Plasmapause asymmetry effect in the localization of the main ionospheric trough

Details Plasmapause asymmetry effect in the localization of the main ionospheric trough Plasmapause asymmetry effect in the localization of the main ionospheric trough

Apr 1985

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1985ge%26ae..25..320k&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 25, Mar.-Apr. 1985, p. 320-322. In Russian.

Computer Science

Sound

Ionospheric Disturbances, Plasmapause, Troughs, Winter, Asymmetry, Diurnal Variations, Ionospheric Electron Density

Scientific paper

The plasmapause asymmetry effect in the localization of the main ionospheric trough (MIT) is investigated on the basis of a high-latitude model which takes into account the noncoincidence of geographic and geomagnetic coordinates for winter (delta = -23 deg) and solar minimum conditions; data from vertical-sounding stations of the Iakutsk meridional chain for December 1973 are used. A comparison of calculations with experimental data shows that the observed narrowing of the MIT at midnight is due to plasmapause asymmetry relative to the geomagnetic pole. This narrowing 'divides' the MIT bottom into evening and morning hours, forming 'holes' in the ionosphere.

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