Abstract
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 (B r), the flow was classified into three cases: (1) when bottom topography has little influence on the propagation and spatial structure of the ISW (B r<0.5), (2) where the ISW is distorted significantly by the blocking effect of the topography (though no wave breaking occurs, (0.5<B r<0.7), and (3) where the ISW is broken as it encounters and passes over the bottom topography (0.7<B r). The numerical results obtained here are consistent with those obtained in laboratory experiments. The breaking process of the incident ISW when B r≈0.7 was completely reproduced. Dissipation rate was linearly related to the blocking parameter when B r<0.7, and the maximum dissipation rate could reach about 34% as B r raised to about 1.0. After that, instead of breaking, more reflection happened. Similarly, breaking induced mixing was also most effective during B r around 1.0, and can be up to 0.16.
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Foundation item: 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.
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Li, Q., Xu, Z., Yin, B. et al. Modeling the interaction of an internal solitary wave with a sill. Acta Oceanol. Sin. 34, 32–37 (2015). https://doi.org/10.1007/s13131-015-0745-1
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DOI: https://doi.org/10.1007/s13131-015-0745-1