The Dynamic Chromosphere

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The Dynamic Chromosphere Mats Carlsson Institute of Theoretical Astrophysics, University of Oslo JAXA, November 20 2008

description

The Dynamic Chromosphere. Mats Carlsson Institute of Theoretical Astrophysics, University of Oslo JAXA, November 20 2008. Semi-empirical model. VAL3C. Ca II H-line intensity. 1D NLTE hydrodynamic modelling. SUMER observations. Carlsson, Judge, Wilhelm 1997. Ca H timeseries from Hinode. - PowerPoint PPT Presentation

Transcript of The Dynamic Chromosphere

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The Dynamic Chromosphere

Mats CarlssonInstitute of Theoretical Astrophysics, University of

OsloJAXA, November 20 2008

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Semi-empirical model

VAL3C

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Ca II H-line intensity

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1D NLTE hydrodynamic modelling

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SUMER observations

Carlsson, Judge, Wilhelm 1997

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Ca H timeseries from Hinode

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•Broad band filter contains too much photospheric signal for chromospheric diagnostics on-disk

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3D models from convection zone to corona

•16x8x16 Mm (2 Mm below, 14 Mm above z=0)

•Open boundaries

•Detailed radiative transfer along 48 rays

•Multi-group opacities (4 bins) with scattering

•NLTE radiative losses in chromosphere (CaII, H)

•Optically thin losses in corona

•Conduction along field-lines

•Various initial magnetic field configurations

•No imposed driving (selfconsistent convection)

Hansteen 2004, Hansteen, Carlsson, Gudiksen 2007, Sykora, Hansteen, Carlsson 2008

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Ca H timeseries from Hinode

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Ca-H timeseries from model

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Red field lines

Coloring is temperature

(red=chromosphere

green/blue= TR)

Carlsson & Hansteen

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Heating of the middle chromosphere

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•Chromosphere highly dynamic and filamentary

•Hot and cool gas coexist

•Non-magnetic chromosphere may be wholly dynamic

•Magnetic fields crucial for the understanding of chromospheric heating, dynamics and connection with upper layers

•Network chromosphere and internetwork mid-upper chromosphere magnetically heated

•Whole zoo of wavemodes

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Ca emission at the limb

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What can be done from the ground?

•Limb: scattering in atmosphere, difficult with adaptive optics

•Spectroscopy: Image restorations difficult

•Fabry-Perot: Hα, CaII 8542, photosphere

Examples taken from Oslo-group observations at the Swedish 1m Solar Telescope (SST) on La Palma

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Hα blue wing at SST, Aug 10, 2007

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SST: CaII 866.2

Red Blue

Spectroscopy

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Fabry-Perot

•Swedish 1m Solar Telescope on La Palma

•CRISP

•Ca II 854.2 nm, spectral resolution 90 mÅ

•29 line positions -1900 mÅ to +1900 mÅ, step 100-200 mÅ, 11s cadence (full scan)

•24 line positions -900 mÅ to +190 mÅ, step 50 mÅ, 9s cadence (full scan), 33 min timeseries

•diffraction limited (0.21”) (after MOMFBD restoration), 0.071”/pixel, FOV 66”x67”

• June 13-15 2008

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Hα observations with SST

• June 15th 2008

•CRISP Fabry-Perot

•25 line positions -1800mÅ to +800mÅ, step 100mÅ, spectral resolution 60mÅ

•6.7s cadence (full scan), 30 minutes timeseries

•diffraction limited (0.16”), 0.071”/pixel, FOV 66”x67”

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Hα line center

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-800 mÅ

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+800 mÅ

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Why space?

•UV gives much better diagnostics for the chromosphere (91.2-152 nm, Mg II 280 nm)

•spectroscopy

•observing across β=1

•coupling to transition region-corona

•consistent time-series of any target

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What do we need?•UV

•High spatial and temporal resolution

•0.2”, 1-10s

•Spectroscopic capability

• line shapes, 1 km/s

•Polarimetry

•3D radiation-MHD combined with 3D NLTE modelling

•20 km resolution: 10243 : 4 months on 1000 cores

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Conclusions

•Chromosphere is very dynamic and structured with small scales

•Absolutely essential to have diagnostics from chromospheric plasmas together with higher temperature plasmas

•Need 3D radiation-MHD modelling

•Need mission like Solar-C plan B