IOCAS-IR  > 海洋地质与环境重点实验室
Deepwater circulation variation in the South China Sea since the Last Glacial Maximum
Zheng, Xufeng1; Kao, ShuhJi2; Chen, Zhong1; Menviel, Laurie3; Chen, Han4; Du, Yan5; Wan, Shiming6; Yan, Hong7; Liu, Zhonghui8; Zheng, Liwei2; Wang, Shuhong1; Li, Dawei2; Zhang, Xu9
2016-08-28
Source PublicationGEOPHYSICAL RESEARCH LETTERS
Volume43Issue:16Pages:8590-8599
SubtypeArticle
AbstractDeepwater circulation plays a central role in global climate. Compared with the Atlantic, the Pacific deepwater circulation's history remains unclear. The Luzon overflow, a branch of the North Pacific deep water, determines the ventilation rate of the South China Sea (SCS) basin. Sedimentary magnetic properties in the SCS reflect millennial-scale fluctuations in deep current intensity and orientation. The data suggest a slightly stronger current at the Last Glacial Maximum compared to the Holocene. But, the most striking increase in deep current occurred during Heinrich stadial 1 (H1) and to a lesser extent during the Younger Dryas (YD). Results of a transient deglacial experiment suggest that the northeastern current strengthening at the entrance of the SCS during H1 and the YD, times of weak North Atlantic Deep Water formation, could be linked to enhanced formation of North Pacific Deep Water.
KeywordSouth China Sea Deep Current Anisotropy Of Magnetic Susceptibility Heinrich 1 Atlantic-pacific Seesaw
DOI10.1002/2016GL070342
Indexed BySCI
Language英语
WOS IDWOS:000384443800031
Citation statistics
Cited Times:9[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Version出版稿
Identifierhttp://ir.qdio.ac.cn/handle/337002/136190
Collection海洋地质与环境重点实验室
Affiliation1.Chinese Acad Sci, South China Sea Inst Oceanol, Key Lab Marginal Sea Geol, Guangzhou, Guangdong, Peoples R China
2.Xiamen Univ, State Key Lab Marine Environm Sci, Xiamen, Peoples R China
3.Univ New South Wales, Climate Change Res Ctr, ARC Ctr Excellence Climate Syst Sci, Sydney, NSW, Australia
4.State Ocean Adm, Isl Res Ctr, Fuzhou, Peoples R China
5.Chinese Acad Sci, South China Sea Inst Oceanol, State Key Lab Trop Oceanog, Guangzhou, Guangdong, Peoples R China
6.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao, Peoples R China
7.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian, Peoples R China
8.Univ Hong Kong, Dept Earth Sci, Hong Kong, Hong Kong, Peoples R China
9.Helmholtz Zentrum Polar & Meeresforsch, Alfred Wegener Inst, Bremerhaven, Germany
First Author AffilicationInstitute of Oceanology, Chinese Academy of Sciences
Recommended Citation
GB/T 7714
Zheng, Xufeng,Kao, ShuhJi,Chen, Zhong,et al. Deepwater circulation variation in the South China Sea since the Last Glacial Maximum[J]. GEOPHYSICAL RESEARCH LETTERS,2016,43(16):8590-8599.
APA Zheng, Xufeng.,Kao, ShuhJi.,Chen, Zhong.,Menviel, Laurie.,Chen, Han.,...&Zhang, Xu.(2016).Deepwater circulation variation in the South China Sea since the Last Glacial Maximum.GEOPHYSICAL RESEARCH LETTERS,43(16),8590-8599.
MLA Zheng, Xufeng,et al."Deepwater circulation variation in the South China Sea since the Last Glacial Maximum".GEOPHYSICAL RESEARCH LETTERS 43.16(2016):8590-8599.
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