Jump to content

Capping inversion

From Wikipedia, the free encyclopedia
This is an old revision of this page, as edited by Allen3 (talk | contribs) at 20:16, 20 April 2005 (Stub-sorting. You can help!.). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

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.

Sources

Stub icon

This article about atmospheric science is a stub. You can help Wikipedia by expanding it.

Retrieved from "https://en.wikipedia.org/w/index.php?title=Capping_inversion&oldid=16104231"