Effect of magnetospheric convection on the large-scale structure of the high-latitude ionosphere

Details Effect of magnetospheric convection on the large-scale structure of the high-latitude ionosphere Effect of magnetospheric convection on the large-scale structure of the high-latitude ionosphere

Feb 1988

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1988ge%26ae..28...50k&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 28, Jan.-Feb. 1988, p. 50-54. In Russian.

Physics

Convective Flow, Earth Magnetosphere, Ionospheric Disturbances, Polar Regions, Atmospheric Models, Differential Equations, Magnetohydrodynamic Flow, Mathematical Models

Scientific paper

The effect of magnetospheric convection on the macrostructure of the polar ionosphere is analyzed on the basis of a mathematical model of the ionosphere which self-consistently describes composition, dynamics, and thermal conditions in the three-dimensional case for average heliogeophysical conditions. It is shown that the main ionospheric trough does not disappear even in the complete absence of convective plasma motion, which affects only the longitidunal extent of the trough.

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