Concept information
Preferred term
تندرتوفانِ لایههای بالایی جو
Type
-
http://www.irandoc.ac.ir/onto/irandoc-meta/Concept
Broader concept
Definitions
- Generally, a thunderstorm based at a comparatively high altitude in the atmosphere, roughly 2400 m or higher. These storms form most strikingly over arid regions, and frequently their precipitation is evaporated before reaching the earth's surface.
Obsolete
- false
In other languages
-
English
URI
http://www.irandoc.acir/onto/irandoc/SWEETT08038
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