Possible change in the collision frequency in the lower ionosphere with an increase of the height of isobaric surfaces in the stratosphere

Details Possible change in the collision frequency in the lower ionosphere with an increase of the height of isobaric surfaces in the stratosphere Possible change in the collision frequency in the lower ionosphere with an increase of the height of isobaric surfaces in the stratosphere

Feb 1988

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1988ge%26ae..28..134s&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 28, Jan.-Feb. 1988, p. 134, 135. In Russian.

Physics

Atmospheric Attenuation, Collision Parameters, Electron Scattering, Lower Ionosphere, Stratosphere, D Region, E Region, Geopotential, Vertical Distribution

Scientific paper

The paper presents an analysis of midday-absorption values according to the A1 method for Rostov-on-Don for 1970-1982, Ashkhabad for 1973-1977, and Alma-Ata for 1971-1977 as a function of the 10-hPa isobaric surface height for magnetically quiet conditions. It is shown that a negative dependence of absorption on geopotential with a simultaneous increase of electron density in the D and E regions is possible only in the case of a nonlinear increase in the collision frequency.

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