New 2-D horizontal free-surface-flow models with applications for water waves

被引:0
|
作者
Yang, Zhengtong [1 ]
Liu, Philip L. -F. [1 ,2 ,3 ,4 ]
机构
[1] Natl Univ Singapore, Dept Civil & Environm Engn, Singapore 117576, Singapore
[2] Cornell Univ, Sch Civil & Environm Engn, Ithaca, NY 14850 USA
[3] Natl Cent Univ, Inst Hydrol & Ocean Sci, Taoyuan 320, Taiwan
[4] Natl Cheng Kung Univ, Dept Hydraul & Ocean Engn, Tainan 70101, Taiwan
基金
新加坡国家研究基金会;
关键词
coastal engineering; surface gravity waves; NONLINEAR BOUSSINESQ MODEL; DEEP-WATER; EVOLUTION; SHALLOW; EQUATIONS; ACCURACY; BREAKING; PART;
D O I
10.1017/jfm.2024.604
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
The depth-integrated horizontal momentum equations and continuity equation are employed to develop a new model. The vertical velocity and pressure can be expressed exactly in terms of horizontal velocities and free-surface elevation, which are the only unknowns in the model. Dividing the water column into elements and approximating horizontal velocities using linear shape function in each element, a set of model equations for horizontal velocities at element nodes is derived by adopting the weighted residual method. These model equations can be applied for transient or steady free-surface flows by prescribing appropriate lateral boundary conditions and initial conditions. Here, only the wave-current-bathymetry interaction problems are investigated. Theoretical analyses are conducted to examine various linear wave properties of the new models, which outperform the Green-Naghdi-type models for the range of water depth to wavelength ratios and the Boussinesq-type models as they are capable of simulating vertically sheared currents. One-dimensional horizontal numerical models, using a finite-difference method, are applied to a wide range of wave-current-bathymetry problems. Numerical validations are performed for nonlinear Stokes wave and bichromatic wave group propagation in deep water, sideband instability, regular wave transformation over a submerged shoal and focusing wave group interacting with linearly sheared currents in deep water. Very good agreements are observed between numerical results and laboratory data. Lastly, numerical experiments of wave shoaling from deep to shallow water are conducted to further demonstrate the capability of the new model.
引用
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页数:54
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