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Nonlinear Processes in Geophysics An interactive open-access journal of the European Geosciences Union

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Nonlin. Processes Geophys., 16, 131-139, 2009
http://www.nonlin-processes-geophys.net/16/131/2009/
doi:10.5194/npg-16-131-2009
© Author(s) 2009. This work is distributed
under the Creative Commons Attribution 3.0 License.
 
24 Feb 2009
The effect of third-order nonlinearity on statistical properties of random directional waves in finite depth
A. Toffoli1, M. Benoit2, M. Onorato3, and E. M. Bitner-Gregersen1 1Det Norske Veritas, Veritasveien 1, Høvik, 1322, Norway
2Saint-Venant Laboratory for Hydraulics, Université Paris Est (Joint Research Unit EDF R & D, CETMEF, Ecole des Ponts ParisTech), 6 quai Watier, BP 49, 78401 Chatou, France
3Dip. di Fisica Generale, Università di Torino, Via P. Giuria 1, 10125 Torino, Italy
Abstract. It is well established that third-order nonlinearity produces a strong deviation from Gaussian statistics in water of infinite depth, provided the wave field is long crested, narrow banded and sufficiently steep. A reduction of third-order effects is however expected when the wave energy is distributed on a wide range of directions. In water of arbitrary depth, on the other hand, third-order effects tend to be suppressed by finite depth effects if waves are long crested. Numerical simulations of the truncated potential Euler equations are here used to address the combined effect of directionality and finite depth on the statistical properties of surface gravity waves; only relative water depth kh greater than 0.8 are here considered. Results show that random directional wave fields in intermediate water depths, kh=O(1), weakly deviate from Gaussian statistics independently of the degree of directional spreading of the wave energy.

Citation: Toffoli, A., Benoit, M., Onorato, M., and Bitner-Gregersen, E. M.: The effect of third-order nonlinearity on statistical properties of random directional waves in finite depth, Nonlin. Processes Geophys., 16, 131-139, doi:10.5194/npg-16-131-2009, 2009.
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