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The fractional width ŷ of the
upstream current lying above the continental slope that is deflected
offshore (cf. Fig. 2) as a function of nondimensional slope
s = ½ + 1/F2 when the potential
vorticity (P) vanishes. M1: F2 = 2, ɛ =
½; M2: F2 = 4, ɛ =
½; M3: F2 = 4, ɛ =
; M4: F2 = 4, ɛ =
.
