Disturbed large-scale eddy in the ionosphere

Details Disturbed large-scale eddy in the ionosphere Disturbed large-scale eddy in the ionosphere

Oct 1983

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1983ge%26ae..23..858g&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 23, Sept.-Oct. 1983, p. 858, 859. In Russian.

Computer Science

Annual Variations, Diurnal Variations, E Region, F Region, Ionospheric Disturbances, Vortices, Atmospheric Circulation, Velocity Distribution, Vertical Distribution, Wind Velocity

Scientific paper

An analysis is made of vertical profiles of velocity components and of the diurnal and seasonal behavior of the distributed nongeostrophic large-scale eddy in the E and F regions. It is shown that below 270 km the role of the ionospheric plasma mainly consists in a twisting effect, with velocities reaching a maximum at 200 km. Above 270 km the role of inductive deceleration increases sharply, leading to a significant decrease of wind velocity with height.

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