Capping inversion
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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
- National Science Digital Library - Capping Inversion (http://www.nsdl.arm.gov/Library/glossary.shtml#Capping_inversion)Template:Climate-stub