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| Intrusion Pattern of the Offshore Kuroshio Branch Current and Its Effects on Nutrient Contributions in the East China Sea | |
Wang, Wentao1,2 ; Yu, Zhiming1,2; Song, Xiuxian1,2; Yuan, Yongquan1,2; Wu, Zaixing1,2; Zhou, Peng1,2,3; Cao, Xihua1,2
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| 2018-03-01 | |
| Source Publication | JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
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| ISSN | 2169-9275 |
| Volume | 123Issue:3Pages:2116-2128 |
| Corresponding Author | Yu, Zhiming(zyu@qdio.ac.cn) |
| Abstract | During the autumn season of 2014 (October-November), nutrient samples and nitrogen and oxygen isotope samples from the East China Sea (ECS) were collected and analyzed, and auxiliary physical parameters were determined. Distinctive high-salinity water column conditions with significant haloclines and pycnoclines similar to those observed during the spring were detected at the bottom of the ECS during the autumn. These water column conditions were attributed to the intrusion of the Kuroshio Subsurface Water (KSSW), which then separated into two currents, including the Offshore Kuroshio Branch Current (OKBC). Compared with spring, this intrusion transported higher phosphorus (P) concentrations onto the ECS continental shelf in autumn. However, according to multiple analyses, biogeochemical nitrogen processes are unable to explain the variations in the P concentrations (increase) while assuming that each distinctive water column is consistent. Identifying the water columns by their salinities and P concentrations revealed that the northern ECS water column was similar to the deep KSSW while the southern ECS water column was similar to the shallow KSSW. Therefore, we speculate that the distinctions among the seasonal variations of P-enriched water masses were attributable to the different intrusion positions of the Kuroshio. The shift of the KSSW intrusion location moved toward the northeast during the autumn relative to the spring. This shift, which was proved by the oceanic vortex data, caused the deeper KSSW water upwelled to the ECS and formed the OKBC, thereby supplying additional P during the autumn. |
| Keyword | East China Sea Kuroshio phosphate branch current intrusion nutrients cycles |
| DOI | 10.1002/2017JC013538 |
| Indexed By | SCI |
| Language | 英语 |
| Funding Project | Strategic Priority Research Program of the Chinese Academy of Sciences[XDA11020601] ; National Key Research and Development Program of China[2016YFE0101500] ; Aoshan Talent Cultivation Program[2017ASTCP-OS16] |
| WOS Research Area | Oceanography |
| WOS Subject | Oceanography |
| WOS ID | WOS:000430918500031 |
| Publisher | AMER GEOPHYSICAL UNION |
| Citation statistics | |
| Document Type | 期刊论文 |
| Identifier | http://ir.qdio.ac.cn/handle/337002/157592 |
| Collection | 海洋生态与环境科学重点实验室 |
| Corresponding Author | Yu, Zhiming |
| Affiliation | 1.Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao, Peoples R China 2.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao, Peoples R China 3.Univ Chinese Acad Sci, Beijing, Peoples R China |
| First Author Affilication | Institute of Oceanology, Chinese Academy of Sciences |
| Corresponding Author Affilication | Institute of Oceanology, Chinese Academy of Sciences |
| Recommended Citation GB/T 7714 | Wang, Wentao,Yu, Zhiming,Song, Xiuxian,et al. Intrusion Pattern of the Offshore Kuroshio Branch Current and Its Effects on Nutrient Contributions in the East China Sea[J]. JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS,2018,123(3):2116-2128. |
| APA | Wang, Wentao.,Yu, Zhiming.,Song, Xiuxian.,Yuan, Yongquan.,Wu, Zaixing.,...&Cao, Xihua.(2018).Intrusion Pattern of the Offshore Kuroshio Branch Current and Its Effects on Nutrient Contributions in the East China Sea.JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS,123(3),2116-2128. |
| MLA | Wang, Wentao,et al."Intrusion Pattern of the Offshore Kuroshio Branch Current and Its Effects on Nutrient Contributions in the East China Sea".JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS 123.3(2018):2116-2128. |
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| Intrusion Pattern of（10845KB） | 期刊论文 | 出版稿 | 开放获取 | CC BY-NC-SA | View Application Full Text | |
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