Deepwater circulation variation in the South China Sea since the Last Glacial Maximum
文献类型：期刊论文
| 作者 | Zhang, Xu7; Liu, Zhonghui8; Zheng, Liwei3; Wang, Shuhong6; Li, Dawei3; Zheng, Xufeng6; Kao, ShuhJi3; Chen, Zhong6; Menviel, Laurie2; Chen, Han1 |
| 刊名 | GEOPHYSICAL RESEARCH LETTERS
 |
| 出版日期 | 2016-08-28 |
| 卷号 | 43期号:16页码:8590-8599 |
| 关键词 | South China Sea Deep Current Anisotropy Of Magnetic Susceptibility Heinrich 1 Atlantic-pacific Seesaw |
| DOI | 10.1002/2016GL070342 |
| 文献子类 | Article |
| 英文摘要 | Deepwater 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. |
| WOS关键词 | MERIDIONAL OVERTURNING CIRCULATION ; ATLANTIC-PACIFIC SEESAW ; NORTH PACIFIC ; BOTTOM-WATER ; MAGNETIC-SUSCEPTIBILITY ; OCEAN CIRCULATION ; DEGLACIATION ; CLIMATE ; SEDIMENTS ; ANISOTROPY |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000384443800031 |
| 源URL | [http://ir.ieecas.cn/handle/361006/5649]  |
| 专题 | 地球环境研究所_古环境研究室 |
| 作者单位 | 1.State Ocean Adm, Isl Res Ctr, Fuzhou, Peoples R China 2.Univ New South Wales, Climate Change Res Ctr, ARC Ctr Excellence Climate Syst Sci, Sydney, NSW, Australia 3.Xiamen Univ, State Key Lab Marine Environm Sci, Xiamen, Peoples R China 4.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao, 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, South China Sea Inst Oceanol, Key Lab Marginal Sea Geol, Guangzhou, Guangdong, Peoples R China 7.Helmholtz Zentrum Polar & Meeresforsch, Alfred Wegener Inst, Bremerhaven, Germany 8.Univ Hong Kong, Dept Earth Sci, Hong Kong, Hong Kong, Peoples R China 9.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian, Peoples R China |
| 推荐引用方式 GB/T 7714 | Zhang, Xu,Liu, Zhonghui,Zheng, Liwei,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 | Zhang, Xu.,Liu, Zhonghui.,Zheng, Liwei.,Wang, Shuhong.,Li, Dawei.,...&Yan, Hong.(2016).Deepwater circulation variation in the South China Sea since the Last Glacial Maximum.GEOPHYSICAL RESEARCH LETTERS,43(16),8590-8599. |
| MLA | Zhang, Xu,et al."Deepwater circulation variation in the South China Sea since the Last Glacial Maximum".GEOPHYSICAL RESEARCH LETTERS 43.16(2016):8590-8599. |
入库方式： OAI收割
来源：地球环境研究所
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