globalchange  > 气候变化与战略
DOI: 10.5194/cp-13-1063-2017
Scopus记录号: 2-s2.0-85028586315
论文题名:
Centennial to millennial climate variability in the far northwestern Pacific (off Kamchatka) and its linkage to the East Asian monsoon and North Atlantic from the Last Glacial Maximum to the early Holocene
作者: Gorbarenko S.A.; Shi X.; Yu Malakhova G.; Bosin A.; Zou J.; Liu Y.; Chen M.-T.
刊名: Climate of the Past
ISSN: 18149324
出版年: 2017
卷: 13, 期:8
起始页码: 1063
结束页码: 1080
语种: 英语
英文摘要: High-resolution reconstructions based on productivity proxies and magnetic properties of core LV63-41-2 (off Kamchatka) reveal prevailing centennial productivity/climate variability in the northwestern (NW) Pacific from the Last Glacial Maximum (LGM) to the early Holocene (EH). The age model of the core is established by AMS 14C dating and by projections of AMS 14C data of the nearby core SO-201-12KL through correlation of the productivity proxies and relative paleomagnetic intensity. The resulting sequence of centennial productivity increases/climate warming events in the NW Pacific occurred synchronously with the East Asian summer monsoon (EASM) sub-interstadials during the LGM (four events), Heinrich Event 1 (HE1) (four events), Bølling-Allerød (B/A) warming (four events), and over the EH (four events). Remarkable similarity of the sequence of the NW Pacific increased-productivity events with the EASM sub-interstadials over the LGM-HE1 implies that the Siberian High is a strong and common driver. The comparison with the Î18O record from Antarctica suggests that another mechanism associated with the temperature gradient in the Southern Hemisphere may also be responsible for the EASM/NW Pacific centennial events over the LGM-HE1. During the B/A warming and resumption of the Atlantic Meridional Overturning Circulation (AMOC), clear synchronicity between the NW Pacific, EASM and Greenland sub-interstadials was mainly controlled by changes in the atmospheric circulation. During the EH the linkages between solar forcing, ocean circulation, and climate changes likely control the synchronicity of abrupt climate changes in the NW Pacific and North Atlantic. The sequence of centennial events recorded in this study is a persistent regional feature during the LGM-EH, which may serve as a template in high-resolution paleoceanography and sediment stratigraphy in the NW Pacific. © 2017 Author(s).
Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/48889
Appears in Collections:气候变化与战略

Files in This Item:

There are no files associated with this item.


Recommended Citation:
Gorbarenko S.A.,Shi X.,Yu Malakhova G.,et al. Centennial to millennial climate variability in the far northwestern Pacific (off Kamchatka) and its linkage to the East Asian monsoon and North Atlantic from the Last Glacial Maximum to the early Holocene[J]. Climate of the Past,2017-01-01,13(8)
Service
Recommend this item
Sava as my favorate item
Show this item's statistics
Export Endnote File
Google Scholar
Similar articles in Google Scholar
[Gorbarenko S.A.]'s Articles
[Shi X.]'s Articles
[Yu Malakhova G.]'s Articles
百度学术
Similar articles in Baidu Scholar
[Gorbarenko S.A.]'s Articles
[Shi X.]'s Articles
[Yu Malakhova G.]'s Articles
CSDL cross search
Similar articles in CSDL Cross Search
[Gorbarenko S.A.]‘s Articles
[Shi X.]‘s Articles
[Yu Malakhova G.]‘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.