scholarly journals Forced three-wave interactions of capillary-gravity surface waves

2019 ◽  
Vol 4 (7) ◽  
Author(s):  
Annette Cazaubiel ◽  
Florence Haudin ◽  
Eric Falcon ◽  
Michael Berhanu
2016 ◽  
Vol 93 (4) ◽  
Author(s):  
Florence Haudin ◽  
Annette Cazaubiel ◽  
Luc Deike ◽  
Timothée Jamin ◽  
Eric Falcon ◽  
...  

2013 ◽  
Vol 48 (2) ◽  
pp. 223-231 ◽  
Author(s):  
A. A. Abrashkin ◽  
Yu. P. Bodunova

Nonlinear wave-wave interactions play a central role in the development of wind-generated surface waves. A detailed review of com putational techniques which have been proposed for their evaluation is provided. Numerical experiments are used to determine the manner in which the nonlinear terms control spectral development with fetch, the directional spread of the spectrum and the high-frequency spectral tail. In addition, the nonlinear terms have a shape-stabilizing role, continually smoothing local perturbations in the spectrum and forcing it back to a ‘preferred’ shape.


2017 ◽  
Author(s):  
Adhi Susilo ◽  
Will Perrie ◽  
Bash Toulany

Abstract. Nonlinear wave-wave interactions among ocean surface waves are dominated by quadruplet wave-wave interactions. Computing the nonlinear 4-wave interactions with the Boltzmann integral requires finding the loci of interactions for the quadruplets or solving the delta functions. This is an important part of the computation, but so far it is done by an iteration method that consumes computational time and may not converge after doing several iterations. In this paper, an explicit methodology to find the loci of the quadruplet interactions is presented. This research target is to develop a better method to compute the loci. To illustrate the method, there are 4 cases that will be discussed in this paper. Results show that the new method gives better results than the previous methods that have been applied. Moreover, without iterations the presented method requires less computational loops and some variables, for example the distance between loci, denoted ds, can be determined without any looping. Therefore, the new method leads to better and faster computations than the previous iteration method.


1997 ◽  
Vol 345 ◽  
pp. 79-99 ◽  
Author(s):  
Y. AGNON ◽  
A. SHEREMET

We derive a deterministic directional shoaling model and a stochastic directional shoaling model for a gravity surface wave field, valid for a beach with parallel depth contours accounting for refraction and nonlinear quadratic (three wave) interactions. A new phenomenon of non-resonant spectral evolution arises due to the medium inhomogeneity. The kernels of the kinetic equation depend on the bathymetry through an integral operator. Preliminary tests carried out on laboratory data for a unidirectional case indicate that the stochastic model also works rather well beyond the region where the waves may be regarded as nearly Gaussian. The limit of its applicability is decided by the dispersivity of the medium (relative to the nonlinearity). Good agreement with both laboratory data and the underlying deterministic model is found up to a value of about 1.5 for the spectral peak Ursell number. Beyond that only the deterministic model matches the measurements.


Solar Physics ◽  
1992 ◽  
Vol 141 (2) ◽  
pp. 205-234 ◽  
Author(s):  
Alan J. Miles ◽  
B. Roberts

Author(s):  
Viktor Ivanovich Bukreev ◽  
◽  
Vladimir Vladimirovich Degtyarev ◽  
Alexey Vladimirovich Chebotnikov ◽  
◽  
...  

Solar Physics ◽  
1992 ◽  
Vol 141 (2) ◽  
pp. 235-251 ◽  
Author(s):  
Alan J. Miles ◽  
H. R. Allen ◽  
B. Roberts

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