Numerical study of tidal effect on the water flux across the Korea/Tsushima Strait | |
Jiang, Wenxin1,2,3,4,5; Yang, Dezhou1,2,3,4,5; Xu, Lingjing1,2,3,4; He, Zhiwei1,2,3,4; Cui, Xuan1,2,3,4; Yin, Baoshu1,2,3,4,5 | |
刊名 | FRONTIERS IN MARINE SCIENCE |
2023-11-20 | |
卷号 | 10页码:14 |
关键词 | Korea/Tsushima Strait Tsushima warm current East China Sea tide numerical modeling |
DOI | 10.3389/fmars.2023.1287611 |
通讯作者 | Yang, Dezhou(yangdezhou@qdio.ac.cn) |
英文摘要 | Tremendous amounts of materials and energy are transported from the East China Sea (ECS) to the East/Japan Sea (EJS) through the Korea/Tsushima Strait (KTS). Tides undoubtedly play an important role in regulating ocean circulation on the broad continental shelf of the ECS, while the effects of tides on the water exchange between the ECS and EJS remain unclear. Using a three-dimensional Regional Oceanic Modeling System (ROMS) circulation model, we conducted numerical experiments with tides, without tides, and only barotropic tides. The results showed that the water flux across the KTS can increase by up to 13% (in summer) when excluding tides from the numerical simulation. To understand how tidal forcing regulates the KTS water flux, we performed a dynamic diagnostic analysis and revealed that the variation in sea surface height under tidal effect is the main reason for the water flux variation across the KTS. The tidal effect can adjust the sea surface height, weaken the pressure gradient and reduce the water flux across the KTS, which affect the intensity of water exchange between the ECS and EJS. The tidal effect can alter sea level difference between the Taiwan Strait and the KTS, which influences the KTS water flux. Tides can also influence the KTS water flux by altering the sea surface height through interaction with topography and stratification. We also found that tidal effect weakens the northward intrusion of the Yellow Sea Warm Current in winter and in turn enhances the water flux across the KTS according to volume conservation. These modeling results imply that tides must be considered when simulating the ocean environment of the northwestern Pacific Ocean. |
资助项目 | Key Research Infrastructures in the Field Stations of Chinese Academy of Sciences[KFJ-SW-YW047] ; Laoshan Laboratory Science and Technology Innovation Project[LSKJ202202504] ; Laoshan Laboratory Science and Technology Innovation Project[LSKJ2022020103] ; National Natural Science Foundation of China (NSFC)[92158202] ; National Natural Science Foundation of China (NSFC)[42076022] ; Strategic Priority Research Program, CAS[XDB42000000] ; CAS-CSIRO BAU project[133137KYSB20180141] ; High-Performance Computing Center at the Institute of Oceanology, CAS (IOCAS) ; Youth Innovation Promotion Association, CAS |
WOS关键词 | TSUSHIMA WARM CURRENT ; EAST CHINA SEA ; VOLUME TRANSPORT ; KOREA STRAIT ; YELLOW SEA ; SYSTEM ; VARIABILITY ; MECHANISM ; EXTENSION ; CURRENTS |
WOS研究方向 | Environmental Sciences & Ecology ; Marine & Freshwater Biology |
语种 | 英语 |
出版者 | FRONTIERS MEDIA SA |
WOS记录号 | WOS:001115124300001 |
内容类型 | 期刊论文 |
源URL | [http://ir.qdio.ac.cn/handle/337002/184125] |
专题 | 海洋研究所_海洋生态与环境科学重点实验室 |
通讯作者 | Yang, Dezhou |
作者单位 | 1.Chinese Acad Sci, Inst Oceanol, CAS Key Lab Ocean Circulat & Waves, Qingdao, Peoples R China 2.Pilot Natl Lab Marine Sci & Technol, Qingdao, Peoples R China 3.Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao, Peoples R China 4.Chinese Acad Sci, CAS Engn Lab Marine Ranching, Inst Oceanol, Qingdao, Peoples R China 5.Univ Chinese Acad Sci, Beijing, Peoples R China |
推荐引用方式 GB/T 7714 | Jiang, Wenxin,Yang, Dezhou,Xu, Lingjing,et al. Numerical study of tidal effect on the water flux across the Korea/Tsushima Strait[J]. FRONTIERS IN MARINE SCIENCE,2023,10:14. |
APA | Jiang, Wenxin,Yang, Dezhou,Xu, Lingjing,He, Zhiwei,Cui, Xuan,&Yin, Baoshu.(2023).Numerical study of tidal effect on the water flux across the Korea/Tsushima Strait.FRONTIERS IN MARINE SCIENCE,10,14. |
MLA | Jiang, Wenxin,et al."Numerical study of tidal effect on the water flux across the Korea/Tsushima Strait".FRONTIERS IN MARINE SCIENCE 10(2023):14. |
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