Concept information
Preferred term
وارونگی زمینی
Type
-
http://www.irandoc.ac.ir/onto/irandoc-meta/Concept
Broader concept
Definitions
- An air layer with its base at the ground surface and in which temperature increases with height. These often form at night over land under clear skies and are statically stable. See inversion, lapse rate.
Obsolete
- false
In other languages
-
English
URI
http://www.irandoc.acir/onto/irandoc/SWEETT03756
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