North-south asymmetry in storm time variation of f0F2

Physics

Scientific paper

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Scientific paper

The study of Dst (f0F2) variations at equatorial and subtropical stations at different longitude zones for 1951-1956, show that at equatorial stations of any in the zones the variation indicates an increase of f0F2 during the main phase. The northern subtropical stations in any of the zones indicate a decrease of f0F2 during the main phase. The southern subtropical stations show decreased f0F2 for Asian and African zones but at American and Pacific zones an increase of f0F2 during main phase of the storm is noted.

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