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浪流相互作用对北部湾内波浪、冷水团及冲淡水的影响研究
引用本文:杨婧灵,姜绍材,吴俊杉,谢玲玲,张书文,白鹏.浪流相互作用对北部湾内波浪、冷水团及冲淡水的影响研究[J].海洋学报(英文版),2020,39(1):25-40.
作者姓名:杨婧灵  姜绍材  吴俊杉  谢玲玲  张书文  白鹏
作者单位:广东海洋大学海洋与气象学院, 广东省近海海洋变化与灾害预警重点实验室, 湛江, 524088;南方海洋科学与工程广东省实验室(湛江), 湛江, 524025,自然资源部南海局北海海洋环境监测中心站, 北海, 536000,自然资源部东海局, 上海, 200137,广东海洋大学海洋与气象学院, 广东省近海海洋变化与灾害预警重点实验室, 湛江, 524088;南方海洋科学与工程广东省实验室(湛江), 湛江, 524025,海洋科学研究院, 理学院, 汕头大学, 汕头, 515063,广东海洋大学海洋与气象学院, 广东省近海海洋变化与灾害预警重点实验室, 湛江, 524088;南方海洋科学与工程广东省实验室(湛江), 湛江, 524025
基金项目:The Program for Scientific Research Start-up Funds of Guangdong Ocean University under contract No. 101302/R18001; the Fund of Southern Marine Science and Engineering Guangdong Laboratory (Zhanjiang) under contract No. ZJW-2019-08; the National Key Research and Development Program of China under contract No. 2016YFC1401403; the National Natural Science Foundation of China under contract Nos 41476009 and 41776034.
摘    要:Wave-current interaction and its effects on the hydrodynamic environment in the Beibu Gulf(BG) have been investigated via employing the Coupled Ocean–Atmosphere–Wave–Sediment Transport(COAWST) modeling system. The model could simulate reasonable hydrodynamics in the BG when validated by various observations.Vigorous tidal currents refract the waves efficiently and make the seas off the west coast of Hainan Island be the hot spot where currents modulate the significant wave height dramatically. During summer, wave-enhanced bottom stress could weaken the near-shore component of the gulf-scale cyclonic-circulation in the BG remarkably, inducing two major corresponding adjustments: Model results reveal that the deep-layer cold water from the southern BG makes critical contribution to maintaining the cold-water mass in the northern BG Basin.However, the weakened background circulation leads to less cold water transported from the southern gulf to the northern gulf, which finally triggers a 0.2°C warming in the cold-water mass area; In the top areas of the BG, the suppressed background circulation reduces the transport of the diluted water to the central gulf. Therefore, more freshwater could be trapped locally, which then triggers lower sea surface salinity(SSS) in the near-field and higher SSS in the far-field.

关 键 词:浪流相互作用  北部湾  河口羽流  冷水团  COAWST
收稿时间:2018/12/19 0:00:00

Effects of wave-current interaction on the waves,cold-water mass and transport of diluted water in the Beibu Gulf
Yang,Jingling,Jiang,Shaocai,Wu,Junshan,Xie,Lingling,Zhang,Shuwen,Bai,Peng.Effects of wave-current interaction on the waves,cold-water mass and transport of diluted water in the Beibu Gulf[J].Acta Oceanologica Sinica,2020,39(1):25-40.
Authors:Yang  Jingling  Jiang  Shaocai  Wu  Junshan  Xie  Lingling  Zhang  Shuwen  Bai  Peng
Institution:Guangdong Province Key Laboratory for Coastal Ocean Variation and Disaster Prediction, College of Ocean andMeteorology, Guangdong Ocean University, Zhanjiang 524088, China;Marine Resources Big Data Center of South China Sea, Southern Marine Science and Engineering Guangdong Laboratory (Zhanjiang), Zhanjiang 524025, China;Beihai Marine Environmental Monitoring Center, South China Sea Bureau of Ministry of Natural Resources, Beihai 536000, China;East China Sea Bureau of Ministry of Natural Resources, Shanghai 200137, China;Institute of Marine Science, College of Science, Shantou University, Shantou 515063, China
Abstract:Acta Oceanologica Sinica - Wave-current interaction and its effects on the hydrodynamic environment in the Beibu Gulf (BG) have been investigated via employing the Coupled...
Keywords:wave-current interaction  Beibu Gulf  river plume  cold-water mass  COAWST
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