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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Bibliographic Details
Published inJournal of physical oceanography Vol. 38; no. 4; pp. 803 - 816
Main Authors Wirth, A., Barnier, B.
Format Journal Article
LanguageEnglish
Published Boston, MA American Meteorological Society 01.04.2008
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