Erratum for: Diffusion reduction in an arbitrary scale third generation wind wave model

2003 ◽  
Vol 30 (6) ◽  
pp. 831
Author(s):  
W.E. Rogers ◽  
J.M. Kaihatu ◽  
H.A.H. Petit ◽  
N. Booij ◽  
L.H. Holthuijsen
2002 ◽  
Vol 29 (11) ◽  
pp. 1357-1390 ◽  
Author(s):  
W.E. Rogers ◽  
J.M. Kaihatu ◽  
H.A.H. Petit ◽  
N. Booij ◽  
L.H. Holthuijsen

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.


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

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.


Author(s):  
Fedor Gippius ◽  
Fedor Gippius ◽  
Stanislav Myslenkov ◽  
Stanislav Myslenkov ◽  
Elena Stoliarova ◽  
...  

This study is focused on the alterations and typical features of the wind wave climate of the Black Sea’s coastal waters since 1979 till nowadays. Wind wave parameters were calculated by means of the 3rd-generation numerical spectral wind wave model SWAN, which is widely used on various spatial scales – both coastal waters and open seas. Data on wind speed and direction from the NCEP CFSR reanalysis were used as forcing. The computations were performed on an unstructured computational grid with cell size depending on the distance from the shoreline. Modeling results were applied to evaluate the main characteristics of the wind wave in various coastal areas of the sea.


2011 ◽  
Vol 38 (2-3) ◽  
pp. 456-467 ◽  
Author(s):  
Tai-Wen Hsu ◽  
Jian-Ming Liau ◽  
Jaw-Guei Lin ◽  
Jinhai Zheng ◽  
Shan-Hwei Ou
Keyword(s):  

1994 ◽  
Vol 20 (4) ◽  
pp. 613-624 ◽  
Author(s):  
Stephen Clodman
Keyword(s):  

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