properties of prominence motions observed in the uv
DESCRIPTION
Properties of Prominence Motions Observed in the UV. T. A. Kucera (NASA/GSFC) E. Landi (Artep Inc, NRL). Intent of this investigation:. - PowerPoint PPT PresentationTRANSCRIPT
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Properties of Prominence Motions Observed in the UV
T. A. Kucera (NASA/GSFC)
E. Landi (Artep Inc, NRL)
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Intent of this investigation:
To make observations with which to test models of prominences formation and the nature and cause of flows in prominences by measuring the thermal and kinetic properties of moving prominence features.
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Previous observations: Prominences movies show prominences made up of moving features with velocities typically 5-20 km/s in H (sometimes faster) and often 30 km/s and higher in UV and EUV. Some of these motions apparently multi-thermal over a wide range of temperatures (104-105K), and lasting for 10s of minutes.
Question what causes motions in prominences? How can we test models of these processes?
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Simplistic Description of Model Predictions
Model Kinetic Thermal
Jets Can be quite fast
(80 km/s no problem)
If from chromosphere should show cooling
Chromospheric
evaporation
Current models, slow motions (~10 km/s)
Multi temperature blobs for extended periods, thermal structure in simple 1-D model
Wave acceleration slow motions (~10 km/s)
??
Upward magnetic field
steady models slow (~10 km/s)
Cool? heating via reconnection?
Thermal wave no Doppler shift
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Observational problem: In order to study the thermal characteristics of these motions you need to study the motions with a high temporal cadence(≥1 image/min), good spatial resolution (>2") in a range of optically thin, resolved spectral lines. This combination can’t be done in 2D with any existing instrument.
Technique: Use a UV spectrograph (SOHO/ SUMER or CDS) in sit and stare mode with a narrow slit (i.e., 1-D). Combine with imaging instrument to get 2-D information.
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ObservationsApril 17, 2003: SUMER, CDS, TRACE
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Inst. cadence spatial res.
spectral res. (FWHM)
wave
band
SUMER 90s 2" 86 mA 750-790 Å
CDS 52s 4-8" 2.6 A lines in 513-633 Å
TRACE 60-91 s 1" ------- 1600 Å
1216 Å
195 Å
Data Characteristics
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SUMER spectrum
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SUMER LinesIon Wavelength Log T (K)N III 764.34 Å 4.9N III 763.33 Å 4.9N IV 765.15 Å 5.2
S V 786.47 Å 5.2O V 760.43,760.21 Å 5.4O V 761.99 Å 5.4Ne VIII 770.42 Å 5.8Mg VIII 782.34 Å 5.9Mg VIII 762.65 Å 5.9S XI 783.01 Å 6.2
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Observations
Prominence in days before observations
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QuickTime™ and aYUV420 codec decompressorare needed to see this picture.
TRACE 1216 Å bandpass(Lyman )
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TRACE 1600 Å bandpassC IV, Si Continuum, Fe II
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TRACE 195 Å bandpassFe XII
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TRACE 1600 Å (C IV, Si Continuum, Fe II)
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SUMER N IV 765.15 Å
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Three checks for temperature variations:
•Line ratios
•Differential Emission Measure (DEM)
•Feature shifts
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Differential Emission Measure
Assumes:Ionization EquilibriumOptically thin plasmaSmooth function (spline)
No material below 104 K or above 107 K
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Summary of Observations:
Consistent with last study: Many features going ~25 km/s Visible along slit for 15 min, last longer in TRACE movie. Doppler shifted (in UV!) - real motions
8104 to 2.5 105 for one set of repeating features8104 to1.5 106 K for one abrupt featureTo within the ability to measure with the SUMER data there is no evidence of cooling with time in features D-E.
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To Do
•Complete kinetic information for sources•Continue to work on DEM for thermal energy content.
•Determine if there are any models which can predict this information.
•Coronal Evaporation Model of Antiochos et al 1999, and Karpen et al 2001 •Reconnection Jet Models (Wang 1999, Litvinenko & Martin 1999)