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    A Two-Layer Wind-Driven Ocean Model in a Multiply Connected Domain with Bottom Topography 

    Source: Journal of Physical Oceanography:;1997:;Volume( 027 ):;issue: 011:;page 2395
    Author(s): Krupitsky, Alexander; Cane, Mark A.
    Publisher: American Meteorological Society
    Abstract: The behavior of the solution to a two-layer wind-driven model in a multiply connected domain with bottom topography imitating the Southern Ocean is described. The abyssal layer of the model is forced by interfacial friction, ...
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    A Linear Equivalent Barotropic Model of the Antarctic Circumpolar Current with Realistic Coastlines and Bottom Topography 

    Source: Journal of Physical Oceanography:;1996:;Volume( 026 ):;issue: 009:;page 1803
    Author(s): Krupitsky, Alexander; Kamenkovich, Vladimir M.; Naik, Naomi; Cane, Mark A.
    Publisher: American Meteorological Society
    Abstract: A linear equivalent barotropic (EB) model is applied to study the effects of the bottom topography H and baroclinicity on the total transport and the position of the Antarctic Circumpolar Current (ACC). The model is based ...
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    On the Utility and Disutility of JEBAR 

    Source: Journal of Physical Oceanography:;1998:;Volume( 028 ):;issue: 003:;page 519
    Author(s): Cane, Mark A.; Kamenkovich, Vladimir M.; Krupitsky, Alexander
    Publisher: American Meteorological Society
    Abstract: The usefulness of the concept of JEBAR, the joint effect of baroclinicity and relief, in large-scale ocean dynamics is critically analyzed. The authors address two questions. Does the JEBAR term properly characterize the ...
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