中国物理B ›› 2012, Vol. 21 ›› Issue (10): 109201-109201.doi: 10.1088/1674-1056/21/10/109201

• GEOPHYSICS, ASTRONOMY, AND ASTROPHYSICS • 上一篇    下一篇

Effect of oceanic current on typhoon-wave modeling in the East China Sea

崔红a, 何海伦a b, 刘晓辉a, 李熠a   

  1. a State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China;
    b Key Laboratory of Coastal Disaster and Defense of Ministry of Education, Hohai University, Nanjing 210098, China
  • 收稿日期:2012-02-10 修回日期:2012-06-28 出版日期:2012-09-01 发布日期:2012-09-01
  • 基金资助:
    Project supported by the Public Science and Technology Research Funds of Ocean (Grant No. 201105018), the Young Scientist Fund of the National Natural Science Foundation of China (Grant No. 41106019), the Natural Science Foundation of Jiangsu Province of China (Grant No. BK2012315), and the Young Scientist Fund of State Oceanic Administration, China (Grant No. 2011258).

Effect of oceanic current on typhoon-wave modeling in the East China Sea

Cui Hong (崔红)a, He Hai-Lun (何海伦)a b, Liu Xiao-Hui (刘晓辉)a, Li Yi (李熠)a   

  1. a State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China;
    b Key Laboratory of Coastal Disaster and Defense of Ministry of Education, Hohai University, Nanjing 210098, China
  • Received:2012-02-10 Revised:2012-06-28 Online:2012-09-01 Published:2012-09-01
  • Contact: He Hai-Lun E-mail:hehailun@sio.org.cn
  • Supported by:
    Project supported by the Public Science and Technology Research Funds of Ocean (Grant No. 201105018), the Young Scientist Fund of the National Natural Science Foundation of China (Grant No. 41106019), the Natural Science Foundation of Jiangsu Province of China (Grant No. BK2012315), and the Young Scientist Fund of State Oceanic Administration, China (Grant No. 2011258).

PDF (PC)

1049

赞

摘要： We use the WAVEWATCH-III model to quantify the effect of oceanic current on typhoon-wave modeling in the East-China-Sea (ECS). Typhoons Jelawat and Saomai in the autumn of 2000 are hindcasted. The oceanic currents in the ECS are mainly constituted of Kuroshio and typhoon-generated currents. The results show distinguishable differences in wave height and wave period under the typhoon conditions. The oceanic current causes the maximum differences, of up to a 0.5 m significant wave height and a 1 s mean wave period. Comparisons between typhoons Jelawat and Saomai show the dependence of the current effect on the typhoon characteristics.

关键词: wave-current interaction, East China Sea, typhoon wave, WAVEWATCH-III

Abstract: We use the WAVEWATCH-III model to quantify the effect of oceanic current on typhoon-wave modeling in the East-China-Sea (ECS). Typhoons Jelawat and Saomai in the autumn of 2000 are hindcasted. The oceanic currents in the ECS are mainly constituted of Kuroshio and typhoon-generated currents. The results show distinguishable differences in wave height and wave period under the typhoon conditions. The oceanic current causes the maximum differences, of up to a 0.5 m significant wave height and a 1 s mean wave period. Comparisons between typhoons Jelawat and Saomai show the dependence of the current effect on the typhoon characteristics.

Key words: wave-current interaction, East China Sea, typhoon wave, WAVEWATCH-III

中图分类号:  (Ocean waves and oscillations)

  • 92.10.Hm
92.10.Fj (Upper ocean and mixed layer processes) 92.40.Cy (Modeling; general theory) 92.60.Qx (Storms)