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R. M. Samelson

of the gap, the circulation south of the gap may be taken to be barotropic and driven by a uniform compensating vertical velocity W * into the surface Ekman layer, so that In the circumpolar-current region, y 1 < y < y 2 , V Ek is assumed constant across the current so that Then, because the condition [Eq. (18) ] also guarantees that Eq. (6) is solvable for Φ on the full domain. Equations (6) , (7) , (18) , (19) , and (20) can be solved numerically by an iterative algorithm. For

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