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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

 
This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Secondary_circulation". A list of authors is available in Wikipedia.
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