Antarctic anticyclone: Difference between revisions
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<div class="definition"><div class="short_definition">( | <div class="definition"><div class="short_definition">(''Or'' antarctic high.) The [[glacial]] anticyclone that has been said to overlie the continent of Antarctica; analogous to the [[Greenland anticyclone]].</div><br/> <div class="paragraph">Until the International Geophysical Year there had been insufficient observational evidence to either support or contradict this theory.</div><br/> </div><div class="reference">Court, A. 1951. Compendium of Meteorology. 918–922. </div><br/> | ||
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Revision as of 13:38, 20 February 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.
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.
