An evaluation of wave propagation simulations over a barred beach with a Boussinesq-type model

被引:2
|
作者
Mil-Homens, Joao [2 ]
Fortes, Conceicao J. E. M. [1 ]
Pires-Silva, Antonio A. [3 ]
机构
[1] LNEC DHA NPE, Lab Nacl Engn Civil, P-1700066 Lisbon, Portugal
[2] WW Consultores Hidraul & Obras Maritimas SA, P-2685223 Portela, Portugal
[3] Univ Tecn Lisboa, Inst Super Tecn, P-1049001 Lisbon, Portugal
关键词
Numerical modelling; Nonlinear wave propagation; Barred beach propagation; Boussinesq model; FUNWAVE model; Validation; Bispectrum; SURFACE-WAVES; GRAVITY-WAVES; BREAKING; TRANSFORMATION; EQUATIONS; SPECTRA; WATER; GENERATION; EVOLUTION; DEPTH;
D O I
10.1016/j.oceaneng.2009.11.001
中图分类号
U6 [水路运输]; P75 [海洋工程];
学科分类号
0814 ; 081505 ; 0824 ; 082401 ;
摘要
The FUNWAVE model is used for simulating simulation of monochromatic and irregular wave propagation in a channel with a bar-trough profile. FUNWAVE is based upon the extended Boussinesq equations. The study aims to analyze the model's performance when simulating shoaling, wave breaking and nonlinear interactions that are present in nearshore wave propagation. For that, high-order time domain statistics (root mean-square wave height, skewness, asymmetry and the kurtosis) of the model simulations and of the observations were compared along the whole channel. Also, a frequency domain analysis including standard spectral analysis and the bispectrum was carried out in selected points of the flume. The evaluation included the role of the wave breaking internal model parameters. The main conclusion is that, in general, the one-dimensional version of FUNWAVE simulates quite well the nonlinear transformation of a wave over a bottom with a bar-tough profile, for both regular and irregular wave conditions. The model reproduces the transformation of the wave shape, specially the increasing sharper wave crests and flatter troughs and also the lack of vertical symmetry with crests pitching forward, as it propagates along the domain. However, some differences persist after wave breaking, mainly due to the nature of the wave-breaking module. In this module, the energy dissipation is induced by the increase of viscosity, a rather simple mechanism, without the modification of the wave shape. Also, the energy dissipation develops in a smooth way which is appropriated for spilling breaking waves, but not for plunging breaking waves where the dissipation starts more abruptly. (C) 2009 Elsevier Ltd. All rights reserved.
引用
收藏
页码:236 / 251
页数:16
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