Antarctic anticyclone: Difference between revisions
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|Meaning= | |Meaning=(''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]]. | |Explanation=Until the International Geophysical Year there had been insufficient observational evidence to either support or contradict this theory.<br/> Court, A. 1951. Compendium of Meteorology. 918–922. | ||
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Latest revision as of 21:24, 13 January 2024
(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.
