Longitudinal variations of atomic oxygen in the thermosphere, calculated from ionospheric data

Details Longitudinal variations of atomic oxygen in the thermosphere, calculated from ionospheric data Longitudinal variations of atomic oxygen in the thermosphere, calculated from ionospheric data

Feb 1984

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1984ge%26ae..24...69d&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 24, Jan.-Feb. 1984, p. 69-72. In Russian.

Computer Science

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F 2 Region, Ionospheric Sounding, Longitude, Oxygen Atoms, Thermosphere, Incoherent Scattering, Solar Activity Effects, Summer, Winter

Scientific paper

Incoherent-scatter data from the Millstone-Hill and Kharkov stations are used to calculate longitudinal variations of atomic oxygen in the F2-region. It is shown that during high solar activity in the summer months the longitudinal difference of O concentration reaches 40 percent, the concentration being higher in the European sector. In the winter months the O concentration is higher by about 17 percent in the American sector. No longitudinal differences are noted during low solar activity.

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