Antarctic anticyclone: Difference between revisions
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Revision as of 16:26, 26 January 2012
antarctic anticyclone[edit | edit source]
(
Or antarctic high.) The glacial anticyclone that has been said to overlie the continent of Antarctica; analogous to the Greenland anticyclone.
Or antarctic high.) The glacial anticyclone that has been said to overlie the continent of Antarctica; analogous to the Greenland anticyclone.
Until the International Geophysical Year there had been insufficient observational evidence to either support or contradict this theory.
Court, A. 1951. Compendium of Meteorology. 918–922.
