Static Diffusion Models of the Upper Atmosphere with Empirical Temperature Profiles

Computer Science

Scientific paper

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Scientific paper

Tables of atmospheric density and composition are computed for a wide range of exospheric temperatures, starting from a fixed set of boundary conditions at 120 km. The diffusion equation is integrated following empirical temperature profiles of exponential form capable of reproducing the densities derived from satellite drag over the years. Formulas are given that relate the exospheric temperature to solar and geomagnetic activity and allow for the diurnal and semiannual variations. The different response of the density at the 200-km level to different types of heating is briefly discussed.

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