Numerical study on effect of tidal phase on storm surge in the South Yellow Sea

Weisheng ZHANG; Ling TENG; Jinshan ZHANG; Mengjie XIONG; Chengtuan YIN

doi:10.1007/s00343-019-8277-8

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Numerical study on effect of tidal phase on storm surge in the South Yellow Sea

Updated：2023-05-20

- Numerical study on effect of tidal phase on storm surge in the South Yellow Sea
- Numerical study on effect of tidal phase on storm surge in the South Yellow Sea
- 海洋湖沼学报（英文） 2019年37卷第6期页码：2037-2055
- Affiliations：
  
  Nanjing Hydraulic Research Institute, State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Nanjing 210029, China
- Author bio：
  
  ZHANG Jinshan, E-mail:jszhang@nhri.cn
- Funds：
  
  the National Key Research and Development Program of China(2016YFC1402000)
- DOI：10.1007/s00343-019-8277-8
  中图分类号：
- 收稿：2019-01-24，
  
  录用：2019-4-15，
  
  网络首发：2019-08-23，
  
  纸质出版：2019-11
- Accepted：
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Numerical study on effect of tidal phase on storm surge in the South Yellow Sea[J]. 海洋湖沼学报（英文）, 2019,37(6):2037-2055.

Weisheng ZHANG, Ling TENG, Jinshan ZHANG, et al. Numerical study on effect of tidal phase on storm surge in the South Yellow Sea[J]. Journal of Oceanology and Limnology, 2019, 37(6): 2037-2055.
Numerical study on effect of tidal phase on storm surge in the South Yellow Sea[J]. 海洋湖沼学报（英文）, 2019,37(6):2037-2055. DOI： 10.1007/s00343-019-8277-8.

Weisheng ZHANG, Ling TENG, Jinshan ZHANG, et al. Numerical study on effect of tidal phase on storm surge in the South Yellow Sea[J]. Journal of Oceanology and Limnology, 2019, 37(6): 2037-2055. DOI： 10.1007/s00343-019-8277-8.

摘要

Abstract

Because of the special topography and large tidal range in the South Yellow Sea

the dynamic process of tide and storm surge is very complicated. The shallow water circulation model Advanced Circulation (ADCIRC) was used to simulate the storm surge process during typhoon Winnie

Prapiroon

and Damrey

which represents three types of tracks attacking the South Yellow Sea

which are

moving northward after landing

no landing but active in offshore areas

and landing straightly to the coastline. Numerical experiments were carried out to investigate the effects of tidal phase on the tide-surge interaction as well as storm surge. The results show that the peak surge caused by Winnie and Prapiroon occurs 2-6 h before the high tide and its occurring time relative to high tide has little change with tidal phase variations. On the contrary

under the action of Damrey

the occurring time of the peak surge relative to high tide varies with tidal phase. The variation of tide-surge interaction is about 0.06-0.37 m

and the amplitude variations of interaction are smooth when tidal phase changes for Typhoon Winnie and Prapiroon. While the interaction is about 0.07-0.69 m

and great differences exists among the stations for Typhoon Damrey. It can be concluded that the tide-surge interaction of the former is dominated by the tidal phase modulation

and the time of surge peak is insensitive to the tidal phase variation. While the interaction of the latter is dominated by storm surge modulation due to the water depth varying with tide

the time of surge peak is significantly affected by tidal phase. Therefore

influence of tidal phase on storm surge is related to typhoon tracks which may provide very useful information at the design stage of coastal protection systems.

关键词

Keywords

references

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