Taking the vertical component of the curl of the momentum equation gives
The continuity equation gives , and hence
Since initially and ,
Taking the divergence of the momentum equation and using
gives
Differentiate continuity in time and substitute the last two identities to obtain
Let the Rossby deformation radius be
The even, decaying steady solution of
with continuous value and derivative at is
The steady momentum balance is a geostrophic balance:
Thus the flow is parallel to the two edges of the raised strip, in opposite -directions on the two sides; for , it points toward on the left and on the right. Its magnitude is concentrated within a few deformation radii of the edges.

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