On the physical mechanism of the ionospheric storms in the F2-layer

Details On the physical mechanism of the ionospheric storms in the F2-layer On the physical mechanism of the ionospheric storms in the F2-layer

Oct 1992

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992adspr..12..269m&link_type=abstract

(The earth's middle and upper atmosphere; Proceedings of the Topical Meeting of the Interdisciplinary Scientific Commission C /M

Computer Science

Sound

F 2 Region, Geomagnetism, Ionospheric Sounding, Ionospheric Storms, Thermosphere, Aeronomy, Atmospheric Models, Nitrogen, Oxygen Atoms

Scientific paper

AE-C satellite data on the neutral thermospheric composition and temperature along with the ground-based ionospheric sounding data at Winnipeg, Boulder, and Havana were used to analyze the physcial mechanism of F2-layer parameter variations during the ionospheric storm on January 25, 1974. Rishbeth's isobaric F2-layer concept concerning a negative F2-layer storms is analyzed. The observed negative as well as positive n(e)mF2 variations during January 25, 1974 storm period may be explained within the scope of the current F2-region theory without taking into account additional processes proposed by Rishbeth.

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