Magnetic storm dynamics of the thermosphere

Physics

Scientific paper

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Atmospheric Heating, Diurnal Variations, Ionospheric Disturbances, Magnetic Storms, Resistance Heating, Thermosphere, Atmospheric Circulation, Atmospheric Composition, Atmospheric Models, Electric Fields, Electron Precipitation, F 2 Region, Ogo-6, Ohmic Dissipation, Satellite Observation

Scientific paper

A theoretical study of the Dst component of magnetic storms is presented. The dynamic characteristics are found significantly different for Joule dissipation and electron precipitation, leading to the conclusion that the former is probably the predominant heat source for the upper thermosphere. Composition measurements on OGO-6, which reveal markedly different characteristics in N2, O and He, can be explained on the basis of energy advection and diffusive mass transport by thermospheric winds. Essential features in the F2-region response are explicable in terms of these dynamic processes. Electric field induced motions are estimated and it is concluded that resultant adiabatic heating could be significant.

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