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 issued from Wikipedia - version of the 10/17/2015. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.