Secondary circulation
 | This article does not cite any references or sources. (December 2009) |
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 fluid dynamics-related article is a stub. You can help Oilfield Wiki by expanding it. |