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An Improvement of Wave Refraction-diffraction Effect in Swan

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並列摘要


SWAN, a wind wave model, has been modified to take into account wave refraction-diffraction effects from the extended mild-slope equation when wind waves pass through a extremely uneven sea bottom in the presence of current. In our modified model, the diffraction correction parameter introducedby Holthuijsen et al. [10] has been adjusted to better predict the combined effect of the higher-order bottom effect, wave-bottom interaction and wave-current interaction. After a preliminary analysis, the influence of the correction parameter is discussed, and a comparison is made between the original and the new phase-decoupled versions of SWAN through some typical examples of wave fields around semiinfinite breakwaters, breakwaters with gap, and detached breakwaters on different bathymetries. The results show that the new phase-decoupled model exhibits improvements in both numerical convergence and Prediction results for the case of a steep varying an extremely uneven sea bottom than the original one.

參考文獻


Arthur, R. S., “Refraction of shallow water waves: The combined effects of currents and underwater topography,” EOS Transaction, American Geo- physical Union, Vol. 31, pp. 549-552 (1952).
Booij, N., Ris, R. C., and Holthuijsen, L. H., ”A third generation wave model for coastal regions: Part I. Model description and validation,” Journal of Geophysical Research, Vol. 104, No. C4, pp. 7649-7666 (1999).
Chamberlain, P. G. and Porter, D., “The modified mild-slope equation,” Journal of Fluid Mechanics, Vol. 291, pp. 393-407 (1995).
Chamberlain, P. G. and Porter, D., “Decomposition methods for wave scattering by topography with application to ripple beds,” Wave Motion, Vol. 22, pp. 201-214 (1995).
Holthuijsen, L. H., Herman, A., and Booij, N., “Phase-decoupled refrac- tion-diffraction for spectral wave models,” Coastal Engineering, Vol. 49, pp. 291-305 (2003).

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