Variations of aeronomic parameters in the upper D-region

Details Variations of aeronomic parameters in the upper D-region Variations of aeronomic parameters in the upper D-region

Oct 1989

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1989ge%26ae..29..812k&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 29, Sept.-Oct. 1989, p. 812-817. In Russian.

Mathematics

Logic

Aeronomy, D Region, Ion Recombination, Ion Density (Concentration), Mathematical Models, Meteorological Parameters, Temperature Dependence

Scientific paper

A simplified model of the ionization-recombination cycle is used to explain the behavior of the relative content of f(+) binding ions and the effective recombination coefficient in the upper D-region. Variations of the effective recombination coefficient in disturbed conditions in the upper D-region can be explained by the strong dependence of the mean constant of dissociative recombination on a number of meteorological parameters.

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