Supergranulation-Scale Solar Convection Simulations - PowerPoint PPT Presentation

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Supergranulation-Scale Solar Convection Simulations

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3rd order Runga-Kutta. Equation of state. tabular ... Components Composite : Uz at 17.3 Mm. Mean Atmosphere State. Temperature, Density and Pressure ... – PowerPoint PPT presentation

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Title: Supergranulation-Scale Solar Convection Simulations


1
Supergranulation-Scale Solar Convection
Simulations
  • David Benson, Michigan State University, USA
  • Robert Stein, Michigan State University, USA
  • Aake Nordlund, Astronomical Observatory, NBIfAFG,
    Denmark
  • AGU - SPD Conference May, 2005 New
    Orleans, LA

2
Overview
  • Purpose
  • Computational Methodology (brief)
  • Methods for Initializing Simulations
  • Preliminary Results Simulations In-Progress
  • 50Mm x 50Mm x 20Mm (deep) simulations
  • Relaxing thermally and dynamically
  • Future Directions

3
Significance and Questions
  • Second Helium Ionization Zone
  • Separate the role of second helium ionization
    zone from the effect of the increasing scale
    height with depth
  • Helioseismology
  • Simulations serve as a tool for analyzing local
    helioseismic inversion techniques
  • Nature of the Surface Shear Layer
  • Development and Maintenance of the Magnetic
    Network

4
Computational Domain
  • 50Mm x 50Mm x 20Mm
  • 5003 grid points
  • Grid clustering near visible surface

Computational Domain for the CFD Simulations of
Solar Convection
5
Numerical Method
  • Spatial differencing
  • 6th-order centered f.d.
  • staggered
  • Time advancement
  • 3rd order Runga-Kutta
  • Equation of state
  • tabular
  • including ionization
  • H, He abundant elements
  • Radiative transfer
  • 3D, LTE
  • 4 bin opacity distrib. fxn
  • Quenching

6
Computational Information
  • Fortran 90
  • Parallelized - OpenMP
  • single parallel region
  • Michigan State University
  • 64 processor Altix
  • NCSA
  • IBM P690
  • NASA Ames
  • Altix (128 processors)
  • Objective
  • layer MPI on top of the OpenMP

7
Initialization Methods
  • 24 Mm and 12 Mm Simulations
  • 12 Mm simulation (9 Mm deep)
  • well-relaxed
  • extended adiabatically to 20 Mm
  • Relax dynamics 12 Mm -- 20 Mm deep
  • Create 24 Mm wide box - and relax the following
  • 12 Mm stretched to 24Mm
  • generates large scale structure
  • 12 Mm doubled to 24 Mm

8
Initialization Methods
  • Construction of 50 Mm Initial State
  • Stretch 12 Mm x 20 Mm to 50 Mm
  • Generates large scale structure
  • Breaks symmetry
  • Stretch 24 Mm x 20 Mm to 50 Mm
  • Generates intermediate level structure
  • Quadruple 12 Mm x 20 Mm to 50 Mm
  • Produces small scale structure
  • Combine Relax

9
Initialization Snapshots
  • Components Composite Uz at 0.25 Mm

Snapshots of methods composite (?)
10
Initialization Snapshots
  • Components Composite Uz at 17.3 Mm

11
Mean Atmosphere State
  • Temperature, Density and Pressure

12
Mean Atmosphere State
  • Ionization of H and He

13
Energy Fluctuation
  • Need for Relaxation

14
Future Research Direction
  • Relax hydrodynamic simulations (further)
  • Implement magnetic field boundary conditions and
    add Coriolis force terms
  • Results will be available to help in answering
    questions about ...
  • Maintenance of magnetic network
  • f-plane rotation -- Coriolis force
  • Local helioseismic inversion techniques
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