Wave-current interaction during Typhoon Nuri (2008) and Hagupit (2008): an application of the coupled ocean-wave modeling system in the northern South China Sea

张晨; 侯一筠; 李健

doi:10.1007/s00343-018-6088-y

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Wave-current interaction during Typhoon Nuri (2008) and Hagupit (2008): an application of the coupled ocean-wave modeling system in the northern South China Sea

Physics | Updated：2023-05-19

- Wave-current interaction during Typhoon Nuri (2008) and Hagupit (2008): an application of the coupled ocean-wave modeling system in the northern South China Sea
- Wave-current interaction during Typhoon Nuri (2008) and Hagupit (2008): an application of the coupled ocean-wave modeling system in the northern South China Sea
- 海洋湖沼学报（英文） 2018年36卷第3期页码：663-675
- Affiliations：
  
  1.Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
  2.Key Laboratory of Ocean Circulation and Waves, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
  3.University of Chinese Academy of Sciences, Beijing 100049, China
  4.North China Sea Branch of State Oceanic Administration, Qingdao 266071, China
  5.Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China
- Author bio：
  
  HOU Yijun, yjhou@qdio.ac.cn
- Funds：
  
  the National Key Research and Development Program of China(2016YFC1402000);the National Natural Science Foundation of China(41376027);the National Natural Science Foundation of China(U1133001);the National Natural Science Foundation of China(41606024);the National Program on Global Change and Air-Sea Interaction(GASI-IPOVAI-01-06);the NSFC-Shandong Joint Fund for Marine Science Research Centers(U1406401);the National Natural Science Foundation of China(41421005);the High Performance Computing Environment Qingdao Branch of Chinese Academy of Science(CAS)
- DOI：10.1007/s00343-018-6088-y
  中图分类号：
- 收稿：2016-03-21，
  
  录用：2016-4-12，
  
  网络首发：2017-03-27，
  
  纸质出版：2018-05
- Accepted：
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张晨, 侯一筠, 李健. Wave-current interaction during Typhoon Nuri (2008) and Hagupit (2008): an application of the coupled ocean-wave modeling system in the northern South China Sea[J]. 海洋湖沼学报（英文）, 2018,36(3):663-675.

Chen ZHANG, Yijun HOU, Jian LI. Wave-current interaction during Typhoon Nuri (2008) and Hagupit (2008): an application of the coupled ocean-wave modeling system in the northern South China Sea[J]. Chinese Journal of Oceanology and Limnology, 2018, 36(3): 663-675.
张晨, 侯一筠, 李健. Wave-current interaction during Typhoon Nuri (2008) and Hagupit (2008): an application of the coupled ocean-wave modeling system in the northern South China Sea[J]. 海洋湖沼学报（英文）, 2018,36(3):663-675. DOI： 10.1007/s00343-018-6088-y.

Chen ZHANG, Yijun HOU, Jian LI. Wave-current interaction during Typhoon Nuri (2008) and Hagupit (2008): an application of the coupled ocean-wave modeling system in the northern South China Sea[J]. Chinese Journal of Oceanology and Limnology, 2018, 36(3): 663-675. DOI： 10.1007/s00343-018-6088-y.

摘要

Abstract

The northern South China Sea (SCS) is frequently affected by typhoons. During severe storm events

wave-current interactions produce storm surges causing enormous damage in the path of the typhoon. To evaluate the influence of wave-current interactions on storm surge

we used a coupled ocean-atmospherewave-sediment transport (COAWST) modeling system with radiation-stress and vortex-force formulations to simulate two typically intense tropical storms that invaded the SCS

namely Typhoons Nuri (2008) and Hagupit (2008)

and compared results with observations from the Hong Kong Observatory. Both radiationstress and vortex-force formulations significantly improved the accuracy of the simulation. Depending on which typhoon and the topography encountered

the influence of surface waves on the oceanic circulation showed different characteristics

including the differences of range and intensity of storm surge between vortex-force and radiation-stress experiments. During typhoon landing

strong sea-surface elevation in concert with wave set-up/set-down caused the adjustment of the momentum balance. In the direction perpendicular to the current

but especially in the cross-shore direction

the pressure gradient and wave effects on the current dominated the momentum balance.

关键词

Keywords

references

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