Effects of large zonal plasma drifts on the subauroral ionosphere

Details Effects of large zonal plasma drifts on the subauroral ionosphere Effects of large zonal plasma drifts on the subauroral ionosphere

Jul 1991

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1991jatp...53..557s&link_type=abstract

(Thermospheric and ionospheric dynamics; Symposium, Exeter, England, July 1989, Selected Papers. A92-10626 01-46) Journal of Atm

Physics

25

Auroral Zones, Earth Ionosphere, F Region, Ionospheric Heating, Plasma Drift, Plasmasphere, Atmospheric Composition, Ion Temperature, Ionospheric Ion Density, Oxygen Ions

Scientific paper

A model of the earth's ionosphere and plasmasphere is used to investigate the effects of an imposed westward plasma drift of maximum velocity 2 km/s. A closed subauroral tube of plasma is considered and the velocity spike persists for 10 min. Ion-neutral frictional heating causes rapid elevation of the F-region O(+) temperature. The F-layer O(+) concentration is decreased due to increased O(+) loss rate and rapid ion flows both upward and downward from the F-region. The upward flux of O(+) through the topside ionosphere can each 5 x 10 exp 9/sq cm/s; when the velocity spike ceases there is a return flow of O(+) that tends to replenish the F-layer. Most of the features revealed by the model for the F-region and topside ionosphere are in accord with observations of subauroral ion drifts. Downward flows that are predicted to be persistently present around the 300 km altitude level appear to agree with observations only occasionally; suggestions are made to resolve this discrepancy.

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