For a steady flow independent of , geostrophic balance gives
Hence , and the definition of becomes
Equivalently,
With the Rossby deformation radius , the bounded solution for the stated potential-vorticity step is
Continuity of and at gives
Therefore
and
When , the surface height increases smoothly from to , while is a positive eastward jet with its maximum at the discontinuity and exponential decay on the Rossby-radius scale:

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