Physics
Scientific paper
Sep 1961
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1961saosr..75.....n&link_type=abstract
SAO Special Report #75 (1961)
Physics
9
Scientific paper
Atmospheric models based on diffusion equilibrium in which helium plays a role are derived by use of heat conduction as the essential process that determines the gradient of temperature. Introduction of boundary conditions at 120 km, where diffusion begins for major constituents, leads to atmospheric models that can be used for analysis of variations of day-to-night and solar activity in the whole thermosphere from 150 km to 2000 km. Physical parameters such as density, pressure, concentration, mean molecular mass, and local scale height are given as functions of the temperature, which is considered the fundamental parameter.
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