The classic solution of Fofonoff to the problem of free inertial flow in a closed basin is extended to the case where the potential vorticity,
q, is linearly proportional to the streamfunction, with a
negative definite constant,
. Such a relation arises naturally in the presence of an eastward flow, instead of Fofonoff’s westward zonal flow on the β plane. The resulting solutions can be wavelike if
=
exceeds the critical value of 1 where
U is the magnitude of the eastward flow and
L is the characteristic meridional scale of the motion. Solutions are presented with various boundary conditions on the basin boundaries, and conditions for which the solutions suffer a resonance are also obtained. It is suggested that oceanic circulations with eastward flows naturally excite these Fofonoff
negative modes. The possibility of resonance and instability adds additional physical complexity to the modes.
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