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Modeling the interaction of an internal solitary wave with a sill 被引量:3

Modeling the interaction of an internal solitary wave with a sill
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摘要 A nonhydrostatic numerical model was developed and numerical experiments performed on the interaction of an internal solitary wave (ISW) with a sill, for a two-layer fluid with a diffusive interface. Based on the blocking parameter (Br), the flow was classified into three cases: (1) when bottom topography has little influence on the propagation and spatial structure of the ISW (Br〈0.5), (2) where the ISW is distorted significantly by the blocking effect of the topography (though no wave breaking occurs, (0.5〈Br〈0.7), and (3) where the ISW is broken as it encounters and passes over the bottom topography (0.7〈Br). The numerical results obtained here are consistent with those obtained in laboratory experiments. The breaking process of the incident ISW when Br=0.7 was completely reproduced. Dissipation rate was linearly related to the blocking parameter when B,〈0.7, and the maximum dissipation rate could reach about 34% as Br raised to about 1.0. After that, instead of breaking, more reflection happened. Similarly, breaking induced mixing was also most effective during Br around 1.0, and can be up to 0.16. A nonhydrostatic numerical model was developed and numerical experiments performed on the interaction of an internal solitary wave (ISW) with a sill, for a two-layer fluid with a diffusive interface. Based on the blocking parameter (Br), the flow was classified into three cases: (1) when bottom topography has little influence on the propagation and spatial structure of the ISW (Br〈0.5), (2) where the ISW is distorted significantly by the blocking effect of the topography (though no wave breaking occurs, (0.5〈Br〈0.7), and (3) where the ISW is broken as it encounters and passes over the bottom topography (0.7〈Br). The numerical results obtained here are consistent with those obtained in laboratory experiments. The breaking process of the incident ISW when Br=0.7 was completely reproduced. Dissipation rate was linearly related to the blocking parameter when B,〈0.7, and the maximum dissipation rate could reach about 34% as Br raised to about 1.0. After that, instead of breaking, more reflection happened. Similarly, breaking induced mixing was also most effective during Br around 1.0, and can be up to 0.16.
出处 《Acta Oceanologica Sinica》 SCIE CAS CSCD 2015年第11期32-37,共6页 海洋学报(英文版)
基金 The National Natural Science Foundation of China under contract Nos 41528601 and 41376029 the Youth Innovation Promotion Association of Chinese Academy of Sciences under contract No.Y4KY07103L the Strategic Priority Research Program of the Chinese Academy of Sciences under contract No.XDA11020101
关键词 internal solitary wave nonhydrostatic model wave breaking blocking degree internal solitary wave, nonhydrostatic model, wave breaking, blocking degree
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