Choice of lower boundary conditions for modeling atmospheric energetics at heights of 50-500 km

Details Choice of lower boundary conditions for modeling atmospheric energetics at heights of 50-500 km Choice of lower boundary conditions for modeling atmospheric energetics at heights of 50-500 km

Dec 1978

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1978ge%26ae..18.1119b&link_type=abstract

Geomagnetizm i Aeronomiia, vol. 18, Nov.-Dec. 1978, p. 1119-1121. In Russian.

Computer Science

Atmospheric Heating, Atmospheric Models, Boundary Conditions, Boundary Value Problems, Turbulent Diffusion, Atmospheric Temperature, Diffusion Coefficient, Nitrogen, Oxygen Atoms, Ozone, Steady State

Scientific paper

The proposed model of a steady-state atmosphere sets the lower boundary condition for the temperature and the turbulence diffusion coefficient as a function of the height. Equations are introduced which refer to four components - O, O2, N2, and O3. Forms of heating are considered, and calculated temperature profiles are compared with an observed profile.

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