Antarctic anticyclone: Difference between revisions

From Glossary of Meteorology
imported>Perlwikibot
No edit summary
m (Rewrite with Template:Term and clean up)
 
(2 intermediate revisions by 2 users not shown)
Line 1: Line 1:
 
{{Term
 
|Display title=antarctic anticyclone
{{TermHeader}}
|Definitions={{Definition
{{TermSearch}}
|Num=1
 
|Meaning=(''Or'' antarctic high.) The [[glacial]] anticyclone that has been said to overlie the  continent of Antarctica; analogous to the [[Greenland anticyclone]].
<div class="termentry">
|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&ndash;922.  
  <div class="term">
}}
== antarctic anticyclone ==
}}
  </div>
 
<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&ndash;922. </div><br/>
</div>
 
{{TermIndex}}
{{TermFooter}}
 
[[Category:Terms_A]]

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.


An atmospheric anticyclonic circulation, a closed circulation. The wind in an anticyclone is in the clockwise direction in the Northern Hemisphere and counterclockwise in the Southern Hemisphere.

Retrieved from "https://glossarystaging.ametsoc.net/w/index.php?title=Antarctic_anticyclone&oldid=28078"
Powered by MediaWiki
Powered by WikiTeq
Powered by Semantic MediaWiki
Copyright 2025 American Meteorological Society (AMS). For permission to reuse any portion of this work, please contact permissions@ametsoc.org. Any use of material in this work that is determined to be “fair use” under Section 107 of the U.S. Copyright Act (17 U.S. Code § 107) or that satisfies the conditions specified in Section 108 of the U.S.Copyright Act (17 USC § 108) does not require AMS’s permission. Republication, systematic reproduction, posting in electronic form, such as on a website or in a searchable database, or other uses of this material, except as exempted by the above statement, require written permission or a license from AMS. Additional details are provided in the AMS Copyright Policy statement.