Advantages and limitations of the nonlinear Schrödinger equation in describing the evolution of nonlinear water-wave groups
In: Proceedings of the Estonian Academy of Sciences, Band 64, Heft 3, S. 356
ISSN: 1736-7530
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In: Proceedings of the Estonian Academy of Sciences, Band 64, Heft 3, S. 356
ISSN: 1736-7530
In: Natural hazards and earth system sciences: NHESS, Band 13, Heft 8, S. 2101-2107
ISSN: 1684-9981
Abstract. Experiments on extremely steep deterministic waves generated in a large wave tank by focusing of a broad-banded wave train serve as a motivation for the theoretical analysis of the conditions leading to wave breaking. Particular attention is given to the crest of the steepest wave where both the horizontal velocity and the vertical acceleration attain their maxima. Analysis is carried out up to the third order in wave steepness. The apparent, Eulerian and Lagrangian accelerations are computed for wave parameters observed in experiments. It is demonstrated that for a wave group with a wide spectrum, the crest propagation velocity differs significantly from both the phase and the group velocities of the peak wave. Conclusions are drawn regarding the applicability of various criteria for wave breaking.
In: Natural hazards and earth system sciences: NHESS, Band 10, Heft 11, S. 2421-2427
ISSN: 1684-9981
Abstract. In the past decade it became customary to relate the probability of appearance of extremely steep (the so-called freak, or rogue waves) to the value of the Benjamin-Feir Index (BFI) that represents the ratio of wave nonlinearity to the spectral width. This ratio appears naturally in the cubic Schrödinger equation that describes evolution of unidirectional narrow-banded wave field. The notion of this index stems from the Benjamin-Feir linear stability analysis of Stokes wave. The application of BFI to evaluate the evolution of wave fields, with non-vanishing amplitudes of sideband disturbances, is investigated using the Zakharov equation as the theoretical model. The present analysis considers a 3-wave system for which the exact analytical solution of the model equations is available.