Analysis of the typhoon wave distribution simulated in WAVEWATCH-Ⅲ model in the context of Kuroshio and wind-induced current

Yuyi HU; Weizeng SHAO; Jian SHI; Jian SUN; Qiyan JI; Lina CAI

doi:10.1007/s00343-019-9133-6

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Analysis of the typhoon wave distribution simulated in WAVEWATCH-Ⅲ model in the context of Kuroshio and wind-induced current

Special Section on Indo-Pac Project | Updated：2023-04-27

- Analysis of the typhoon wave distribution simulated in WAVEWATCH-Ⅲ model in the context of Kuroshio and wind-induced current
- Analysis of the typhoon wave distribution simulated in WAVEWATCH-Ⅲ model in the context of Kuroshio and wind-induced current
- 海洋湖沼学报（英文） 2020年38卷第6期页码：1692-1710
- Affiliations：
  
  1.Marine Science and Technology College, Zhejiang Ocean University, Zhoushan 316022, China
  2.College of Meteorology and Oceanography, National University of Defense Technology, Nanjing 210007, China
  3.Physical Oceanography Laboratory, Ocean University of China, Qingdao 266100, China
- Author bio：
  
  SHAO Weizeng, shaoweizeng@zjou.edu.cn
- Funds：
  
  the Fundamental Research Funds for Zhejiang Provincial Universities and Research Institutes(2019J00010);the National Key R&D Program of China(2017YFA0604901);the National Natural Science Foundation of China(41806005);the National Natural Science Foundation for Young Scientists of China(41776183);the National Natural Science Foundation of China(41706206);the Public Welfare Technical Applied Research Project of Zhejiang Province of China(LGF19D060003);the Science and Technology Project of Zhoushan City(2019C21008);© Chinese Society for Oceanology and Limnology, Science Press and Springer-Verlag GmbH Germany, part of Springer Nature 2020
- DOI：10.1007/s00343-019-9133-6
  中图分类号：
- 收稿：2019-05-16，
  
  录用：2019-8-14，
  
  网络首发：2019-10-19，
  
  纸质出版：2020-11
- Accepted：
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Analysis of the typhoon wave distribution simulated in WAVEWATCH-Ⅲ model in the context of Kuroshio and wind-induced current[J]. 海洋湖沼学报（英文）, 2020,38(6):1692-1710.

Yuyi HU, Weizeng SHAO, Jian SHI, et al. Analysis of the typhoon wave distribution simulated in WAVEWATCH-Ⅲ model in the context of Kuroshio and wind-induced current[J]. Journal of Oceanology and Limnology, 2020, 38(6): 1692-1710.
Analysis of the typhoon wave distribution simulated in WAVEWATCH-Ⅲ model in the context of Kuroshio and wind-induced current[J]. 海洋湖沼学报（英文）, 2020,38(6):1692-1710. DOI： 10.1007/s00343-019-9133-6.

Yuyi HU, Weizeng SHAO, Jian SHI, et al. Analysis of the typhoon wave distribution simulated in WAVEWATCH-Ⅲ model in the context of Kuroshio and wind-induced current[J]. Journal of Oceanology and Limnology, 2020, 38(6): 1692-1710. DOI： 10.1007/s00343-019-9133-6.

摘要

Abstract

To investigate the relationship between surface currents and wave distributions in typhoons

we took the Typhoon Talim in 2017 as a case

and found that the track of the typhoon winds up to 50 m/s was almost consistent with the Kuroshio track

particularly from September 13 to 16

2017. The surface current data

derived from the NCEP Climate Forecast System Version 2 (CFSv2) from the National Center of Atmospheric Research (NCAR)

revealed that the speed of the wind-induced current exceeded that of the Kuroshio in the region with the maximum wind speed. In this study

was utilized a third-generation numeric wave model

WAVEWATCH-Ⅲ (the latest version 5.16)

developed by the National Oceanic and Atmospheric Administration (NOAA)

to simulate the wave fields of Typhoon Talim using the European Centre for Medium-Range Weather Forecasts (ECMWF) reanalysis wind data in 0.125°×0.125° grid as the forcing field. We found that the root-mean-square error (RMSE) of the significant wave height (SWH) was 0.34 m when validated against measurements from altimeter Jason-2. In addition

we discovered that the SWH had a similar tendency to the change in the surface current speed that was approximately 0.5 m/s at the beginning of Typhoon Talim. However

the relationship became weak as the surface current speed was below 0.2 m/s. Our findings show that the distribution of typhoon waves is resulted from the interaction of surface current and the wind-sea portion of the wave system

since the distribution pattern of wind-sea is consistent with the surface current

and there is a weak relationship between surface current and swell.

关键词

Keywords

references

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