Viscous Effects on Evolution of Stokes Waves

Abstract
The effects of laminar viscosity on the evolution of a steady Stokes wave train are investigated by employing a boundary‐layer method. It is assumed that the nonlinearity of the second order in the wave slope, 0(ka)2, is in the same order of magnitude as the viscous effect; i.e., 0(ka)2=0(kδ), where δ=v/2ω=the Stokes boundary layer thickness. A nonlinear Schrödinger equation with a dissipation term is derived as the governing equation for the wave envelope. It is shown that the viscosity not only reduces the wave amplitude but also causes a phase shift in the same order of magnitude.

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