Abstract
The problem of the bimodal behavior of the Kuroshio path, south of Japan is discussed by use of the Korteweg-de Vries equation with forcing and dissipation. We show that a localized, large meander of the ocean current is produced by coastal step-like geometry when the upstream current is faster than the long Rossby wave speed. In particular, even if the forcing due to coastal geometry is weak, our dynamical system has a chance to jump from a small meander state to a large meander state because of multiple equilibria. This transition is accomplished by capturing a large, propagating disturbance. These model results are consistent, at least qualitatively, with observations of the Kuroshio.