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Current patterns are presented for flows resulting from non-linearities in the continuity equation, and for those due to density gradients, advection non-linearities, and friction non linearities in the momentum equation. The comparison of computed with observed currents shows qualitiative similarities at most of the stations, and reasonable agreement for those stations where observations were carried out over one month, and where allowance is made for the expected depth variations due to density gradients.   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