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 | |
Gorbarenko, Sergey A.1; Shi, Xuefa2,3; Malakhova, Galina Yu.4; Bosin, Aleksandr A.1; Zou, Jianjun2,3; Liu, Yanguang2,3; Chen, Min-Te5 | |
刊名 | CLIMATE OF THE PAST |
2017-08-30 | |
卷号 | 13期号:8页码:1063-1080 |
ISSN号 | 1814-9324 |
DOI | 10.5194/cp-13-1063-2017 |
英文摘要 | High-resolution reconstructions based on productivity proxies and magnetic properties of core LV63-412 (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 C-14 dating and by projections of AMS C-14 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), Bolling-Allerod (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 delta O-18 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 LGMHE1. During the B/A warming and resumption of the At-lantic 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. |
资助项目 | [16-05-00127] |
WOS关键词 | INTERMEDIATE-WATER VENTILATION ; RADIOCARBON AGE CALIBRATION ; BERING-SEA ; ICE-CORE ; HIGH-RESOLUTION ; OKHOTSK SEA ; ENVIRONMENTAL-CHANGES ; SCALE VARIABILITY ; BOTTOM SEDIMENTS ; RECORDS |
WOS研究方向 | Geology ; Meteorology & Atmospheric Sciences |
语种 | 英语 |
出版者 | COPERNICUS GESELLSCHAFT MBH |
WOS记录号 | WOS:000408642400001 |
内容类型 | 期刊论文 |
源URL | [http://ir.fio.com.cn:8080/handle/2SI8HI0U/25720] |
专题 | 自然资源部第一海洋研究所 |
通讯作者 | Gorbarenko, Sergey A. |
作者单位 | 1.VI Ilichev Pacific Oceanol Inst, Vladivostok, Russia 2.SOA, Inst Oceanog 1, Key Lab Marine Sedimentol & Environm Geol, Qingdao, Peoples R China 3.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao, Peoples R China 4.North East Interdisciplinary Sci Res Inst FEB RAS, Magadan, Russia 5.Natl Taiwan Ocean Univ, Keelung, Taiwan |
推荐引用方式 GB/T 7714 | Gorbarenko, Sergey A.,Shi, Xuefa,Malakhova, Galina Yu.,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,2017,13(8):1063-1080. |
APA | Gorbarenko, Sergey A..,Shi, Xuefa.,Malakhova, Galina Yu..,Bosin, Aleksandr A..,Zou, Jianjun.,...&Chen, Min-Te.(2017).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.CLIMATE OF THE PAST,13(8),1063-1080. |
MLA | Gorbarenko, Sergey A.,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".CLIMATE OF THE PAST 13.8(2017):1063-1080. |
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