Progress of studies on the internal tide generated by the passage of barotropic tide over continental shelf/slope

Jiang Mingshun; Fang Xinhua

doi:10.1007/BF02844743

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Progress of studies on the internal tide generated by the passage of barotropic tide over continental shelf/slope

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- Progress of studies on the internal tide generated by the passage of barotropic tide over continental shelf/slope
- Progress of studies on the internal tide generated by the passage of barotropic tide over continental shelf/slope
- 海洋湖沼学报（英文） 1992年10卷第2期页码：119-134
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- DOI：10.1007/BF02844743
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- 纸质出版：1992
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Progress of studies on the internal tide generated by the passage of barotropic tide over continental shelf/slope[J]. 海洋湖沼学报（英文）, 1992,10(2):119-134.

Mingshun, J., Xinhua, F. Progress of studies on the internal tide generated by the passage of barotropic tide over continental shelf/slope., Chin. J. Ocean. Limnol. 10, 119–134 (1992). https://doi.org/10.1007/BF02844743
Progress of studies on the internal tide generated by the passage of barotropic tide over continental shelf/slope[J]. 海洋湖沼学报（英文）, 1992,10(2):119-134. DOI： 10.1007/BF02844743.

Mingshun, J., Xinhua, F. Progress of studies on the internal tide generated by the passage of barotropic tide over continental shelf/slope., Chin. J. Ocean. Limnol. 10, 119–134 (1992). https://doi.org/10.1007/BF02844743 DOI：

摘要

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 far 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.

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references

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