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The Effect of Sub-surface Fields on the Dynamic Evolution of a Model Corona

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To model the evolution of the coronal magnetic field as eruptive events occur ... of the models by simulating known eruptive events and comparing model data with ... – PowerPoint PPT presentation

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Title: The Effect of Sub-surface Fields on the Dynamic Evolution of a Model Corona


1
The Effect of Sub-surface Fields on the Dynamic
Evolution of a Model Corona
  • Goals
  • To predict the onset of a CME based upon
    reliable measurements of photospheric magnetic
    field
  • It may be possible to obtain a
    velocity field via LCT, feature tracking,
  • or spectroscopic measurements
  • To model the evolution of the coronal magnetic
    field as eruptive events occur
  • To test reliability of the models by simulating
    known eruptive events and comparing model data
    with existing observational data
  • MURI candidate event AR8210 May 1
    1998

2
First Step
  • Use dynamic sub-surface models of active region
    evolution to drive the model corona.
  • Though it is possible to truly couple
    numerical models via a domain decomposition
    framework such as PARAMESH, we will not have the
    freedom to allow our coronal model to affect the
    observationally obtained photospheric boundary
    --- thus we must explore the consequences of
    driving a model corona without allowing
    feedback into the photospheric zones
  • A distinct advantage of this approach
  • Sub-surface code provides for self-consistent
    magnetic fields and flows throughout the boundary
    layers
  • eg. The induction equation is automatically
    satisfied throughout the
  • boundary layers

3
Approach
  • Use a compressible MHD code (eg. Zeus3D, ZeusAMR,
    ARMS) to model the dynamic evolution of the
    magnetic field in the low-beta corona above an
    active region
  • Since vector magnetograms are measures of the
    magnetic field in the photosphere, reliable
    models must
  • 1. Include in the computational domain
    the geometrically thin transition layers between
    the photosphere (where Hp102km, and the plasma
    beta is of order unity) along with the low-beta
    corona.
  • 2. Approximate (or treat exactly) the
    effects of optically thin radiative cooling, and
    thermal conduction in the transition layers so as
    to maintain a physical temperature and pressure
    stratification
  • 3. Require that magnetic field is known
    along only a single slice in the photospheric
    layers of the simulation domain, and no
    additional sub-surface information is available



  • some chromospheric measurements available

4
Results1
1. From Abbett Fisher 2003 (Jan 1) ApJ (in
press)
5
Results
  • The presence and distribution of boundary flows
    (particularly the component of the flow
    perpendicular to the boundary) are of great
    importance to the dynamic emergence process,
    since (in an ideal calculation) such a flow is
    necessary to transport magnetic field into the
    model corona while conserving flux.
  • As the apex of a (slightly) twisted Omega-loop
    emerges into the corona, the simulations suggest
    that in most regions surrounding the emerging
    structure, the field configuration differs from a
    force-free (or potential) configuration

6
Second Step AR8210 (May 1 1998 1940)
  • A significant challenge
  • Only the photospheric magnetic field is known.
    Since boundary flows are important to the
    dynamics of the coronal simulation, we must
    specify a self-consistent velocity field in the
    boundary layers that (at least) satisfies the
    vertical component of the induction equation
  • Options
  • 1. LCT (does NOT guarantee consistency)
  • 2. Feature tracking (does NOT guarantee
    consistency)
  • 3. MEF method (DOES guarantee
    consistency)
  • theoretical method that generates a velocity
    field given the vector magnetic field along a
    2D slice with the constraint that kinetic energy
    is minimized --- does guarantee consistency, but
    the calculated flow field is part of a family of
    solutions and may not necessarily represent the
    true flows present in AR8210.

7
MEF method (D. Longcope)
8
AR8210
  • The initial atmosphere must be specified
  • 1. Potential field extrapolation
  • 2. Force-free model
  • Initial dynamic run --- uses MEF method at the
    photospheric boundary with an initial FFF
    atmosphere provided by S. Regnier

9
Toward comparison with observational data
---Calculating temperatures and emissivities a
posteriori along model coronal loops (L.
Lundquist)
1401
1940
1757
2112
Yohkoh SXT 01 May 1998
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