A numerical study of the tide-surge interaction in the East China Sea and the South China Sea

Pan Hai; Liu Feng-shu

doi:10.1007/BF02845468

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A numerical study of the tide-surge interaction in the East China Sea and the South China Sea

OriginalPaper | Updated：2023-05-16

- A numerical study of the tide-surge interaction in the East China Sea and the South China Sea
- A numerical study of the tide-surge interaction in the East China Sea and the South China Sea
- 海洋湖沼学报（英文） 1994年12卷第1期页码：13-21
- Affiliations：
  
  Institute of Oceanology
- Author bio：
- Funds：
  
  Contribution No. 2234 from the Institute of Oceanology, Chinese Academy of Sciences.
- DOI：10.1007/BF02845468
  中图分类号：
- 纸质出版：1994
- Accepted：
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A numerical study of the tide-surge interaction in the East China Sea and the South China Sea[J]. 海洋湖沼学报（英文）, 1994,12(1):13-21.

Hai, P., Feng-shu, L. A numerical study of the tide-surge interaction in the East China Sea and the South China Sea., Chin. J. Ocean. Limnol. 12, 13–21 (1994). https://doi.org/10.1007/BF02845468
A numerical study of the tide-surge interaction in the East China Sea and the South China Sea[J]. 海洋湖沼学报（英文）, 1994,12(1):13-21. DOI： 10.1007/BF02845468.

Hai, P., Feng-shu, L. A numerical study of the tide-surge interaction in the East China Sea and the South China Sea., Chin. J. Ocean. Limnol. 12, 13–21 (1994). https://doi.org/10.1007/BF02845468 DOI：

摘要

Abstract

Nearshore sea levels in the East China Sea (ECS) and the South China Sea (SCS) during tropical cyclones—Typhoon 8007 (Joe

1980) and Typhoon 7209 (Betty

1972) were simulated. The tide-surge interactions in the two regions are remarkable and locally produced. The corresponding nonlinear effects were derived from the different nonlienar terms. The contribution of the quadratic friction term is the most important

the shallow term comes second the convective term is the least; the phases of the interactions generated by the various nonlinear terms are asynchronous. Both the quadratic friction and the convective term can stimulate and aggravate the surge structure with more peaks. The bottom friction features have crucial influences on tides and surges

and the interaction is sensitive to the changes of tide and surge.

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references

Banks, J. E., 1974. A mathematical model of a river-shallow sea system used to investigate tide, surge and their interaction in the Thames-Southern North Sea region.Phil. Trans. R. Soc. A 275: 567–609.

Fang Guohong, 1980. The nonlinear effects of the tidal friction (I).Oceanol. et Limnol. Sinica 11(2): 98–107. (in Chinese with English abstract)

Fang Guobong, 1981. The nonlinear effects of the tidal friction (II).Oceanol. et Limnol. Sinica 12(3): 195–209 (in Chinese with English abstract)

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