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Term: Radiation inversion Class:  
 vernacular   (0%)
Created 6 June 2017
Last modified 6 June 2017
Contributed by GCW Glossary

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  n2t.net/ark:/99152/h3130

Definition: Temperature inversion produced by nocturnal radiational cooling of the Earth's surface, a snow or ice surface, or the upper part of a cloud layer, etc.  WMOMeteoterm 

 GCW 
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