Anticyclogenesis: Difference between revisions

Revision as of 16:31, 7 November 2023

Any strengthening or development of anticyclonic circulation in the atmosphere; the opposite of anticyclolysis.
This applies to the development of anticyclonic circulation (or the initial appearance of a high) where previously it was nonexistent, as well as to intensification of existing anticyclonic flow. The most common application of this term is to the formation of a new anticyclone. Care should be taken, however, to distinguish the increase in anticyclonic circulation from the increase in atmospheric pressure (filling), although they usually occur simultaneously.
Compare cyclogenesis.

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+{{Term
+|Display title=anticyclogenesis
-{{TermHeader}}
+|Definitions={{Definition
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+|Num=1
+|Meaning=
-<div class="termentry">
+Any strengthening or [[development]] of [[anticyclonic circulation]] in the [[atmosphere]];  the opposite of [[anticyclolysis]].<br/> This applies to the development of anticyclonic circulation (or the initial appearance of a [[high]])  where previously it was nonexistent, as well as to [[intensification]] of existing [[anticyclonic]] flow.  The most common application of this term is to the formation of a new [[anticyclone]]. Care should  be taken, however, to distinguish the increase in anticyclonic circulation from the increase in  [[atmospheric pressure]] ([[filling]]), although they usually occur simultaneously. <br/>''Compare'' [[cyclogenesis]].
-  <div class="term">
+}}
-== anticyclogenesis ==
+}}
-  </div>
-<div class="definition"><div class="short_definition">Any strengthening or [[development]] of [[anticyclonic circulation]] in the [[atmosphere]];  the opposite of [[anticyclolysis]].</div><br/> <div class="paragraph">This applies to the development of anticyclonic circulation (or the initial appearance of a [[high]])  where previously it was nonexistent, as well as to [[intensification]] of existing [[anticyclonic]] flow.  The most common application of this term is to the formation of a new [[anticyclone]]. Care should  be taken, however, to distinguish the increase in anticyclonic circulation from the increase in  [[atmospheric pressure]] ([[filling]]), although they usually occur simultaneously. <br/>''Compare'' [[cyclogenesis]].</div><br/></div>
-</div>
-{{TermIndex}}
-{{TermFooter}}
-[[Category:Terms_A]]