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Capping inversion
A capping inversion is an elevated inversion layer that caps a convective boundary layer, keeping the convective elements from rising higher into the atmosphere. Capping inversions contribute to the formation of radiation fog and severe thunderstorms.
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10-26-2009 08:16:03
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The contents of this article is licensed from www.wikipedia.org under the GNU Free Documentation License. Click here to see the transparent copy and copyright details


