F. Crisciani et R. Purini, BOUNDARY-CONDITION OF THE SVERDRUP SOLUTION FROM FLOW ENERGETICS, Journal of physical oceanography, 27(2), 1997, pp. 357-361
The energetics of the wind-driven, quasigeostrophic circulation is use
d to rule out the vanishing of the Sverdrup solution in the western bo
undary of the ocean, apart from the total solution near the eastern bo
undary. The result holds for every wind stress curl.