首页|Typhoon-Induced Ocean Waves and Stokes Drift:A Case Study of Typhoon Mangkhut(2018)

Typhoon-Induced Ocean Waves and Stokes Drift:A Case Study of Typhoon Mangkhut(2018)

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Ocean waves and Stokes drift are generated by typhoons.This study investigated the characteristics of ocean waves and wave-induced Stokes drift and their effects during Typhoon Mangkhut using European Centre for Medium-Range Weather Forecasts(ECMWF)ERA5 datasets and observational data.The results revealed that the typhoon generated intense cyclones and huge typhoon waves with a maximum wind speed of 45 m/s,a minimum pressure of 955 hPa,and a maximum significant wave height of 12 m.The Stokes drift caused by typhoon waves exceeded 0.6 m/s,the Stokes depth scale exceeded 18 m,and the maximum Stokes transport reached 6 m2/s.The spatial distribution of 10-m wind speed,typhoon wave height,Stokes drift,Stokes depth,and Stokes transport during the typhoon was highly correlated with the typhoon track.The distribution along the typhoon track showed significant zonal asymme-try,with greater intensity on the right side of the typhoon track than on the left side.These findings provide important insights into the impact of typhoons on ocean waves and Stokes drift,thus improving our understanding of the inter-actions between typhoons and the ocean environment.This study also investigated the contribution of Stokes transport to the total net transport during typhoons using Ekman-Stokes Numbers as a comparative measure.The results indicated that the ratio of Stokes transport to the total net transport reached up to 50%within the typhoon radius,while it was approximately 30%outside the radius.Strong Stokes transport induced by typhoon waves led to divergence in the transport direction,which resulted in upwelling of the lower ocean as a compensation current.Thus,Stokes transport played a crucial role in the vertical mixing of the ocean during typhoons.The findings suggested that Stokes transport should be paid more attention to,particularly in high latitude ocean regions,where strong winds can amplify its effects.

Stokes drifttyphoon wavesEkman-Stokes transportvertical mixingTyphoon Mangkhut

WU Zhi-yuan、GAO Kai、CHEN Jie、ZHANG Hao-jian、DENG Bin、JIANG Chang-bo、LIU Yi-zhuang、LYU Zhao、YAN Ren

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School of Hydraulic and Environmental Engineering,Changsha University of Science&Technology,Changsha 410114,China

Key Laboratory of Water-Sediment Sciences and Water Disaster Prevention of Hunan Province,Changsha 410114,China

State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering,Hohai University,Nanjing 210024,China

State Key Laboratory of Coastal and Offshore Engineering,Dalian University of Technology,Dalian 116024,China

School of Civil Engineering,Hunan University of Technology,Zhuzhou 412007,China

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国家重点研发计划国家自然科学基金Belt and Road Special Foundation of the State Key Laboratory of Hydrology-Water Resources and Hydraulic EngineeringOpen Research Foundation of the State Key Laboratory of Coastal and Offshore Engineering,Dalian University of TechnologyScience and Technology Innovation Program of Hunan Province湖南省自然科学基金Educational Science Foundation of Hunan Province

2021YFB2601100521712462019491911LP20052023RC31362022JJ2004123A0265

2024

中国海洋工程(英文版)
中国海洋学会

中国海洋工程(英文版)

CSTPCDEI
影响因子:0.338
ISSN:0890-5487
年,卷(期):2024.38(4)
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