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- W1987382010 abstract "A two-dimensional linear steady-state model of the ocean circulation of the world which includes the effects of the rotation of the earth, lateral and bottom friction, and a steady-state wind stress is considered. The two-dimensional equations of motion for mass transports are obtained by integration of the equations of motion with respect of depth and linearization. A stream function ψ for the mass transports is then introduced and a fourth-order partial differential equation for ψ is obtained. The boundary conditions ψ = const.and ∂ψ/∂n = 0 are implemented at the land-sea boundaries of the model, which correspond closely to actual boundaries except that small isolated islands are omitted and larger islands such as Australia are joined to the mainland. The numerical solution of the partial differential equation is achieved by approximating it by finite difference equations on the Mercator projection of the earth, and solving these equations by a combination of iterative and direct techniques. The finite difference equations involve values of ψ at certain land grid points near the boundaries, and at each stage of the iteration, values of ψ are assigned to these points in such a way that the boundary conditions are satisfied for the current approximation to ψ The results so far produced qualitatively agree very well with the known patterns of ocean circulation. Western boundary currents such as the Gulf Stream are prominent and smaller circulations such as the eddies off the coast of Antarctica are also present." @default.
- W1987382010 created "2016-06-24" @default.
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- W1987382010 date "1969-12-01" @default.
- W1987382010 modified "2023-09-26" @default.
- W1987382010 title "Numerical Model for Wind-Driven Circulation of the Oceans of the World" @default.
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- W1987382010 doi "https://doi.org/10.1063/1.1692434" @default.
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