Lunar Tide in the F2 Layer of the Ionosphere near the Geomagnetic Equator

Details Lunar Tide in the F2 Layer of the Ionosphere near the Geomagnetic Equator Lunar Tide in the F2 Layer of the Ionosphere near the Geomagnetic Equator

Jan 1961

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1961natur.189..214r&link_type=abstract

Nature, Volume 189, Issue 4760, pp. 214-215 (1961).

Physics

Scientific paper

IT is well known that the maximum in the lunar tide variation of f0F2 occurs at about 10 lunar hours at moderate geomagnetic latitudes and at about 04 lunar hours near the geomagnetic equator1,2. Recent analyses of the lunar variations at Singapore, Ibadan and Bombay have indicated non-agreement in the phases of the variation at stations having the same geomagnetic latitudes.

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