modeling long-lived “super-hydrostatic” active region loops

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Modeling Long-Lived “Super- Hydrostatic” Active Region Loops Harry Warren Amy Winebarger John Mariska Naval Research Laboratory Washington, DC Solar-B Science Meeting Japan February 3-5, 2003 Heating Function? E H (s,t)

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Heating Function? E H (s,t). Modeling Long-Lived “Super-Hydrostatic” Active Region Loops. Harry Warren Amy Winebarger John Mariska Naval Research Laboratory Washington, DC Solar-B Science Meeting Japan February 3-5, 2003. - PowerPoint PPT Presentation

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Page 1: Modeling Long-Lived “Super-Hydrostatic” Active Region Loops

Modeling Long-Lived “Super-Hydrostatic” Active Region Loops

Harry Warren Amy Winebarger

John Mariska

Naval Research LaboratoryWashington, DC

Solar-B Science MeetingJapan

February 3-5, 2003Heating Function? EH(s,t)

Page 2: Modeling Long-Lived “Super-Hydrostatic” Active Region Loops

Motivation: Understanding the properties of active region loops observed with TRACE

Aschwanden et al., 2001, ApJ, v550, p1036

Page 3: Modeling Long-Lived “Super-Hydrostatic” Active Region Loops

Static Models Don’t Work!

RTVS (uniform heating) scaling law predicts very low densities for long loops.

TRACE observations show nobs/nuni ~ 100!

RTVS (foot point heating) scaling law gives densities that are higher, but only by a factor of about ~3. Highly localized footpoint heating → instability.

Winebarger et al., ApJ, in press

Page 4: Modeling Long-Lived “Super-Hydrostatic” Active Region Loops

Impulsive Heating Steady Heating

n ≈ T1/2 n ≈ T2

10 MK → 1 MK

n → n/3

10 MK → 1 MK

n → n/100

Dynamic solutions can be much denser than static solutions

Rosner et al., 1978, ApJ, 220, 643Cargill et al., 1995, ApJ, 439, 1034

Warren et al., 2002, ApJL, v570, p41

Page 5: Modeling Long-Lived “Super-Hydrostatic” Active Region Loops

Cooling loops can be overdense near 1 MK

Page 6: Modeling Long-Lived “Super-Hydrostatic” Active Region Loops

Loops cool faster than they drain

Page 7: Modeling Long-Lived “Super-Hydrostatic” Active Region Loops

Simulated TRACE light curves

Delay between the appearance of the

loop in 195 and 171

Page 8: Modeling Long-Lived “Super-Hydrostatic” Active Region Loops

4-Jul-1998 (Aschwanden Loop #23)

Winebarger et al., ApJ, submitted

Page 9: Modeling Long-Lived “Super-Hydrostatic” Active Region Loops

18-Aug-1998 (Aschwanden Loop #2)

Page 10: Modeling Long-Lived “Super-Hydrostatic” Active Region Loops

Simulated loop cools too fast!

EF = 2 ergs cm-3 s-1, δ = 680 s

Page 11: Modeling Long-Lived “Super-Hydrostatic” Active Region Loops

Not one loop, many filaments? – Consistent with the light curve

10 filaments, EF ≈ 0.2-2 ergs cm-3 s-1, δ = 680 s

Page 12: Modeling Long-Lived “Super-Hydrostatic” Active Region Loops

Filaments lead to flat filter ratios

Page 13: Modeling Long-Lived “Super-Hydrostatic” Active Region Loops

SXT→TRACE Loops

Page 14: Modeling Long-Lived “Super-Hydrostatic” Active Region Loops

SXT→TRACE Loops

Page 15: Modeling Long-Lived “Super-Hydrostatic” Active Region Loops

Light curves of loop cooling from SXT to TRACE

Page 16: Modeling Long-Lived “Super-Hydrostatic” Active Region Loops

Single cooling loop produces too much intensity in TRACE

Page 17: Modeling Long-Lived “Super-Hydrostatic” Active Region Loops

SXT/TRACE intensity ratios are consistent with filamentation

Page 18: Modeling Long-Lived “Super-Hydrostatic” Active Region Loops

Conclusions/Implications for Solar-B

Dynamics and filamentation are important in determining what is observed

EIS+XRT+SOT will provide an unprecedented opportunity to study the dynamical evolution of active region loops

More modeling is needed to identify signatures of coronal heating