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Paola Cessi and Christopher L. Wolfe

,1. Given the sense of propagation of the similarity variables, b w has to adapt to b e at ŷ = 1, while b e has to match b w at ŷ = 0. Thus the buoyancies on the east and west boundaries, although they have a qualitatively different scaling [cf. (23) with (40) ], are interdependent. The linear solution in the interior, illustrated in Fig. 11 by three plan views at representative depths, shows the general southwest to northeast slant of the isopycnals, with a reversal of the north

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