A multi-layer model for nonlinear internal wave propagation in shallow water

被引:18
|
作者
Liu, Philip L. -F. [1 ,2 ]
Wang, Xiaoming [1 ,3 ]
机构
[1] Cornell Univ, Sch Civil & Environm Engn, Ithaca, NY 14853 USA
[2] Natl Cent Univ, Inst Hydrol & Ocean Sci, Tao Yuan 32001, Taiwan
[3] GNS Sci, Wairakei 3377, New Zealand
基金
美国国家科学基金会;
关键词
internal waves; shallow water flows; topographic effects; INTERFACIAL SOLITARY WAVES; CONTINENTAL-SLOPE; CONJUGATE FLOWS; GENERATION; SOLITONS; TIDE; REFRACTION; EQUATIONS; EVOLUTION; BREAKING;
D O I
10.1017/jfm.2012.24
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
In this paper, a multi-layer model is developed for the purpose of studying nonlinear internal wave propagation in shallow water. The methodology employed in constructing the multi-layer model is similar to that used in deriving Boussinesq-type equations for surface gravity waves. It can also be viewed as an extension of the two-layer model developed by Choi & Camassa. The multi-layer model approximates the continuous density stratification by an N-layer fluid system in which a constant density is assumed in each layer. This allows the model to investigate higher-mode internal waves. Furthermore, the model is capable of simulating large-amplitude internal waves up to the breaking point. However, the model is limited by the assumption that the total water depth is shallow in comparison with the wavelength of interest. Furthermore, the vertical vorticity must vanish, while the horizontal vorticity components are weak. Numerical examples for strongly nonlinear waves are compared with laboratory data and other numerical studies in a two-layer fluid system. Good agreement is observed. The generation and propagation of mode-1 and mode-2 internal waves and their interactions with bottom topography are also investigated.
引用
收藏
页码:341 / 365
页数:25
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