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- W2175998019 abstract "Abstract The circulation of a geostrophic, two-layer ocean with Ekman layers at the top, the bottom, and the interface and driven by an anticyclonic wind stress is determined by numerical integration. Inertial effects and lateral friction are ignored. A nominal ratio of upper- to lower-layer thicknesses of 0.15 leads to the formation of a region in the northwestern corner of the basin with lower-layer geostrophic contours that originate from and return to the western boundary layer. This region is referred to as unblocked. Elsewhere in the interior the lower layer is quiescent and the system behaves like a reduced-gravity system. The smallest amount of friction that could be treated by the variable grid procedure that was used leads to a western boundary layer with a width that is 0.1% of the width of the basin. For this limiting case fluid in the lower layer of the unblocked region flows out of the western boundary and turns southward and then southwestward to return to the western boundary layer as a re..." @default.
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- W2175998019 date "1994-04-01" @default.
- W2175998019 modified "2023-09-24" @default.
- W2175998019 title "Strong Deep Recirculations in a Two-Layer Wind-Driven Ocean" @default.
- W2175998019 doi "https://doi.org/10.1175/1520-0485(1994)024<0759:sdriat>2.0.co;2" @default.
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