globalchange  > 科学计划与规划
DOI: 10.1002/2016GL070342
论文题名:
Deepwater circulation variation in the South China Sea since the Last Glacial Maximum
作者: Zheng X.; Kao S.; Chen Z.; Menviel L.; Chen H.; Du Y.; Wan S.; Yan H.; Liu Z.; Zheng L.; Wang S.; Li D.; Zhang X.
刊名: Geophysical Research Letters
ISSN: 0094-8722
EISSN: 1944-8453
出版年: 2016
卷: 43, 期:16
起始页码: 8590
结束页码: 8599
语种: 英语
英文关键词: anisotropy of magnetic susceptibility ; Atlantic-Pacific seesaw ; deep current ; Heinrich 1 ; South China Sea
Scopus关键词: Magnetic anisotropy ; Magnetic susceptibility ; Anisotropy of magnetic susceptibility ; Atlantic-Pacific seesaw ; Deep currents ; Heinrich 1 ; South China sea ; Glacial geology
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. ©2016. American Geophysical Union. All Rights Reserved.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84982295135&doi=10.1002%2f2016GL070342&partnerID=40&md5=ff1daf55a22b06fb287d00cd1b9ffa73
Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/9685
Appears in Collections:科学计划与规划
气候变化与战略

Files in This Item:

There are no files associated with this item.


作者单位: Key Laboratory of Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, China

Recommended Citation:
Zheng X.,Kao S.,Chen Z.,et al. Deepwater circulation variation in the South China Sea since the Last Glacial Maximum[J]. Geophysical Research Letters,2016-01-01,43(16).
Service
Recommend this item
Sava as my favorate item
Show this item's statistics
Export Endnote File
Google Scholar
Similar articles in Google Scholar
[Zheng X.]'s Articles
[Kao S.]'s Articles
[Chen Z.]'s Articles
百度学术
Similar articles in Baidu Scholar
[Zheng X.]'s Articles
[Kao S.]'s Articles
[Chen Z.]'s Articles
CSDL cross search
Similar articles in CSDL Cross Search
[Zheng X.]‘s Articles
[Kao S.]‘s Articles
[Chen Z.]‘s Articles
Related Copyright Policies
Null
收藏/分享
所有评论 (0)
暂无评论
 

Items in IR are protected by copyright, with all rights reserved, unless otherwise indicated.