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| Mountain breeze and valley breeze ： ウィキペディア英語版 |
Mountain breeze and valley breeze
A mountain breeze and a valley breeze are two related, localized winds that occur one after the other on a daily cycle. They are not the same as katabatic winds, which are larger and stronger.
Mountain and valley breezes form through a process similar to sea and land breezes. During the day, the sun heats up valley air rapidly. Convection causes it to rise, causing a valley breeze. At night, the process is reversed. Mountain air cools rapidly at night and "falls" downslope, causing a mountain breeze.
== See also ==
* Anabatic wind
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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