Toward an explanation of longitudinal variations of f0E and f0F2 in the Eurasian region

Details Toward an explanation of longitudinal variations of f0E and f0F2 in the Eurasian region Toward an explanation of longitudinal variations of f0E and f0F2 in the Eurasian region

Jan 1989

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1989ge%26ae..29...56g&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 29, Jan. 1989, p. 56-59. In Russian.

Computer Science

Sound

E Region, F 2 Region, Ionospheric Electron Density, Longitude, Atmospheric Circulation, Atmospheric Models, Atmospheric Temperature, Ionospheric Sounding, Thermosphere

Scientific paper

Calculations of electron density at the E and F2 layer maxima based on a current thermosphere model (Kohnlein, 1980) are compared with multiyear vertical-sounding observations over the Eurasian region. It is shown that existing hypotheses about longitudinal effects of a geomagnetic nature are insufficient to explain the observed phenomena. Instead, it is proposed that the planetary structure of circulation, temperature, and composition in the upper atmosphere contains a smaller-scale component of meteorological fields than that yielded by currently used thermosphere models.

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