Nonlinear interaction between astronomical tides and storm surges at wusong tidal station

Wang Jingyong; Chai Fei

doi:10.1007/BF02842749

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Nonlinear interaction between astronomical tides and storm surges at wusong tidal station

OriginalPaper | Updated：2023-05-16

- Nonlinear interaction between astronomical tides and storm surges at wusong tidal station
- Nonlinear interaction between astronomical tides and storm surges at wusong tidal station
- 海洋湖沼学报（英文） 1989年7卷第2期页码：135-142
- Affiliations：
  
  Ocean University of Qingdao
- Author bio：
- Funds：
- DOI：10.1007/BF02842749
  中图分类号：
- 纸质出版：1989
- Accepted：
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Nonlinear interaction between astronomical tides and storm surges at wusong tidal station[J]. 海洋湖沼学报（英文）, 1989,7(2):135-142.

Jingyong, W., Fei, C. Nonlinear interaction between astronomical tides and storm surges at wusong tidal station., Chin. J. Ocean. Limnol. 7, 135–142 (1989). https://doi.org/10.1007/BF02842749
Nonlinear interaction between astronomical tides and storm surges at wusong tidal station[J]. 海洋湖沼学报（英文）, 1989,7(2):135-142. DOI： 10.1007/BF02842749.

Jingyong, W., Fei, C. Nonlinear interaction between astronomical tides and storm surges at wusong tidal station., Chin. J. Ocean. Limnol. 7, 135–142 (1989). https://doi.org/10.1007/BF02842749 DOI：

摘要

Abstract

There are obvious periodic oscillations in the observations of storm surges in the East China Sea. The storm surges are not only controlled by the wind stresses and isolated long wave caused by typhoons but also affected by the interaction between astronomical tides and storm surges. In the present paper we simulate the interaction between tides and storm surges by using a two dimensional numerical model. In our numerical experiments we use the data of the storm surge induced by Typhoon 8114. The calculations tally with the measured data well. The results indicate that the periodic oscillations occurring in the elevations of the surge are mainly caused by the interaction between the tide and the storm surge. The numerical experiments also indicate that the forecasting precision may be notably improved if the nonlinear interaction between tides and storm surges is taken into account.

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references

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Doodson, 1956. Tides and storm surges in a long uniform gulf, Proc. Roy. Soc. A 237, 325.

Liu Fengshu, 1984. An analysis of the fundamental characteristics and variations of storm surges by Typhoon 8114.Oceanologia et Limnologia Sinica 15(6): 568–580. (In Chinese with English abstract).

Liu Fengzhen, 1985. The agricultural climate in Shanghai region, XueLin Publishing House, Shanghai, pp. 81–96.

Prandle, D., and Wolf, J., 1978. The interaction of surge and tide in the North Sea and River Thames,Geophy. J. R. Soc.

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Shen Yujiang and Ye Anle, 1984. Three-dimensional semidiurnal current field in the East China Sea,Transactions of Oceanology and Limnology 1: 1–10 (In Chinese with English abstract).

Wang Jingyong, 1985. A numerical experiment on storm surge simulation in the East China Sea.Journal of Shandong College of Oceanology 13(3): 40–47.

Zhang Yanting and Wang Yiqiao, 1986. A preliminary study on the nonlinear interaction between tide and Typhoon 8114 surge. Journal of Oceanology 8(3).

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