work was supported by the Russian Foundation for Basic Research,
  project no. 12-02-00792-a.

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Title: Formation of sunspot groups: Do we see manifestations of the
    rising-tube mechanism?
Authors: Getling, Alexander; Ishikawa, Ryohko; Buchnev, Aleksei
2014cosp...40E.974G    Altcode:
  A comparison is made between the expected manifestations of two
  mechanisms suggested to account for the formation of local photospheric
  magnetic fields, viz., the rising of an Omega-shaped flux tube of
  a strong magnetic field and the emph{in situ} amplification and
  structuring of magnetic field by convection. The ultimate aim of
  the study is to elaborate observational criteria to find out which
  mechanism controls the process in any given case. To this end, the
  full velocity and magnetic-field vectors in growing active regions
  and sunspot groups at a photospheric level were recorded nearly
  simultaneously. Observations of a young bipolar subregion developing
  within AR 11313 were carried out on 9-10 October 2011, with the Solar
  Optical Telescope on the emph{Hinode} satellite, which yielded 5576-Å
  filtergrams and Dopplergrams and also spectropolarimetric records of
  the magnetic-field vector. To determine the tangential-velocity field,
  a technique similar to but more reliable than local correlation tracking
  (LCT) was applied to the series of filtergrams, and the trajectories
  of corks were computed. According to our preliminary findings, the
  velocity pattern in the growing active region cannot be described
  as a spreading flow on the scale of the entire bipolar region, which
  could be expected if a tube of strong magnetic field emerged. Instead,
  normal mesogranular and supergranular flows are observed in agreement
  with Bumba’s inference that the development of an active region
  does not entail the destruction of the existing convective-velocity
  field. Between the magnetic polarities, curves can be found to which
  the surface flows converge rather than diverging from them under
  the action of a rising tube. The convective mechanism appears to be
  better compatible with observations than the rising-tube mechanism. In
  the umbras of the well-developed sunspots, flows converging to the
  umbra centres are revealed. Spreading streams are present around these
  spots. Hinode is a Japanese mission developed and launched by ISAS/JAXA,
  with NAOJ as domestic partner and NASA and STFC (UK) as international
  partners. It is operated by these agencies in cooperation with ESA
  and NSC (Norway). This work was supported by the Russian Foundation
  for Basic Research (project no. 12-02-00792-a).

---------------------------------------------------------
Title: Why can different flow scales coexist in solar convection?
Authors: Getling, Alexander; Shcheritsa, Olga; Mazhorova, Olga
2014cosp...40E.976G    Altcode:
  Solar convection demonstrates a remarkable multiscale structure (the
  coexistence of granules, mesogranules, supergranules and giant cells),
  which largely controls the structure and dynamics of photospheric
  magnetic fields. With the aim of comprehending the possible mechanisms
  of such scale splitting, the effect of particularities of the static
  temperature profile on the structure of convection are considered
  here. To this end, two-dimensional convection in a plane horizontal
  layer of an incompressible fluid heated from below is simulated
  numerically. The stratification of the layer is controlled by
  thermal-diffusivity variations. The static temperature gradient in
  a thin sublayer near the upper surface of the layer is assumed to be
  many times larger than in the remainder of the layer. In some cases,
  distributed heat sinks are assumed to produce a stably stratified region
  overlying the convective layer. Manifestations of the scale-splitting
  effect are observed, which depend on the boundary conditions and
  stratification. The multiscale structure of the flow is manifest most
  clearly in the presence of complex attractors in the pattern of phase
  trajectories of fluid particles. Small-scale convection cells are
  carried by larger-scale flows. This work was supported by the Russian
  Foundation for Basic Research, project no. 12-02-00792-a.

---------------------------------------------------------
Title: Concerning the multiscale structure of solar convection
Authors: Getling, A. V.; Mazhorova, O. S.; Shcheritsa, O. V.
2013Ge&Ae..53..904G    Altcode:
  The discrete scale spectrum of the convective flows observed on the
  Sun has not yet received a convincing explanation. Here, an attempt
  is made to find conditions for the coexistence of convective flows on
  various scales in a horizontal fluid layer heated from below, where
  the thermal diffusivity varies with temperature in such a way that the
  static temperature difference across a thin sublayer near the upper
  surface of the layer is many times larger than the temperature variation
  across the remainder of the layer. The equations of two-dimensional
  thermal convection are solved numerically in an extended Boussinesq
  approximation, which admits thermal-diffusivity variations. The
  no-slip conditions are assumed at the lower boundary of the layer;
  either no-slip or free-slip conditions, at the upper boundary. In the
  former case, stable large-scale rolls develop, which experience small
  deformations under the action of small structures concentrated near
  the horizontal boundaries. In the latter case, the flow structure is
  highly variable, different flow scales dominate at different heights,
  the number of large rolls is not constant, and a sort of intermittency
  occurs: the enhancement of the small-scale flow component is frequently
  accompanied by the weakening of the large-scale one, and vice versa. The
  scale-splitting effects revealed here should manifest themselves in
  one way or another in the structure of solar convection.

---------------------------------------------------------
Title: Convective mechanism of amplification and structuring of
    magnetic fields
Authors: Getling, A. V.; Kolmychkov, V. V.; Mazhorova, O. S.
2013IAUS..294..137G    Altcode:
  Magnetoconvection in a horizontal layer of incompressible fluid
  is simulated numerically. The initial magnetic field is assumed
  to be uniform and horizontal. The interaction of quasi-ordered
  cellular convection with the magnetic field is shown to be able to
  produce bipolar (and also diverse more complex) configurations of a
  substantially amplified magnetic field. The operation of this mechanism,
  which can be regarded as a modification of the mechanism suggested by
  Tverskoi (1966), is controlled by the very topology of the cellular
  flow, should be manifest on various spatial scales, and does not
  require strong initial fields. Magnetic configurations develop both in
  the central parts of convection cells, where circulatory fluid motion
  “winds” magnetic field lines, and in the network formed by their
  peripheral regions due to the “sweeping” of magnetic field lines.

---------------------------------------------------------
Title: The flow helicity in quasi-orderedcellular convection
Authors: Getling, A. V.
2013IAUS..294..359G    Altcode:
  The helicity of cellular convective flows in a horizontal layer of
  compressible fluid (gas) heated from below and rotating about a vertical
  axis is studied using finite-difference numerical simulations. The
  medium is assumed to be polytropically stratified. An initial thermal
  perturbation is introduced so as to produce a system of Bénard-type
  hexagonal convection cells. The flow gradually becomes less ordered,
  and the mean helicity grows initially and decreases sharply after the
  substantial chaotisation of the flow. Given the Rayleigh and Prandtl
  numbers, the maximum value reached by the mean helicity increases with
  the decrease of the polytrope index and has a maximum at a certain
  rotational velocity of the layer.

---------------------------------------------------------
Title: Toward understanding the multiscale spatial spectrum of
    solar convection
Authors: Getling, A. V.; Mazhorova, O. S.; Shcheritsa, O. V.
2013IAUS..294..361G    Altcode:
  Convection is simulated numerically based on two-dimensional Boussinesq
  equations for a fluid layer with a specially chosen stratification such
  that the convective instability is much stronger in a thin subsurface
  sublayer than in the remaining part of the layer. The developing
  convective flow has a small-scale component superposed onto a basic
  large-scale roll flow.

---------------------------------------------------------
Title: The helicity of the velocity field for cellular convection
    in a rotating layer
Authors: Getling, A. V.
2012ARep...56..395G    Altcode: 2012AZh....89..441G
  The helicity of a cellular convective flow in a horizontal layer
  of a compressible fluid (gas) heated from below and rotating about
  the vertical axis is studied using finite-difference numerical
  simulations. The medium is assumed to be polytropically stratified. A
  thermal perturbation that produces a system of Bénard-type hexagonal
  convection cells is introduced at the initial time. Next, the cells
  are deformed by the action of the Coriolis force; however, at some
  stage of the evolution, the flow is nearly steady (at later times,
  the cells break down). For given Rayleigh and Prandtl numbers, the
  velocity-field helicity for this stage averaged over the layer increases
  with decreasing polytrope index (i.e., with increasing the curvature of
  the static entropy profile) and has a maximum at a certain rotational
  velocity of the layer. Numerical simulations of such quasi-ordered
  convective flows should reduce the uncertainties in estimates of the
  helicity, a quantity important for the operation of MHD dynamos.

---------------------------------------------------------
Title: Some structural features of the convective-velocity field in
    the solar photosphere
Authors: Getling, A. V.; Buchnev, A. A.
2010ARep...54..254G    Altcode: 2010AZh....87..286G
  An algorithm for measuring horizontal photospheric velocities previously
  employed to process aerospace images is adapted for problems in solar
  physics and realized in a computational code. It differs from the
  standard procedure of local correlation tracking in a special choice
  of trial areas (“targets”), whose displacements are determined
  bymaximizing the correlation between the original and various shifted
  positions of the target. Specifically, an area is chosen as a target
  in a certain neighborhood of each node of a predefined grid if either
  the contrast or the entropy of the brightness distribution reaches
  its maximum in this area. The horizontal velocities obtained are then
  interpolated to the positions of imaginary “corks” using the
  Delaunay triangulation and affine transformations specified by the
  deformation of the obtained triangles at the time step considered. The
  motion of the corks is represented by their trajectories. A
  superposition of flows on different scales, from mesogranular to
  supergranular, can clearly be seen. “Large mesogranules” with
  sizes of order 15 Mm are revealed. In many cases, these are stellate in
  shape. Areas of strong convergence of the horizontal flows are detected;
  this convergence is sometimes accompanied by swirling. Evidence is
  found for the possible coexistence of convection cells with different
  circulation directions, so-called l-type and g-type cells.

---------------------------------------------------------
Title: Do Long-Lived Features Really Exist in the Solar
    Photosphere? II. Contrast of Time-Averaged Granulation Images
Authors: Brandt, P. N.; Getling, A. V.
2008SoPh..249..307B    Altcode: 2008arXiv0802.0204B; 2008SoPh..tmp...64B
  The decrease in the rms contrast of time-averaged images with the
  averaging time is compared between four data sets: (1) a series of
  solar granulation images recorded at La Palma in 1993, (2) a series
  of artificial granulation images obtained in numerical simulations
  by Rieutord et al. (Nuovo Cimento25, 523, 2002), (3) a similar
  series computed by Steffen and his colleagues (see Wedemeyer et
  al. in Astron. Astrophys.44, 1121, 2004), (4) a random field with
  some parameters typical of the granulation, constructed by Rast
  (Astron. Astrophys.392, L13, 2002). In addition, (5) a sequence of
  images was obtained from real granulation images by using a temporal
  and spatial shuffling procedure, and the contrast of the average of n
  images from this sequence as a function of n is analysed. The series
  (1) of real granulation images exhibits a considerably slower contrast
  decrease than do both the series (3) of simulated granulation images
  and the series (4) of random fields. Starting from some relatively
  short averaging times t, the behaviour of the contrast in series (3)
  and (4) resembles the t<SUP>−1/2</SUP> statistical law, whereas
  the shuffled series (5) obeys the n<SUP>−1/2</SUP> law from n=2
  on. Series (2) demonstrates a peculiarly slow decline of contrast,
  which could be attributed to particular properties of the boundary
  conditions used in the simulations. Comparisons between the analysed
  contrast-variation laws indicate quite definitely that the brightness
  field of solar granulation contains a long-lived component, which could
  be associated with locally persistent dark intergranular holes and/or
  with the presence of quasi-regular structures. The suggestion that the
  random field (4) successfully reproduces the contrast-variation law
  for the real granulation (Rast in Astron. Astrophys.392, L13, 2002)
  can be dismissed.

---------------------------------------------------------
Title: Widespread Occurrence of Trenching Patterns in the Granulation
Field: Evidence for Roll Convection?
Authors: Getling, A. V.; Buchnev, A. A.
2008SoPh..248..233G    Altcode: 2007arXiv0709.3251G
  Time-averaged series of granulation images are analysed using
  COLIBRI, a purpose-adapted version of a code originally developed
  to detect straight or curvilinear features in aerospace images. The
  image-processing algorithm utilises a nonparametric statistical
  criterion that identifies a straight-line segment as a linear feature
  (lineament) if the photospheric brightness at a certain distance
  from this line on both sides is stochastically lower or higher than
  at the line itself. Curvilinear features can be detected as chains
  of lineaments, using a modified criterion. Once the input parameters
  used by the algorithm are properly adjusted, the algorithm highlights
  "ridges" and "trenches" in the relief of the brightness field, drawing
  white and dark lanes. The most remarkable property of the trenching
  patterns is a nearly universally present parallelism of ridges and
  trenches. Since the material upflows are brighter than the downflows,
  the alternating, parallel light and dark lanes should reflect the
  presence of roll convection in the subphotospheric layers. If the
  numerous images processed by us are representative, the patterns
  revealed suggest a widespread occurrence of roll convection in the
  outer solar convection zone. In particular, the roll systems could form
  the fine structure of larger scale, supergranular and/or mesogranular
  convection flows. Granules appear to be overheated blobs of material
  that could develop into convection rolls owing to instabilities of
  roll motion.

---------------------------------------------------------
Title: Generation of coupled global and local magnetic fields by a
    cellular MHD dynamo
Authors: Getling, A. V.; Simitev, R. D.; Busse, F. H.
2007IAUS..239..482G    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: Is solar convection responsible for the local amplification and
    structuring of magnetic fields? (Observational test of the hypothesis)
Authors: Getling, A. V.; Bao, X. M.
2007IAUS..239..496G    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: Quasi-regular structures in the solar photosphere (trenching
in the brightness relief): Algorithmic treatment
Authors: Getling, A. V.; Buchnev, A. A.
2007IAUS..239..499G    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: Can cellular convection in a rotating spherical shell maintain
    both global and local magnetic fields?
Authors: Getling, A. V.; Simitev, R. D.; Busse, F. H.
2007IJGA....7.1004G    Altcode: 2007IJGA....7I1004G; 2006astro.ph.10753G
  [1] A convection-driven MHD dynamo in a rotating spherical shell, with
  clearly defined structural elements in the flow and magnetic field,
  is simulated numerically. Such dynamos can be called deterministic,
  in contrast to those explicitly dependent on the assumed properties of
  turbulence. The cases most interesting from the standpoint of studying
  the nature of stellar magnetism demonstrate the following features. On
  a global scale, the convective flows can maintain a "general" magnetic
  field with a sign-alternating dipolar component. Local (in many
  cases, bipolar) magnetic structures are associated with convection
  cells. Disintegrating local structures change into background fields,
  which drift toward the poles. From time to time, reversals of the
  magnetic fields in the polar regions occur, as "new" background fields
  expel the "old" fields.

---------------------------------------------------------
Title: Do Quasi-Regular Structures Really Exist in the Solar
    Photosphere? I. Observational Evidence
Authors: Getling, A. V.
2006SoPh..239...93G    Altcode: 2006SoPh..tmp...82G; 2006astro.ph.10698G
  Two series of solar-granulation images - the La Palma series of 5 June
  1993 and the SOHO MDI series of 17 - 18 January 1997 - are analysed
  both qualitatively and quantitatively. New evidence is presented for
  the existence of long-lived, quasi-regular structures (first reported
  by Getling and Brandt, Astron. Astrophys. 382, L5 (paper I), 2002),
  which no longer appear unusual in images averaged over 1 - 2-hour
  time intervals. Such structures appear as families of light and dark
  concentric rings or families of light and dark parallel strips ("ridges"
  and "trenches" in the brightness distributions). In some cases, rings
  are combined with radial "spokes" and can thus form "web" patterns. The
  characteristic width of a ridge or trench is somewhat larger than
  the typical size of granules. Running-average movies constructed from
  the series of images are used to seek such structures. An algorithm
  is developed to obtain, for automatically selected centres, the
  radial distributions of the azimuthally averaged intensity, which
  highlight the concentric-ring patterns. We also present a time-averaged
  granulation image processed with a software package intended for the
  detection of geological structures in aerospace images. A technique of
  running-average-based correlations between the brightness variations
  at various points of the granular field is developed and indications
  are found for a dynamical link between the emergence and sinking of hot
  and cool parcels of the solar plasma. In particular, such a correlation
  analysis confirms our suggestion that granules - overheated blobs -
  may repeatedly emerge on the solar surface. Based on our study, the
  critical remarks by Rast (Astron. Astrophys. 392, L13, 2002) on the
  original paper by Getling and Brandt (paper I) can be dismissed.

---------------------------------------------------------
Title: Cellular dynamo in a rotating spherical shell
Authors: Getling, A. V.; Simitev, R. D.; Busse, F. H.
2005AN....326..241G    Altcode:
  Magnetoconvection in a rotating spherical shell is simulated numerically
  using a code developed by Tilgner and Busse. The thermal stratification
  is convectively unstable in the outer part and stable in the inner
  part of the shell. Regimes are found in which the convective flow is
  weakly affected by rotation and preserves its cellular structure. The
  dipolar component of the large-scale magnetic field exhibits undamped
  oscillations. It appears that convection cells slightly modified by
  rotation can be building blocks of the global dynamo. The generation
  of the magnetic field is thus due to regular “macroscopic” flows,
  and their structure itself may ensure the presence of the α effect
  responsible for the action of the dynamo. Such dynamos can be called
  deterministic, in contrast to those in which the maintenance of the
  magnetic field is related to the statistical predominance of a certain
  sign of helicity in the turbulent velocity field. Investigation of
  conditions under which dynamos of this sort can operate could suggest
  a more definite answer to the question of the origin of solar and
  stellar magnetic fields.

---------------------------------------------------------
Title: Contrast of time-averaged images of the solar granulation
Authors: Brandt, P. N.; Getling, A. V.
2004IAUS..223..231B    Altcode: 2005IAUS..223..231B
  The time-averaged images of the solar granulation exhibit a slower
  decrease in contrast with the averaging time than do time-averaged
  images of numerically simulated granulation and time-averaged random
  fields with some parameters typical of granulation. This confirms the
  hints for long-lived structures in the granulation pattern.

---------------------------------------------------------
Title: Compressible magnetoconvection as the local producer of
    solar-type magnetic structures
Authors: Dobler, W.; Getling, A. V.
2004IAUS..223..239D    Altcode: 2005IAUS..223..239D
  Simulations of cellular magnetoconvection in a compressible fluid
  reveal the formation of magnetic structures with a substantial bipolar
  component as an inherent property of the topology of cellular flows.

---------------------------------------------------------
Title: Structure of solar convection: guesses and observational
    evidence
Authors: Getling, A. V.
2004IAUS..223..247G    Altcode: 2005IAUS..223..247G
  Signs of quasi-regular structures in time-averaged photospheric images
  are described.

---------------------------------------------------------
Title: Regular Photospheric Patterns (Trenching in the Brightness
    Relief) and Persistence of the Granular Field
Authors: Getling, A. V.; Brandt, P. N.
2003ASPC..286..185G    Altcode: 2003ctmf.conf..185G
  No abstract at ADS

---------------------------------------------------------
Title: Convective Mechanism for Formation of Solar Magnetic Bipoles
Authors: Getling, A. V.; Ovchinnikov, I. L.
2003ASPC..286..139G    Altcode: 2003ctmf.conf..139G
  No abstract at ADS

---------------------------------------------------------
Title: Quasi-regular structures of the solar photosphere
Authors: Getling, A. V.; Brandt, P. N.
2002ESASP.506..617G    Altcode: 2002ESPM...10..617G; 2002svco.conf..617G
  As we already reported, the simple procedure of time averaging, when
  applied to the photospheric brightness field, reveals quasi-regular
  structures of the photospheric and subphotospheric flows. Our analysis
  presented here shows that the decrease in the rms contrast of the
  averaged images with the increase of the averaging time τ is slower
  compared to the √τ law, which argues for the real persistence
  of the revealed structures as physical entities. The procedure of
  running-average-based correlation is suggested to seek coherence
  between the brightness variations at the points of emergence and
  sinking of granules. Some results of the correlation analysis confirm
  the notion that granules are overheated blobs of material carried by
  the convective circulation.

---------------------------------------------------------
Title: Solar convection as the producer of magnetic bipoles
Authors: Getling, A. V.; Ovchinnikov, I. L.
2002ESASP.506..819G    Altcode: 2002svco.conf..819G; 2002ESPM...10..819G
  A mechanism for the in situ formation of bipolar magnetic
  configurations, alternative to the well-known rising-tube mechanism, is
  considered. Cellular magnetoconvection is simulated numerically. The
  initial magnetic field is assumed to be fairly weak and directed
  horizontally. A pattern of small-amplitude hexagonal cells is specified
  initially. A hexagonal convection cell can substantially amplify the
  magnetic field and impart bipolar configurations to it. Depending on
  the parameters, the amplified field may form either a simple pair of
  magnetic islands, opposite in polarity, or a more complex superposition
  of bipoles. In particular, very compact magnetic elements of strong
  field can form. The resulting pattern of magnetic-field evolution is
  in better agreement with observations than the rising-tube model.

---------------------------------------------------------
Title: Regular structures of the solar photosphere. (Persistence of
    the granular field and trenching in the brightness relief)
Authors: Getling, A. V.; Brandt, P. N.
2002A&A...382L...5G    Altcode:
  The simple procedure of time averaging, when applied to the
  photospheric brightness field, reveals quasi-regular structures of
  the photospheric and subphotospheric flows. We use an 8-h sub-set of
  the series of photospheric images obtained on 5 June 1993 with the
  Swedish Vacuum Solar Telescope, La Palma. First, the averaged images
  are far from completely smeared and contain a multitude of bright,
  granular-sized blotches even if the averaging period is as long as 8
  h. This suggests that granules prefer to originate at certain sites,
  where they emerge repeatedly, and the granular field demonstrates a
  sort of persistence for many hours. Second, the resulting patterns
  display relatively regular structures, which can be revealed only if
  the averaging period is sufficiently long (the optimum seems to lie
  between 2 and 3 h). The averaged brightness relief is “trenched”:
  it comprises systems of concentric rings and arcs as well as straight
  or slightly wavy lines and systems of parallel strips. The trenching
  patterns resemble the so-called target patterns observed in experiments
  on Rayleigh-Bénard convection. In addition, the brightness values
  at a local averaged-field maximum and at a nearby minimum exhibit a
  distinct tendency to vary in antiphase. Thus, a previously unknown
  type of self-organization is manifest in the solar atmosphere, and
  our findings support the suggestion that granules are associated with
  overheated blobs carried by the convective circulation.

---------------------------------------------------------
Title: Solar convection and sunspot formation mechanishm
Authors: Getling, A. V.
2001A&AT...20..433G    Altcode:
  The rising-flux-tube model of the formation of a bipolar sunspot
  group sharply disgrees with the normally observed features of the
  process. Meanwhile, these features can be successfully accounted
  for in terms of local magnetic-field amplification due to zellular
  convective motions of the solar plasma. Here, magnetoconvection in a
  plane horizontal fluid layer is simulated numberically magnetic field
  and a weak cellular flow are present. Convention can produce bipolar
  configurations of strongly amplified magnetic field. Indications are
  found for the nontrivial effect of flow freezing. The action of the
  convective mechanism may be controlled by the large-scale toroidal
  magnetic field of the Sun.

---------------------------------------------------------
Title: Convective Mechanism for the Formation of Photospheric
    Magnetic Fields
Authors: Getling, A. V.
2001ARep...45..569G    Altcode:
  The well-known model that attributes the formation of a bipolar sunspot
  group to the emergence of a flux tube disagrees sharply with the
  usual observed pattern of phenomena. At the same time, the observed
  patterns can be accounted for quite convincingly in terms of local
  magnetic-field amplification due to cellular convective motions of the
  solar plasma. In this study, magnetoconvection in a plane horizontal
  fluid layer is simulated numerically in the framework of the fully
  nonlinear, three-dimensional problem. A weak horizontal magnetic field
  and weak cellular flow are assumed to be present initially. Convection
  is shown to be capable of producing bipolar magnetic configurations of
  the strongly amplified magnetic field. Indications of magnetic freezing
  of the flow in the cell are found. The action of the amplification
  mechanism under study may be controlled by the large-scale toroidal
  magnetic field of the Sun.

---------------------------------------------------------
Title: Hydrodynamic Instabilities and Photospheric Structures
Authors: Getling, A. V.
2000ARep...44...56G    Altcode:
  The possible role of convective-flow instabilities in the formation
  of certain structures observed in the solar photospheric and
  subphotospheric layers is discussed. High-resolution video records
  suggest that the granulation field is structurally and dynamically
  ordered in accordance with the mesogranulation pattern. Thus, it
  strikingly resembles the so-called spoke patterns of convection
  observed experimentally. These patterns could be produced by some
  instability of the mesogranular flow. Mesogranules seem to be the main
  structural features of the velocity field, whereas granules behave
  as relatively passive elements—blobs of overheated material carried
  by the mesogranular flow. One possible mechanism for their origin is
  the development of a three-dimensional analogue of the one-blob or the
  two-blob instability known from studies of convection. In particular,
  if this interpretation is adopted, the phenomenon of exploding granules
  can be accounted for in a natural way.

---------------------------------------------------------
Title: Numerical modelling of the magnetospheric convection in the
    region of closed force lines of the magnetic field.
Authors: Alekseeva, L. M.; Getling, A. V.; Savelev, V. V.
1982Ge&Ae..22..612A    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: The convective zone of the sun.
Authors: Getling, A. V.
1982IGAFS..61....3G    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: On the scales of convection flows in a horizontal layer with
    radiative energy transfer
Authors: Getling, A. V.
1980FizAO..16..529G    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: Theories of solar activity.
Authors: Getling, A. V.; Tverskoi, B. A.
1980IzSSR..44.2560G    Altcode:
  A solar dynamo model is developed which takes into account the
  relationship between global and local magnetic fields. It is shown that
  the model can explain certain aspects of solar activity. In particular,
  local magnetic fields intensified by convection cells can be the cause
  of sunspot groups. The basic features of the dynamo model are in accord
  with the features of the solar cycle: i.e., the model indicates changes
  of the sign of background fields in polar regions in each 11-year cycle,
  as well as a correlation between spot-forming activity and toroidal
  fields (whose existence in subphotospheric layers is highly probable).

---------------------------------------------------------
Title: Standing acoustic-gravity waves in the high-latitude atmosphere
    with allowance for the rotation of the earth
Authors: Alekseeva, L. M.; Getling, A. V.; Magnitskii, B. V.
1980Ge&Ae..20...72A    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: Model of an Oscillatory Hydromagnetic Dynamo. II
Authors: Getling, A. V.; Tverskoy, B. A.
1971Ge&Ae..11..330G    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: A model of an oscillating hydromagnetic dynamo. II.
Authors: Getling, A. V.; Tverskoj, B. A.
1971GeA....11..389G    Altcode: 1971Ge&Ae..11..389G
  No abstract at ADS

---------------------------------------------------------
Title: Model of an Oscillatory Hydromagnetic Dynamo. I
Authors: Getling, A. V.; Tverskoy, B. A.
1971Ge&Ae..11..176G    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: A model of an oscillating hydromagnetic dynamo. I.
Authors: Getling, A. V.; Tverskoj, B. A.
1971GeA....11..211G    Altcode: 1971Ge&Ae..11..211G
  No abstract at ADS

---------------------------------------------------------
Title: Criteria of thermal (overheat) instability of a transparent
    radiating gas.
Authors: Getling, A. V.; Kuzmin, V. V.; Tverskoj, B. A.
1971DoSSR.196...71G    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: Magnetic Fields in the Convection Cells of the Supergranulation
    Zone.
Authors: Getling, A. V.
1969SvA....12..967G    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: Solution of a class of magnetohydrodynamic problems with
    strengthening of the magnetic field.
Authors: Getling, A. V.
1969DoSSR.187..301G    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: A Possible Mechanism for Producing Sunspot Magnetic Fields.
Authors: Getling, A. V.; Tverskoi, B. A.
1968SvA....12..481G    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: Magnetic Fields in the Convection Cells of the Supergranulation
    Zone.
Authors: Getling, A. V.
1968AZh....45.1222G    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: A Possible Mechanism for Producing Sunspot Magnetic Fields.
Authors: Getling, A. V.; Tverskoi, B. A.
1968AZh....45..606G    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: Propagation of Hydromagnetic Waves in a Slightly Inhomogeneous
    Medium
Authors: Getling, A. V.
1967SvA....11..410G    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: Propagation of Hydromagnetic Waves in a Slightly Inhomogeneous
    Medium
Authors: Getling, A. V.
1967AZh....44..513G    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: Hydromagnetic Waves in a Nonisentropic Medium in the Presence
    of a Gravitational Field
Authors: Getling, A. V.
1965SvA.....9..451G    Altcode:
  No abstract at ADS

---------------------------------------------------------
Title: Hydromagnetic Waves in a Nonisentropic Medium in the Presence
    of a Gravitational Field
Authors: Getling, A. V.
1965AZh....42..568G    Altcode:
  No abstract at ADS