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- W2013462655 abstract "Abstract A three-dimensional theory is presented of the steady wind-driven flow in a homogeneous circumpolar ocean. The bottom topography is a function of longitude and may consist of a series of ridges. The results of Kamenkovich ( Trudy Institut Okeanologiya , 56 , 241–293, 1962) for a transport theory are reproduced here for the three-dimensional velocity field. The model ocean is subdivided into an interior region between surface and bottom Ekman layers. The circumpolar current in the interior to lowest order follows the contours of H / f where H is the depth and f is the Coriolis parameter. The theory shows that in general any deviation from a flat bottom ocean leads to a reduction in transport in the circumpolar current. This decrease in transport can be traced in the theory to an increase in bottom friction as the current turns northward and accelerates over the sloping bottom." @default.
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- W2013462655 date "1975-11-01" @default.
- W2013462655 modified "2023-10-16" @default.
- W2013462655 title "A three-dimensional model of the Southern Ocean with bottom topography" @default.
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- W2013462655 doi "https://doi.org/10.1016/0011-7471(75)90079-0" @default.
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