Computer Science
Scientific paper
Aug 1981
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1981ge%26ae..21..683v&link_type=abstract
Geomagnetizm i Aeronomiia, vol. 21, July-Aug. 1981, p. 683-688. In Russian.
Computer Science
1
Atmospheric Circulation, Atmospheric Composition, Equations Of Motion, Neutral Gases, Thermosphere, Vertical Distribution, Diffusion Coefficient, Nitrogen, Oxygen, Turbulent Diffusion
Scientific paper
A nonstationary solution is obtained for equations of motion and continuity for the basic neutral components O, O2, and N2 in the 80-300 km height region under various conditions (e.g., fluxes of UV radiation, and height profiles of the turbulent diffusion coefficient). Results from the complete system of equations are compared with solutions in various approximations. It is shown that vertical distributions of O and O2 concentrations, corresponding to the solution of the complete system, differ considerably from vertical profiles of these concentrations calculated in the small-impurity approximation, the Friedman approximation, and the Kolegrov approximation.
Davydov V. E.
Vlasov Michael N.
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