At small Rossby number, . For steady flow with , the forced potential-vorticity equation becomes
so
Define a transport streamfunction by and . Choosing the eastern wall as gives the topographic Sverdrup balance solution
and therefore
In each half-basin, the transport streamlines are the level curves . They move westward and toward . This interior solution treats the two sides of the degenerate line separately and requires boundary layers to enforce solid-wall conditions.

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