A mechanism for deep chromospheric heating during solar flares

Astronomy and Astrophysics – Astrophysics

Scientific paper

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Atmospheric Heating, Chromosphere, Hydrogen Ions, Solar Atmosphere, Solar Flares, Ultraviolet Absorption, Electron Density (Concentration), Energy Distribution, Ionization Potentials, Solar Temperature

Scientific paper

The authors reexamine the role of the negative hydrogen ion, H-, in the energy balance of the deep solar chromosphere and find, in contrast with earlier authors, that H- is a source of heating in these levels. The response of this region to an ionizing flux of flare-associated UV radiation (1500 ⪉ λ ⪉ 1900 Å) is then addressed: the authors find that the excess ionization of Si to Si+ increases the local electron number density considerably, since most species are largely neutral at deep chromospheric levels. This in turn increases the electron-hydrogen atom association rate, the H- abundance, and the rate of absorption of photospheric radiation by this ion. The authors find that the excess absorption by this process may lead to a substantial temperature enhancement at temperature minimum levels during flares.

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