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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）』
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