Computer Science
Scientific paper
Oct 1987
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1987ge%26ae..27..728b&link_type=abstract
Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 27, Sept.-Oct. 1987, p. 728-734. In Russian.
Computer Science
2
Annual Variations, Atmospheric Models, F 2 Region, Solar Terrestrial Interactions, Spatial Distribution, Northern Hemisphere, Polar Regions, Solar Activity Effects, Temporal Distribution
Scientific paper
Results of the empirical modeling of cyclic and seasonal variations of the daytime regular F2-layer are presented. It is shown that the formation of the seasonal anomaly in years of high solar activity is determined mainly by a summer anomaly. This summer anomaly is connected with an increase in the content of molecular nitrogen in the polar ionosphere during summer months due to additional heating and turbulent mixing in connection with intense dissipation of the three-dimensional current system under high-conductivity conditions. In solar-minimum years the seasonal anomaly is determined mainly by seasonal variations of the composition of the neutral atmosphere in the passage from winter to summer.
Besprozvannaia A. S.
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