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Preliminary Results from Nonlinear Field Extrapolations using Hinode Boundary Data

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Karel Schrijver, Tom Metcalf, Graham Barnes, Bruce Lites, Ted Tarbell, ... Kanya Kusano, St phane R gnier, Julia Thalmann, Marcel Fuhrmann. Rationale ... – PowerPoint PPT presentation

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Title: Preliminary Results from Nonlinear Field Extrapolations using Hinode Boundary Data


1
Preliminary Results from Nonlinear Field
Extrapolations using Hinode Boundary Data
  • Marc DeRosa (LMSAL), on behalf of the NLFFF Team
  • WG1 SHINE 2007
  • Karel Schrijver, Tom Metcalf, Graham Barnes,
    Bruce Lites, Ted Tarbell, Aad van Ballegooijen,
    Jim McTiernan, Gherardo Valori, Thomas
    Wiegelmann, Mike Wheatland, Tahar Amari,
    Guillaume Aulanier, Pascal Démoulin, Kanya
    Kusano, Stéphane Régnier, Julia Thalmann, Marcel
    Fuhrmann

2
Rationale
  • Understanding the structure and evolution of the
    solar corona requires a quantitative
    understanding of the coronal magnetic field and
    its currents.
  • Nonlinear force-free fields (NLFFFs) provide a
    useful model. These are computed by
    extrapolating upward from a surface (usually
    photospheric) vector magnetogram.
  • Three popular methods
  • Optimization minimize a metric containing (? ?
    B) ? B and ? ? B
  • Current-field iteration compute field, apply
    currents, recompute field,
  • Magneto-frictional solves a MHD-like system of
    equations that include an ad-hoc friction term
    that drives the system toward a force-free state

3
Recap of previous work
  • We have previously used analytic solutions as
    blind test cases, and found that these algorithms
    are viable. However, the fields from these test
    cases do not resemble solar fields. Schrijver
    et al. 2006
  • We also tested the methods on a solar-like model,
    and found Metcalf et al. 2008
  • Correct solution is largely recovered by all
    methods when a chromospheric vector magnetogram
    is used (i.e., a magnetogram containing no net
    Lorentz force or magnetic torque).
  • Correct solution is not recovered when a
    photospheric vector magnetogram is used (i.e.,
    a magnetogram containing forces and torques).
  • Photospheric boundary data can be pre-processed
    to remove forces and torques. However, getting
    accurate measurements of physical quantities
    (such as free energies) remains difficult.

4
Hinode dataset
  • Two vector magnetograms derived from
    Hinode/SOT-SP scans bracketing X flare on 2006
    Dec 13 from AR10930
  • native spatial sampling is 0.16?0.16?
  • slit is 164? long (1024 pixels)
  • 90min for a 160?-wide scan
  • binned 44 for our purposes
  • SOT-SP magnetogram embedded in MDI magnetogram
  • resulting cutout is 320320 pixels (205?205?)
  • Links to Ca H flare movie, and to Hinode/XRT
    flare movie

5
Pre-flare magnetogram
Hinode/SOT-BFI
6
Pre-flare magnetogram
Hinode/SOT-BFI
7
2006.12.12 2030 case
2006.12.12_2030
8
Comparison with observations
  • Start with an image with prominent loops (e.g.,
    TRACE).
  • Trace some loops by hand.
  • Draw fieldlines in the model that interesect
    midpoint of each hand-traced line.
  • Determine the best-fit fieldline for each
    hand-traced fieldline.

9
Comparison with observations
  • Best match determined by evaluating length of
    several spokes in vicinity of crossing point.
  • Minimum aggregate length wins.

10
Hinode/XRT overlay - preflare
fieldlines contained within a 320320128 pixel
volume
2006.12.12_2030
11
Volume renderings of current
pre-flare
post-flare
E/Epot1.32
E/Epot1.14
12
Volume renderings of current
pre-flare
post-flare
E/Epot1.32
E/Epot1.14
13
Summary
  • NLFFF algorithms do not reach a consensus for
    this case.
  • Still, we can determine a best-matching model by
    comparing model fieldlines to observations in
    the EUV (from TRACE) and/or in x-rays (from
    Hinode/XRT).
  • In the best-matching model, free energy drops
    from 32 to 14 of potential energy,
    corresponding to a drop in free energy of 3?1032
    erg, even as total field energy increased by
    1032 erg during this time.
  • Issue 1 EUV and x-ray coverage was not optimal
    for this region, making it hard to determine
    best-fit model. (TRACE had only 285 binned 2?2,
    and x-ray images not the best for identifying
    loops.)
  • Issue 2 Lower boundary did not fully contain
    both flare ribbons. We are currently enlarging
    the lower boundary footprint and will repeat the
    analysis.
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