中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Dynamics of wave generation and dissipation processes during cold wave events in the Bohai Sea

文献类型:期刊论文

作者Peng, Jie3,4; Mao, Miaohua3,4; Xia, Meng1,2
刊名ESTUARINE COASTAL AND SHELF SCIENCE
出版日期2023-01-05
卷号280页码:21
关键词Wave dynamics Winds Cold wave events Numerical model Bohai Sea
ISSN号0272-7714
DOI10.1016/j.ecss.2022.108161
通讯作者Mao, Miaohua(mhmao@yic.ac.cn)
英文摘要Wave dynamics were investigated by applying the wind-wave model Simulating Waves Nearshore to the semi -enclosed Bohai Sea during cold wave events. Wind quality was examined by comparing three wind data sour-ces with buoy observations, and then numerical experiments were conducted to investigate the impacts of model physics settings on simulated waves. After model calibration, the wave dynamics were examined from the aspects of response to various wind conditions (speed, fetch, duration), wave dominant component (wind wave or swell), as well as the dissipation processes during a pair of cold wave events (e.g., northwesterly in 2014 and north-easterly in 2015) with the consideration of spatial differences. The maximum significant wave heights during two cold wave events are similar (e.g., 3.5 m in the central Bohai Basin), which attributes to the impacts of limited fetch difference and insufficient high wind duration. Wind wave is the dominant component, which is reflected in the wave spectra (e.g., wave age less than 1.2). Spatial regions of wave dissipations controlled by whitecapping, bottom friction, and depth-induced breaking during cold wave events are quantified. Whitecapping dominates the wave energy dissipation in deep-water areas, while the bottom friction dissipation controls the major dissipation process as waves propagate towards the coast (e.g., at 5-10 m water depths). Depth-induced dissi-pation only occurs over a narrow strip along the southern coastal area but is significantly beyond the others. Depth-induced dissipation decreases suddenly when reaches a flat bottom, and it decreases with the increase of the width of the bottom slope.
WOS关键词SHALLOW-WATER ; WIND STRESS ; WHITECAPPING DISSIPATION ; SURFACE WIND ; BLACK-SEA ; COASTAL ; MODEL ; CHINA ; SWAN ; SPECTRA
WOS研究方向Marine & Freshwater Biology ; Oceanography
语种英语
WOS记录号WOS:000891762400002
资助机构National Natural Science Foundation of China ; Yantai City Double Hundred Plan Elite Program ; Chinese Academy of Sciences BRJH Program ; Yantai Institute of Coastal Zone Research, Chinese Academy of Sciences
源URL[http://ir.yic.ac.cn/handle/133337/31912]  
专题烟台海岸带研究所_中科院海岸带环境过程与生态修复重点实验室
烟台海岸带研究所_近岸生态与环境实验室
通讯作者Mao, Miaohua
作者单位1.Univ Maryland Eastern Shore, Dept Nat Sci, Princess Anne, MD 21853 USA
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.Shandong Key Lab Coastal Environm Proc, Yantai 264003, Shandong, Peoples R China
4.Chinese Acad Sci, Yantai Inst Coastal Zone Res, CAS Key Lab Coastal Environm Proc & Ecol Remediat, Yantai 264003, Shandong, Peoples R China
推荐引用方式
GB/T 7714
Peng, Jie,Mao, Miaohua,Xia, Meng. Dynamics of wave generation and dissipation processes during cold wave events in the Bohai Sea[J]. ESTUARINE COASTAL AND SHELF SCIENCE,2023,280:21.
APA Peng, Jie,Mao, Miaohua,&Xia, Meng.(2023).Dynamics of wave generation and dissipation processes during cold wave events in the Bohai Sea.ESTUARINE COASTAL AND SHELF SCIENCE,280,21.
MLA Peng, Jie,et al."Dynamics of wave generation and dissipation processes during cold wave events in the Bohai Sea".ESTUARINE COASTAL AND SHELF SCIENCE 280(2023):21.

入库方式: OAI收割

来源:烟台海岸带研究所

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