The signature of chromospheric heating in Ca II H spectra

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Issue		A&A Volume 479, Number 1, February III 2008


Page(s)		213 - 227
Section		The Sun
DOI		http://dx.doi.org/10.1051/0004-6361:20078410

A&A 479, 213-227 (2008)
DOI: 10.1051/0004-6361:20078410

The signature of chromospheric heating in Ca II H spectra

C. Beck^{1, 2}, W. Schmidt², R. Rezaei², and W. Rammacher²

¹ Instituto de Astrofísica de Canarias (CSIC), Via Lactea, 38205 La Laguna, Tenerife, Spain
e-mail: cbeck@iac.es
² Kiepenheuer-Institut für Sonnenphysik, Schöneckstr. 6, 79104 Freiburg, Germany
e-mail: [wolfgang;rrezaei;wr]@kis.uni-freiburg.de

(Received 3 August 2007 / Accepted 22 October 2007)

Abstract
Context.The heating process that balances the solar chromospheric energy losses has not yet been determined. Conflicting views exist on the source of the energy and the influence of photospheric magnetic fields on chromospheric heating.
Aims.We analyze a 1-h time series of cospatial $\ion{Ca}{ii}$ H intensity spectra and photospheric polarimetric spectra around 630 nm to derive the signature of the chromospheric heating process in the spectra and to investigate its relation to photospheric magnetic fields. The data were taken in a quiet Sun area on disc center without strong magnetic activity.
Methods.We have derived several characteristic quantities of $\ion{Ca}{ii}$ H to define the chromospheric atmosphere properties. We study the power of the Fourier transform at different wavelengths and the phase relations between them. We perform local thermodynamic equilibrium (LTE) inversions of the spectropolarimetric data to obtain the photospheric magnetic field, once including the Ca intensity spectra.
Results.We find that the emission in the $\ion{Ca}{ii}$ H line core at locations without detectable photospheric polarization signal is due to waves that propagate in around 100 s from low forming continuum layers in the line wing up to the line core. The phase differences of intensity oscillations at different wavelengths indicate standing waves for $\nu <$ 2 mHz and propagating waves for higher frequencies. The waves steepen into shocks in the chromosphere. On average, shocks are both preceded and followed by intensity reductions. In field-free regions, the profiles show emission about half of the time. The correlation between wavelengths and the decorrelation time is significantly higher in the presence of magnetic fields than for field-free areas. The average $\ion{Ca}{ii}$ H profile in the presence of magnetic fields contains emission features symmetric to the line core and an asymmetric contribution, where mainly the blue H $_{\rm 2V}$ emission peak is increased (shock signature).
Conclusions.We find that acoustic waves steepening into shocks are responsible for the emission in the $\ion{Ca}{ii}$ H line core for locations without photospheric magnetic fields. We suggest using wavelengths in the line wing of $\ion{Ca}{ii}$ H, where LTE still applies, to compare theoretical heating models with observations.

Key words: Sun: chromosphere -- Sun: oscillations

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