Abstract:We investigate the eigenvalue problem governing the propagation of long nonlinear surface waves when there is a currentū(y) beneath the surface, y being the vertical coordinate. The amplitude of such waves evolves according to the KdV equation and it was proved by Burns [1] that their speed of propagation c is such that there is no critical layer (i.e., c lies outside the range ofū(y)). If, however, the critical layer is nonlinear, the result of Burns does not necessarily apply because the phase change of line… Show more
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