| 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
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| 2016-08-28 | |
| 发表期刊 | GEOPHYSICAL RESEARCH LETTERS
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| 卷号 | 43期号:16页码:8590-8599 |
| 文章类型 | Article |
| 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. |
| 关键词 | South China Sea Deep Current Anisotropy Of Magnetic Susceptibility Heinrich 1 Atlantic-pacific Seesaw |
| DOI | 10.1002/2016GL070342 |
| 收录类别 | SCI |
| 语种 | 英语 |
| WOS记录号 | WOS:000384443800031 |
| 引用统计 | |
| 文献类型 | 期刊论文 |
| 版本 | 出版稿 |
| 条目标识符 | http://ir.qdio.ac.cn/handle/337002/136190 |
| 专题 | 海洋地质与环境重点实验室 |
| 作者单位 | 1.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 |
| 第一作者单位 | 中国科学院海洋研究所 |
| 推荐引用方式 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. |
| 条目包含的文件 | ||||||
| 文件名称/大小 | 文献类型 | 版本类型 | 开放类型 | 使用许可 | ||
| Deepwater circulatio（1307KB） | 期刊论文 | 出版稿 | 限制开放 | CC BY-NC-SA | 浏览 | |
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