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- W2156990531 startingPage "2689" @default.
- W2156990531 abstract "The impact of a meridional gradient in sea surface temperature (warm toward the equator, cold toward the pole) on the circulation around an island is investigated. The upper-ocean eastward geostrophic flow that balances such a meridional gradient is blocked where the isotherms intersect boundaries. In the case in which the boundaries represent either the eastern or western side of a planetary-scale island, circulation integrals around the island show that some of this eastward transport will flow around both the equatorward and poleward tips of the island. There is also a net downwelling along the western side of the island and a net upwelling along the eastern side of the island. An analytic model of the eastern and western boundary currents is used together with a circulation integral to estimate the fraction of the eastward transport that flows around the equatorward and poleward tips of the island and the net upwelling/downwelling on either side of the island. Calculations with a primitive equation numerical model are in close agreement with the theory. A simple closed-form analytic solution for the transport around the island tips is derived in the limit of strong buoyancy forcing. It is found that, over a wide range of parameter space, a significant fraction of the eastward transport in the upper ocean circulates around the tips of the island from the western basin into the eastern basin." @default.
- W2156990531 created "2016-06-24" @default.
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- W2156990531 date "2003-12-01" @default.
- W2156990531 modified "2023-09-28" @default.
- W2156990531 title "Islands in Zonal Flow*" @default.
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- W2156990531 doi "https://doi.org/10.1175/1520-0485(2003)033<2689:iizf>2.0.co;2" @default.
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