Analysis of Wave Distribution Simulated by WAVEWATCH-III Model in Typhoons Passing Beibu Gulf, China
Shao, Weizeng1; Sheng, Yexin1; Li, Huan2; Shi, Jian3; Ji, Qiyan1; Tan, Wei4; Zuo, Juncheng1
刊名ATMOSPHERE
2018-07
卷号9期号:7
关键词wave distribution typhoon WAVEWATCH-III Beibu Gulf
ISSN号2073-4433
DOI10.3390/atmos9070265
英文摘要The Beibu Gulf is an important offshore region in the South China Sea for the fishing industry and other human activities. In 2017, typhoons Doksuri and Khanun passed the Beibu Gulf in two paths, at maximum wind speeds of up to 50 m/s. Typhoon Doksuri passed the Beibu Gulf through the open waters of the South China Sea and Typhoon Khanun moved towards the Beibu Gulf through the narrow Qiongzhou Strait. The aim of this study is to analyze the typhoon-induced wave distribution in the Beibu Gulf. WAVEWATCH-III (WW3) is a third-generation numeric wave model developed by the National Oceanic and Atmospheric Administration (NOAA), which has been widely used for sea wave research. The latest version of the WW3 (5.16) model provides three packages of nonlinear term for four wave components (quadruplets) wave-wave interactions, including Discrete Interaction Approximation (DIA), Full Boltzmann Integral (WRT), and Generalized Multiple DIA (GMD) with two kinds of coefficients, herein called GMD1 and GMD2. These four packages have been conveniently implemented for simulating wave fields in two typhoons after taking winds from the European Centre for Medium-RangeWeather Forecasts (ECMWF) at 0.125 degrees grids as the forcing fields. It was found that the GMD2 package was the recommended option of the nonlinear term for quadruplets wave-wave interactions due to the minimum error when comparing a number of simulated results from the WW3 model with significant wave height (SWH) from ECMWF and altimeter Jason-2. Then the wave distribution simulated by the WW3 model employing the GMD2 package was analyzed. In the case of Typhoon Doksuri, wind-sea dominated in the early and middle stages while swell dominated at the later stage. However, during Typhoon Khanun, wind-sea dominated throughout and swell distributed outside the bay around the east of Hainan Island, because the typhoon-induced swell at mesoscale was difficult to propagate into the Beibu Gulf through the narrow Qiongzhou Strait.
资助项目ESA Dragon-4 program[32235]
WOS关键词LINEAR ENERGY TRANSFER ; SEA ; WIND ; SPECTRUM ; VALIDATION ; CLIMATE ; HEIGHT ; OCEAN ; HINDCAST
WOS研究方向Meteorology & Atmospheric Sciences
语种英语
出版者MDPI
WOS记录号WOS:000445141400029
内容类型期刊论文
源URL[http://ir.fio.com.cn:8080/handle/2SI8HI0U/25884]  
专题自然资源部第一海洋研究所
通讯作者Shao, Weizeng
作者单位1.Zhejiang Ocean Univ, Marine Sci & Technol Coll, Zhoushan 316022, Peoples R China
2.Natl Marine Data & Informat Serv, Tianjin 300171, Peoples R China
3.Natl Univ Def Technol, Coll Meteorol & Oceanog, Nanjing 210007, Jiangsu, Peoples R China
4.State Ocean Adm, Inst Oceanog 1, Qingdao 266061, Peoples R China
推荐引用方式
GB/T 7714
Shao, Weizeng,Sheng, Yexin,Li, Huan,et al. Analysis of Wave Distribution Simulated by WAVEWATCH-III Model in Typhoons Passing Beibu Gulf, China[J]. ATMOSPHERE,2018,9(7).
APA Shao, Weizeng.,Sheng, Yexin.,Li, Huan.,Shi, Jian.,Ji, Qiyan.,...&Zuo, Juncheng.(2018).Analysis of Wave Distribution Simulated by WAVEWATCH-III Model in Typhoons Passing Beibu Gulf, China.ATMOSPHERE,9(7).
MLA Shao, Weizeng,et al."Analysis of Wave Distribution Simulated by WAVEWATCH-III Model in Typhoons Passing Beibu Gulf, China".ATMOSPHERE 9.7(2018).
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