The nonlinear stage of the modulational (Benjamin -Feir) instability of unidirectional deep water surface gravity waves is simulated numerically by the firth-order nonlinear envelope equations. The conditions of steep and breaking waves are concerned. The results are compared with the solution of the full potential Euler equations and with the lower order envelope models (the 3-order nonlinear Schrödinger equation and the standard 4-order Dysthe equations). The generalized Dysthe model is shown to exhibit the tendency to re-stabilization of steep waves with respect to long perturbations.
IntroductionThe concept of a wave envelope is very efficient in the situations of slow wave modulations, i.e., narrow spectra. It reduces the problem of description of individual waves to a simpler problem of description of the wave modulation. The nonlinear Schrödinger equation (NLS) for water waves was first derived by Benney & Newell (1967) and then by Zakharov (1968) and Hasimoto & Ono (1972) as the leading-order approximation for weakly nonlinear waves, with dominating four-wave interactions. The corresponding nonlinear term is of the order O(ε 3 ), where the small parameter ε << 1 is related to the small wave steepness, ε = kH/2 (k is the wavenumber and H is the wave height). In this theory the dispersion is assumed to be of the same order of magnitude as the nonlinearity, Δk/k = O(ε) (Δk -is the characteristic width of the wavenumber spectrum). However, realistic sea waves are not narrow-banded, and the NLS equation turns out to be a rather rough model for the wave description; its practical applications are very limited due to this reason. Kristian Dysthe derived an improved theory № 5. 5176.2017/8.9)