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Secondary circulation : ウィキペディア英語版
Secondary circulation

A secondary circulation is a circulation induced in a rotating system. For example, the primary circulation of Earth's atmosphere is zonal. If however a parcel of air, that moves in a purely zonal direction, is accelerated or decelerated zonally, the Coriolis force will add a meridional component to its velocity. This meridional circulation is then the secondary circulation.
==See also==

* Hough function
* Primitive equations
* Secondary flow


抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
ウィキペディアで「Secondary circulation」の詳細全文を読む



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