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thermocyclogenesis |
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thermocyclogenesis [¦thər·mō‚sī·klə′jen·ə·səs]
(meteorology) A theory of cyclogenesis by G. Stüve, in which the disturbance is initiated in the stratosphere and is reflected in the development of a disturbance in the lower troposphere. Want to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit the webmaster's page for free fun content. |
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