Mechanism for the formation of the daytime trough in the winter in the Southern Hemisphere

Details Mechanism for the formation of the daytime trough in the winter in the Southern Hemisphere Mechanism for the formation of the daytime trough in the winter in the Southern Hemisphere

Dec 1990

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1990ge%26ae..30..958g&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 30, Nov.-Dec. 1990, p. 958, 959. In Russian.

Computer Science

Sound

Auroras, Electron Density Profiles, Ionospheric Electron Density, Satellite Observation, Southern Hemisphere, Atmospheric Sounding, Cosmos Satellites, Solar Activity

Scientific paper

Latitudinal profiles of electron density determined by the Cosmos-900 Satellite in the Southern Hemisphere are compared with model calculations. It is found that the formation of the subauroral daytime trough in the winter is associated with the absence of an effective ionization source in the 'polar shadow' region which forms in the daytime sector (14-18 UT) in the course of the earth's diurnal rotation.

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