Rogue waves during Typhoon Trami in the East China Sea

Xingjie JIANG; Changlong GUAN; Daolong WANG

doi:10.1007/s00343-019-8256-0

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Rogue waves during Typhoon Trami in the East China Sea

Updated：2023-05-20

- Rogue waves during Typhoon Trami in the East China Sea
- Rogue waves during Typhoon Trami in the East China Sea
- 海洋湖沼学报（英文） 2019年37卷第6期页码：1817-1836
- Affiliations：
  
  1.First Institute of Oceanography (FIO), Ministry of Natural Resources (MNR), Qingdao 266061, China
  2.Ocean University of China, Qingdao 266071, China
- Author bio：
  
  JIANG Xingjie, E-mail:jiangxj@fio.org.cn
- Funds：
  
  the National Key Research and Development Program of China(2016YFC1402004);the National Key Research and Development Program of China(2016YFC1401805)
- DOI：10.1007/s00343-019-8256-0
  中图分类号：
- 收稿：2018-09-25，
  
  录用：2018-11-28，
  
  网络首发：2019-03-19，
  
  纸质出版：2019-11
- Accepted：
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Rogue waves during Typhoon Trami in the East China Sea[J]. 海洋湖沼学报（英文）, 2019,37(6):1817-1836.

Xingjie JIANG, Changlong GUAN, Daolong WANG. Rogue waves during Typhoon Trami in the East China Sea[J]. Journal of Oceanology and Limnology, 2019, 37(6): 1817-1836.
Rogue waves during Typhoon Trami in the East China Sea[J]. 海洋湖沼学报（英文）, 2019,37(6):1817-1836. DOI： 10.1007/s00343-019-8256-0.

Xingjie JIANG, Changlong GUAN, Daolong WANG. Rogue waves during Typhoon Trami in the East China Sea[J]. Journal of Oceanology and Limnology, 2019, 37(6): 1817-1836. DOI： 10.1007/s00343-019-8256-0.

摘要

Abstract

As concluded from physical theory and laboratory experiment

it is widely accepted that nonlinearities of sea state play an important role in the formation of rogue waves; however

the sea states and corresponding nonlinearities of real-world rogue wave events remain poorly understood. Three rogue waves were recorded by a directional buoy located in the East China Sea during Typhoon Trami in August 2013. This study used the WAVEWATCH Ⅲ model to simulate the sea state conditions pertaining to when and where those rogue waves were observed

based on which a comprehensive and full-scale analysis was performed. From the perspectives of wind and wave fields

wave system tracking

High-Order Spectral method simulation

and some characteristic sea state parameters

we concluded that the rogue waves occurred in sea states dominated by second-order nonlinearities. Moreover

third-order modulational instabilities were suppressed in these events because of the developed or fully developed sea state determined by the typhoon wave system. The method adopted in this study can provide comprehensive and full-scale analysis of rogue waves in the real world. The case studied in this paper is not considered unique

and rules could be found and confirmed in relation to other typhoon sea states through the application of our proposed method.

关键词

Keywords

references

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