Typhoon-induced wind waves in the northern East China Sea during two typhoon events: the impact of wind field and wave-current interaction

Zhao LI; Shuiqing LI; Yijun HOU; Dongxue MO; Jian LI; Baoshu YIN

doi:10.1007/s00343-021-1089-7

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Typhoon-induced wind waves in the northern East China Sea during two typhoon events: the impact of wind field and wave-current interaction

Physics | Updated：2023-05-20

- Typhoon-induced wind waves in the northern East China Sea during two typhoon events: the impact of wind field and wave-current interaction
- Typhoon-induced wind waves in the northern East China Sea during two typhoon events: the impact of wind field and wave-current interaction
- 海洋湖沼学报（英文） 2022年40卷第3期页码：934-949
- Affiliations：
  
  1.Key Laboratory of Ocean Circulation and Waves, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
  2.Laboratory for Ocean and Climate Dynamics, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao 266237, China
  3.University of Chinese Academy of Sciences, Beijing 100049, China
  4.Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao 266071, China
  5.North China Sea Marine Forecasting Center of State Oceanic Administration, Qingdao 266061, China
- Author bio：
  
  Shuiqing LI, lishuiqing@qdio.ac.cn
  Baoshu YIN, bsyin@qdio.ac.cn
- Funds：
  
  the National Natural Science Foundation of China(U1706216);the National Natural Science Foundation of China(41976010);the National Natural Science Foundation of China(42006027);the National Natural Science Foundation of China(U1806227);the Natural Science Foundation of Shandong Province, China(ZR2016DQ16);the Key Deployment Project of Center for Ocean Mega-Science, Chinese Academy of Sciences(COMS2019J02);the Key Deployment Project of Centre for Ocean Mega-Research of Science, Chinese Academy of Sciences(COMS2019J05);the CAS Strategic Priority Project(XDA19060202);the Chinese Academy of Sciences Strategic Priority Project(XDA19060502);the National Key Research and Development Program of China(2016YFC1402000);© Chinese Society for Oceanology and Limnology, Science Press and Springer-Verlag GmbH Germany, part of Springer Nature 2022
- DOI：10.1007/s00343-021-1089-7
  中图分类号：
- 纸质出版：2022-03
- Accepted：
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Typhoon-induced wind waves in the northern East China Sea during two typhoon events: the impact of wind field and wave-current interaction[J]. 海洋湖沼学报（英文）, 2022,40(3):934-949.

Zhao LI, Shuiqing LI, Yijun HOU, et al. Typhoon-induced wind waves in the northern East China Sea during two typhoon events: the impact of wind field and wave-current interaction[J]. Journal of Oceanology and Limnology, 2022, 40(3): 934-949.
Typhoon-induced wind waves in the northern East China Sea during two typhoon events: the impact of wind field and wave-current interaction[J]. 海洋湖沼学报（英文）, 2022,40(3):934-949. DOI： 10.1007/s00343-021-1089-7.

Zhao LI, Shuiqing LI, Yijun HOU, et al. Typhoon-induced wind waves in the northern East China Sea during two typhoon events: the impact of wind field and wave-current interaction[J]. Journal of Oceanology and Limnology, 2022, 40(3): 934-949. DOI： 10.1007/s00343-021-1089-7.

摘要

Abstract

We examined the influences of the wind field and wave-current interaction (WCI) on the numerical simulation results of typhoon-induced wind waves in the northern East China Sea (NECS) using the coupled Simulating Waves Nearshore+Advanced Circulation (SWAN+ADCIRC) model. The simulations were performed during two typhoon events (Lekima and Muifa)

and two widely used reanalysis wind fields

the Climate Forecast System Version 2 (CFSv2) from the National Centers for Environmental Prediction (NCEP) and the fifth-generation European Centre for Medium-Range Weather Forecasts (ECMWF) Reanalysis (ERA5)

were compared. The results indicate that the ERA5 and CFSv2 wind fields both reliably reproduced the wind variations measured by in-situ buoys

and the accuracy of the winds from ERA5 were generally better than those from CFSv2 because CFSv2 tended to overestimate the wind speed and the simulated significant wave height (SWH)

particularly the peak SWH. The WCI effects between the two wind field simulations were similar; these effects enhanced the SWH throughout the nearshore NECS during both typhoons but suppressed the SWH on the right side of the Typhoon Muifa track in the deep and offshore sea areas. In summary

variations in the water depth and current propagation direction dominate the modulation of wave height.

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Keywords

references

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