Anticyclogenesis

From Wikipedia, the free encyclopedia

Anticyclogenesis is the development or strengthening of anticyclonic circulation in the atmosphere. It is the opposite of anticyclolysis, and has a cyclonic equivalent—cyclogenesis.[1]

[edit] See also

[edit] References

  1. ^ American Meteorological Society Glossary - Anticyclogenesis. Allen Press Inc. (2000-06). Retrieved on 2006-11-03.
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