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Concept information

Preferred term

صعود کوهستانی هوا  

Type

  • http://www.irandoc.ac.ir/onto/irandoc-meta/Concept

Definitions

  • Ascending air flow caused by mountains. Mechanisms that produce the lifting fall into two broad categories: 1) the upward deflection of horizontal larger-scale flow by the orography acting as an obstacle or barrier; or 2) the daytime heating of mountain surfaces to produce anabatic flow along the slopes and updrafts in the vicinity of the peaks.

Obsolete

  • false

In other languages

URI

http://www.irandoc.acir/onto/irandoc/SWEETT11902

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