Mean Circulation and Structures of Tilted Ocean Deep Convection
Convection in a homogeneous ocean is investigated by numerically integrating the three-dimensional Boussinesq equations in a tilted, rotating frame ( f–F plane) subject to a negative buoyancy flux (cooling) at the surface. The study focuses on determining the influence of the angle (tilt) between th...
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Published in | Journal of physical oceanography Vol. 38; no. 4; pp. 803 - 816 |
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Main Authors | , |
Format | Journal Article |
Language | English |
Published |
Boston, MA
American Meteorological Society
01.04.2008
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Subjects | |
Online Access | Get full text |
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