The Wide Slit

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CDS users meeting CDS users meeting 21st Sept 2005 21st Sept 2005 Imaging The Active Region TR Imaging The Active Region TR With The CDS Wide Slit With The CDS Wide Slit Mike Marsh Centre for Astrophysics, University of Central Lancashire, Preston, UK

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Imaging The Active Region TR With The CDS Wide Slit Mike Marsh Centre for Astrophysics, University of Central Lancashire, Preston, UK. The Wide Slit. Mg IX 368 Å. He I 584 Å. O V 629 Å. 90˝ × 240˝ FOV 26s cadence Produces intensity images (not rastered) in He I, O V & Mg IX - PowerPoint PPT Presentation

Transcript of The Wide Slit

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Imaging The Active Region TR Imaging The Active Region TR With The CDS Wide SlitWith The CDS Wide Slit

Mike Marsh

Centre for Astrophysics, University of Central Lancashire, Preston, UK

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The Wide Slit

Mg IX368 Å

He I584 Å

O V629 Å

•90˝× 240˝ FOV•26s cadence•Produces intensity images (not rastered) in He I, O V & Mg IX•But no spectral data

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Wide Slit Calibration

Mg IX uncalibrated Mg IX calibrated

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AR 10570

TRACE 171 Å

TRACE 1600 Å

TRACE WLEIT 171 Å

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AR 10570

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TRACE 1600 Å

TRACE 1600 +171 Å

TRACE 1600 +O V

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Composite MovieTRACE 1600 Å O V TRACE 171 Å

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Composite MovieO V TRACE 171 Å

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Rastered data

Rastered data gains line profile data, but loses time variability information

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MDI WL + O V + 171TRACE 171 + O

VTRACE 171

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Fourier power maps

Power significant to 95%

3 min band (4.7 – 6.6 mHz) (150 – 210 s)

3-min umbral oscillationsBeckers & Tallant (1969), Gurman (1982), Fludra (2001), Brynildsen (2002)

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3 min He I time series

• He I oscillation amplitude ~2%

• FFT has 2 dominant periods ~(6.1 & 7.1) mHz(140 & 160) Seconds

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3 min O V time series

• O V oscillation amplitude ~4%

• FFT has 2 dominant periods ~(5.9 & 7.3) mHz(140 & 170) Seconds

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AR 10570 with TRACE

~80 kms-1 projected velocity cf. De Moortel et al. (2002) Robbrecht et al. (2001)

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3 min TRACE 171 time series

• TRACE oscillation amplitude ~3%

• FFT has 3 dominant periods ~(3, 5.9 & 7.3) mHz(330, 140 & 170) Seconds

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Conclusions

• Chromospheric/TR Acoustic Waves (Brynildsen, 2004)

• Waves propagate through chromosphere, TR and into the corona

• 3 min oscillations above sunspot umbra in the Chromosphere & TR where the umbral magnetic field is vertical

• Oscillations observed as 3 min propagations at TRACE temperatures where the field is more inclined.

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Acoustic Energy Flux

22

1332

64

I

I

m

TkN

kxtiVeV '

VV 2

2

1

• Assuming acoustic waves with velocity and pressure perturbations V' and P'

• The energy flux of the wave ε is given by:

kxtiPeP '

Assuming:• Optically thin emission →• Ideal gas• Complete ionisation of the plasma & Relative

abundances X=0.9 Y=0.1→

The energy flux of the wave is given by:

2I

eNN 91.0 pmm 29.1

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Acoustic Energy Flux

Log T (K) Log N (cm-3) ΔI/I ε (erg cm-2 s-1)

He I 4.5 10.959 0.02 28.3

O V 5.4 9.859 0.04 201.0

TRACE 171Å 6.0 9.259 0.03 225.6

O VDoyle (2003) derive Ne in sunspot plumes using O V diagnostic

TRACE 171Del Zanna (2003) derive Ne in the footpoints of quiescent coronal loops

He IEstimated Log Ne=11cm-3 for active regions

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Conclusion

• Acoustic waves propagate through chromosphere, TR and into the corona

• Acoustic waves are insufficient to heat active regions

• Technique may be used as a seismological tool to determine plasma properties ρ, T,…

• If ε constant through the atmosphere; may allow derivation of Ne at He I temperatures

• Need active region Ne measurement at He I temperatures