Physics
Scientific paper
Nov 1980
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1980soph...68..125a&link_type=abstract
Solar Physics, vol. 68, Nov. 1980, p. 125-133. NSF-sponsored research;
Physics
11
Atmospheric Heating, Chromosphere, Hydrogen Ions, Radiant Cooling, Solar Atmosphere, Atmospheric Models, Radiant Heating, Solar Physics, Thermodynamic Equilibrium
Scientific paper
The controversial problem of H(-) radiative cooling in the solar chromosphere is examined. It is found, in agreement with Praderie and Thomas (1972, 1976), that H(-) is a substantial source of radiative heating in the outer atmosphere, especially when departures from LTE are important. The role of H(-) as a chromospheric heating agent must be considered carefully before net radiative cooling rates can be assessed from empirical chromospheric models, or calculations of nonradiative heating, for example by acoustic waves, can be pursued meaningfully.
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