The features and mechanisms of the North Shandong Coastal Current: a case study in 2014

doi:10.1007/s10872-021-00597-3

CORC > 烟台海岸带研究所 > 中国科学院烟台海岸带研究所 > 中科院海岸带环境过程与生态修复重点实验室

	The features and mechanisms of the North Shandong Coastal Current: a case study in 2014
	Zheng, Xiangyang 1,2,3; Zhang, Hua 1,2,3; Li, Yanfang 1,2,3; Zou, Tao 1,2,3; Liu, Xin 1,2,3; Xing, Qianguo 1,2,3
刊名	JOURNAL OF OCEANOGRAPHY
	2021-02-26
页码	16
关键词	The North Shandong Coastal Current North Yellow Sea Observational current velocity data Winter large wind events Momentum analysis
ISSN号	0916-8370
DOI	10.1007/s10872-021-00597-3
通讯作者	Xing, Qianguo(qgxing@yic.ac.cn)
英文摘要	The North Shandong Coastal Current (NSCC) is an important transporting route for sediment, drifting algae, and spilled oil from the Bohai Sea to the Yellow Sea. This study investigated the features and formation mechanism of the NSCC using observational data of current velocity and a numerical coastal ocean model. Our results confirmed the existence of the NSCC in the sense of climatological current in winter when northerly wind prevails in the Bohai Sea and Yellow Sea. The magnitude of the NSCC in the monthly time scale ranged 0.07-0.12 m/s and the current direction was parallel to the coastline. The detided residual current on the pathway of the NSCC was unstable, but variable with the local wind speed. The residual current was well correlated with northerly wind speed and tended to be parallel to coastline with the increase of wind speed. Strong wind plays key roles in the formation of eastward mean flow on the pathway of the NSCC in winter. We found that strong wind can generate a stronger eastward current in the southern side of the northern Yellow Sea, but a smaller westward return flow during the strong wind relaxation period. The asymmetry of wind-related residual current during and after strong wind events accounts for the formation of the eastward NSCC. A momentum analysis was performed using the numerical model results during strong wind events. We found that the barotropic pressure gradient was the dominant driving force of the residual current both during and after a strong wind event.
资助项目	Key Deployment Project of Centre for Ocean Mega-Research of Science, Chinese academy of sciences[COMS2019J05] ; Strategic Priority Research Program of the Chinese Academy of Sciences Grant[XDA19060205] ; Key Research and Development project of Yantai[2017ZH095]
WOS研究方向	Oceanography
语种	英语
WOS记录号	WOS:000622267700001
资助机构	Key Deployment Project of Centre for Ocean Mega-Research of Science, Chinese academy of sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences Grant ; Key Research and Development project of Yantai
内容类型	期刊论文
源URL	[http://ir.yic.ac.cn/handle/133337/27393]
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烟台海岸带研究所_海岸带信息集成与综合管理实验室
通讯作者	Xing, Qianguo
作者单位	1.Chinese Acad Sci, Yantai Inst Coastal Zone Res YIC, CAS Key Lab Coastal Environm Proc & Ecol Remediat, Yantai 264003, Shandong, Peoples R China 2.YICCAS, Shandong Key Lab Coastal Environm Proc, Yantai 264003, Shandong, Peoples R China 3.Chinese Acad Sci, Ctr Ocean Megasci, Qingdao, Peoples R China
推荐引用方式 GB/T 7714	Zheng, Xiangyang,Zhang, Hua,Li, Yanfang,et al. The features and mechanisms of the North Shandong Coastal Current: a case study in 2014[J]. JOURNAL OF OCEANOGRAPHY,2021:16.
APA	Zheng, Xiangyang,Zhang, Hua,Li, Yanfang,Zou, Tao,Liu, Xin,&Xing, Qianguo.(2021).The features and mechanisms of the North Shandong Coastal Current: a case study in 2014.JOURNAL OF OCEANOGRAPHY,16.
MLA	Zheng, Xiangyang,et al."The features and mechanisms of the North Shandong Coastal Current: a case study in 2014".JOURNAL OF OCEANOGRAPHY (2021):16.