Third Generation Wind Wave Model Frequency Dependence of the White-Capping Dissipation Source Function

Author(s):  
Eustorgio Meza ◽  
Jun Zhang ◽  
Alejandro Olivares ◽  
Jorge Brambila

This paper proposes new frequency dependence for the empirical formulas presently used to determine wave energy dissipation in ocean wave models. Using an energy focusing technique, several unidirectional transient wave trains were generated. Each of the transient wave train contained an isolated plunging or spilling breaker. By comparing the energy spectra of free-wave components before and after breaker it was found that: 1)the energy loss as function of frequency is almost exclusively from wave components at frequencies higher than the spectral peak frequency; 2)although the energy density of the wave components near the peak frequency are the largest, they do not significantly gain or lose energy after breaking; and 3)wave components of frequencies significantly below or near the peak frequency gain a small portion (about 12%) of energy lost by the high-frequency waves. The empirical formulas presently used to determine white-capping dissipation (Komen et al. 1994; Tolman and Chalikov 1996; Booij 1999) do not agree with the above spectral distribution of energy dissipation. Analysis of the dissipation distribution obtained by Meza et al. (2000), suggest that the dependence of the dissipation rate on the frequency should be described by, (ωωp)(1−(ωωp)E(ω), where ω is the wave frequency, ωp is the spectral peak frequency and E(ω) is the energy density spectrum. An energy dissipation source function with such a frequency dependence is being implemented and tested in a third generation wind wave model.

2002 ◽  
Vol 29 (11) ◽  
pp. 1357-1390 ◽  
Author(s):  
W.E. Rogers ◽  
J.M. Kaihatu ◽  
H.A.H. Petit ◽  
N. Booij ◽  
L.H. Holthuijsen

1966 ◽  
Vol 1 (10) ◽  
pp. 2
Author(s):  
Mikio Hino

It is the aim of this paper to give theoretical derivations of the windwave characteristics from a viewpoint of fundamental mechanism of wind-wave generation. A hypothesis is proposed as a basic principle of the air-sea interaction, which asserts the maximum ratio of the energy transfer from wind to wave to the energy dissipation within wind. As the theoretical consequences of the hypothesis combined with the recent theories on wind-wave spectra by Miles and Phillips, wind-wave characteristics such as the fetch graph, the roughness of the sea, the spectral peak frequency, the ratio of pressure contribution to total drag and the energy transfer from wind to wave are derived with remarkable agreements with experimental data.


2002 ◽  
Vol 9 (3/4) ◽  
pp. 367-371 ◽  
Author(s):  
V. G. Polnikov ◽  
Y. A. Volkov ◽  
F. A. Pogarskii

Abstract. A modern version of a numerical wind wave model of the fourth generation is constructed for a case of deep water. The following specific terms of the model source function are used: (a) a new analytic parameterization of the nonlinear evolution term proposed recently in Zakharov and Pushkarev (1999); (b) a traditional input term added by the routine for an atmospheric boundary layer fitting to a wind wave state according to Makin and Kudryavtsev (1999); (c) a dissipative term of the second power in a wind wave spectrum according to Polnikov (1991). The direct fetch testing results showed an adequate description of the main empirical wave evolution effects. Besides, the model gives a correct description of the boundary layer parameters' evolution, depending on a wind wave stage of development. This permits one to give a physical treatment of the dependence mentioned. These performances of the model allow one to use it both for application and for investigation aims in the task of the joint description of wind and wave fields.


1996 ◽  
Vol 26 (11) ◽  
pp. 2497-2518 ◽  
Author(s):  
Hendrik L. Tolman ◽  
Dmitry Chalikov

2003 ◽  
Vol 30 (6) ◽  
pp. 831
Author(s):  
W.E. Rogers ◽  
J.M. Kaihatu ◽  
H.A.H. Petit ◽  
N. Booij ◽  
L.H. Holthuijsen

Oceanology ◽  
2008 ◽  
Vol 48 (1) ◽  
pp. 7-14 ◽  
Author(s):  
V. G. Polnikov ◽  
V. I. Dymov ◽  
T. A. Pasechnik ◽  
I. V. Lavrenov ◽  
Z. K. Abuzyarov ◽  
...  
Keyword(s):  

1988 ◽  
Vol 1 (21) ◽  
pp. 40
Author(s):  
Luigi Cavaleri ◽  
Luciana Bertotti ◽  
Jose E. De Luis ◽  
Piero Lionello

The application of an advanced third generation wave model to the Mediterranean Sea is described. The model is based on the physical description of the wind wave evolution, avoiding any shortcoming in the estimate of the single terms that contribute to the energy budget. The capability of the model to respond to any meteorological situation is illustrated by applying it to a severe storm occurred in January 1987. The results show that the crucial point for the final accuracy lies in the correct evaluation of the wind field.


2007 ◽  
Vol 417 (2) ◽  
pp. 1375-1379 ◽  
Author(s):  
V. G. Polnikov ◽  
V. I. Dymov ◽  
T. A. Pasechnik ◽  
I. V. Lavrenov ◽  
Yu. N. Abuzyarov
Keyword(s):  

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