Mountain Wave

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They can also be caused by the surface wind blowing over an '''[[escarpment]]''' or '''[[plateau]]''', or even by upper winds deflected over a thermal updraft or cloud street. They can also be caused by the surface wind blowing over an '''[[escarpment]]''' or '''[[plateau]]''', or even by upper winds deflected over a thermal updraft or cloud street.
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 +== '''Also see''' ==
 +*'''[[Snow Cornice]]'''
 +*'''[[Snow drift]]'''
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== '''Reference''' == == '''Reference''' ==

Revision as of 21:44, 7 June 2011

A wave in the atmosphere caused by a barrier, such as a mountain. Sometimes it is marked by lenticular clouds to the lee side of mountain barriers. May be called a standing wave or a lee wave.

They are periodic changes of atmospheric pressure, temperature and orthometric height in a current of air caused by vertical displacement, for example orographic lift when the wind blows over a mountain or mountain range.

They can also be caused by the surface wind blowing over an escarpment or plateau, or even by upper winds deflected over a thermal updraft or cloud street.


Also see


Reference

  • Wikipedia Lee wave [1]

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