The effect of the large ion temperature differences on the solutions of diffusion and continuity equations

Details The effect of the large ion temperature differences on the solutions of diffusion and continuity equations The effect of the large ion temperature differences on the solutions of diffusion and continuity equations

Jan 1988

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1988jatp...50...33g&link_type=abstract

Journal of Atmospheric and Terrestrial Physics (ISSN 0021-9169), vol. 50, Jan. 1988, p. 33-40.

Physics

Atmospheric Diffusion, Earth Ionosphere, Ion Temperature, Numerical Weather Forecasting, Temperature Gradients, Atmospheric Composition, Atmospheric Models, Hydrogen Ions, Oxygen Ions

Scientific paper

Diffusion and continuity equations for O(+) and H(-) ions were integrated along a magnetic field line between 500 and 3000 km. Three sets of equations were used: (1) the standard ones; (2) modified according to the formulas given by St.-Maurice and Schunk (1977); and (3) those derived by Conrad and Schunk (1979). The differences between solutions obtained for each set of equations and the importance of the modifications introduced in the diffusion equations are discussed.

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