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An example of the modification of ocean currents by bottom topography

A mathematical model is presented for steady currents in ocean basins which become deeper towards the poles. Relatively large currents occur in an interior layer at the line where ? ( ?y )( f / h ) changes sign, ( f is the Coriolis parameter, h the depth and y a northward co-ordinate). The flow in the interior layer is described quantitatively and the work thus complements recent studies by Kamenkovich & Mitrofanov (1971) and Brink et al. (1973). DOI: 10.1111/j.2153-3490.1976.tb00674.x