Intrusion of the Kuroshio Subsurface Water in the southern East China Sea and its variation in 2014 and 2015 traced by dissolved inorganic iodine species
Zhou, Peng1,2,3; Song, Xiuxian1,2,3; Yuan, Yongquan1,2; Wang, Wentao1,2; Chi, Lianbao1,2,3; Cao, Xihua1,2; Yu, Zhiming1,2,3
刊名PROGRESS IN OCEANOGRAPHY
2018-07-01
卷号165页码:287-298
关键词Kuroshio Subsurface Water Dissolved inorganic iodine East China Sea continental shelf Ocean circulation Interannual variability Ecological effect
ISSN号0079-6611
DOI10.1016/j.pocean.2018.06.011
通讯作者Song, Xiuxian(songxx@qdio.ac.cn)
英文摘要The circulation systems and ecological environment of the East China Sea (ECS) are greatly influenced by the Kuroshio. The nutrient-rich Kuroshio Subsurface Water (KSSW) has been subject to considerable research attention, but the intrusion pathway, extent and variation of the KSSW over the entire southern ECS shelf are still debated. In June 2015, the dissolved inorganic iodine species (DIIS) were determined, and hydrographic data were collected and analyzed in the southern ECS. Analysis of the collected data suggests that the KSSW mainly intrudes onto the ECS shelf from northeast of Taiwan and bifurcates into a nearshore branch and an offshore branch. The nearshore branch ultimately appears in the subsurface layer within the 50-m isobath off the Zhejiang coast, north of 30 degrees N, and the offshore branch flows along the 100-m isobath and covers the area outside the 80-m isobath. Another KSSW intrusion along the shelf edge is located at similar to 28 degrees N. This additional KSSW intrusion is weaker, and the offshore area in the southern ECS is mainly influenced by the KSSW intrusion northeast of Taiwan. Compared with the KSSW intrusion on the ECS continental shelf (depth < 100 m) in May 2014, the KSSW intrusion northeast of Taiwan in June 2015 was shifted seaward, had a greater geographical reach and intruded farther north off the Zhejiang coast. The KSSW intrusion in the nearshore area off the Zhejiang coast may promote a decrease in dissolved oxygen (DO) in the bottom water as well as the growth of phytoplankton in the upper water. The expansion of the range of the KSSW intrusion northward in 2015 led to the movement of the low-DO, high-chlorophyll area farther north in 2015 relative to its position in 2014 and may have contributed to the variations in hypoxia and algal blooms.
资助项目Strategic Priority Research Program of the Chinese Academy of Sciences[XDA11020601] ; Sino-Australian Centre for Healthy Coasts of National Key Research and Development Plan[2016YFE0101500] ; Aoshan Talent Cultivation Program - Qingdao National Laboratory for Marine Science and Technology[2017ASTCP-OS16] ; NSFC-Shandong Joint Fund for Marine Science Research Centers[U1606404]
WOS研究方向Oceanography
语种英语
出版者PERGAMON-ELSEVIER SCIENCE LTD
WOS记录号WOS:000441489600020
内容类型期刊论文
源URL[http://ir.qdio.ac.cn/handle/337002/157557]  
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Song, Xiuxian
作者单位1.Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Shandong, Peoples R China
2.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao 266237, Shandong, Peoples R China
3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
推荐引用方式
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Zhou, Peng,Song, Xiuxian,Yuan, Yongquan,et al. Intrusion of the Kuroshio Subsurface Water in the southern East China Sea and its variation in 2014 and 2015 traced by dissolved inorganic iodine species[J]. PROGRESS IN OCEANOGRAPHY,2018,165:287-298.
APA Zhou, Peng.,Song, Xiuxian.,Yuan, Yongquan.,Wang, Wentao.,Chi, Lianbao.,...&Yu, Zhiming.(2018).Intrusion of the Kuroshio Subsurface Water in the southern East China Sea and its variation in 2014 and 2015 traced by dissolved inorganic iodine species.PROGRESS IN OCEANOGRAPHY,165,287-298.
MLA Zhou, Peng,et al."Intrusion of the Kuroshio Subsurface Water in the southern East China Sea and its variation in 2014 and 2015 traced by dissolved inorganic iodine species".PROGRESS IN OCEANOGRAPHY 165(2018):287-298.
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