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PROGRESS OF STUDIES ON THE INTERNAL TIDE GENERATED BY THE PASSAGE OF BAROTROPIC TIDE OVER CONTINENTAL SHELF/SLOPE
引用本文:汪明顺,方欣华. PROGRESS OF STUDIES ON THE INTERNAL TIDE GENERATED BY THE PASSAGE OF BAROTROPIC TIDE OVER CONTINENTAL SHELF/SLOPE[J]. 中国海洋湖沼学报, 1992, 10(2): 119-134. DOI: 10.1007/BF02844743
作者姓名:汪明顺  方欣华
作者单位:Ocean University of Qingdao,Qingdao,266003,Ocean University of Qingdao,Qingdao,266003
摘    要:Various aspects of studies on internal tides are reviewed .Both beam-like structure and modal structure of internal tides may exist in the ocean . Bottom intensifications are caused by many factors .e.g. upstream blocking , which is the result of nonlinear interaction among waves . The energy may decay very fast so that internal tides are mostly locally generated .Internal tides may have considerable residual currents.In a 3-D frame, numerical study revealed that internal waves may interfere with each other to cause strong motions fer from the generation sources.The mechanism that determines how the lee waves break to form various nonlinear waves such as solitary waves, hydraulic jumps and internal surges or bores remains unclear. Analytic study is difficult , so numerical method may be effective . A radiation condition on the open boundary must be employed. A complete 3-D model may gain interesting result.Study on internal tides in China is limited to field observations and data analysis .

收稿时间:2001-05-24

Progress of studies on the internal tide generated by the passage of barotropic tide over continental shelf/slope
Jiang Mingshun,Fang Xinhua. Progress of studies on the internal tide generated by the passage of barotropic tide over continental shelf/slope[J]. Chinese Journal of Oceanology and Limnology, 1992, 10(2): 119-134. DOI: 10.1007/BF02844743
Authors:Jiang Mingshun  Fang Xinhua
Affiliation:(1) Ocean University of Qingdao, 266003 Qingdao
Abstract:Various aspects of studies on internal tides are reviewed .Both beam-like structure and modal structure of internal tides may exist in the ocean . Bottom intensifications are caused by many factors .e.g. upstream blocking , which is the result of nonlinear interaction among waves . The energy may decay very fast so that internal tides are mostly locally generated .Internal tides may have considerable residual currents.In a 3-D frame, numerical study revealed that internal waves may interfere with each other to cause strong motions fer from the generation sources.The mechanism that determines how the lee waves break to form various nonlinear waves such as solitary waves, hydraulic jumps and internal surges or bores remains unclear. Analytic study is difficult , so numerical method may be effective . A radiation condition on the open boundary must be employed. A complete 3-D model may gain interesting result.Study on internal tides in China is limited to field observations and data analysis .
Keywords:internal tide    internal wave    baroclinic motion . continental shelf/slope .
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