An explanation of phenomena occurring in the high latitude ionosphere at certain Universal Times

Physics

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Scientific paper

Atmospheric winds which are produced at F-layer heights by neutral-atmosphere pressure gradients could cause various phenomena which are observed in the high-latitude ionosphere at certain Universal Times. These effects include the occurrence of maximum critical frequency and layer height near 06E00 U.T. in the Antarctic region and similar behaviour at 20.00 U.T. at high northern latitudes. Various other phenomena at higher middle latitudes may also be associated with the winds. These include secondary maxima of critical frequency near 03.00 L.M.T., phase differences between the diurnal variations of critical frequency at stations having similar magnetic and geographic latitudes but different magnetic declinations and also the occurrence of sporadic ionization.

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