Depth-integrated, non-hydrostatic model for wave breaking and run-up

被引:243
作者
Yamazaki, Yoshiki [1 ]
Kowalik, Zygmunt [2 ]
Cheung, Kwok Fai [1 ]
机构
[1] Univ Hawaii Manoa, Dept Ocean & Resources Engn, Honolulu, HI 96822 USA
[2] Univ Alaska, Inst Marine Sci, Fairbanks, AK 99775 USA
基金
美国海洋和大气管理局;
关键词
non-hydrostatic; dispersive waves; upwind flux approximation; momentum-conserved advection; breaking waves; run-up; SHALLOW-WATER EQUATIONS; CIRCULAR ISLAND; LINEAR-SYSTEMS; SOLITARY WAVES; PROPAGATION; ALGORITHM; FLOWS;
D O I
10.1002/fld.1952
中图分类号
TP39 [计算机的应用];
学科分类号
081203 ; 0835 ;
摘要
This paper describes the formulation, verification, and validation of a depth-integrated, non-hydrostatic model with a semi-implicit, finite difference scheme. The Formulation builds on the nonlinear shallow-water equations and utilizes a non-hydrostatic pressure term to describe weakly dispersive waves. A momentum-conserved advection scheme enables modeling of breaking waves without the aid of analytical solutions for bore approximation or empirical equations for energy dissipation. An upwind scheme extrapolates the free-surface elevation instead of the flow depth to provide the flux in the momentum and continuity equations. This greatly improves the model stability, which is essential for computation of energetic breaking waves and run-up. The computed results show very good agreement with laboratory data for wave propagation, transformation, breaking, and run-up. Since the numerical scheme to the momentum and continuity equations remains explicit, the implicit non-hydrostatic solution is directly applicable to existing nonlinear shallow-water models. Copyright (C) 2008 John Wiley & Sons, Ltd.
引用
收藏
页码:473 / 497
页数:25
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