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  4. 中国科学院新生代地质与环境重点实验室
Asynchronous 500-year summer monsoon rainfall cycles between Northeast and Central China during the Holocene

文献类型：期刊论文

作者Xu, Deke5,6; Lu, Houyuan4,5,6; Chu, Guoqiang3,6; Shen, Caiming2; Li, Fengjiang1,6; Wu, Jing1,6; Wang, Luo1,6; Li, Hao4,6; Yu, Yinghao4,6; Jin, Yingyu4,6
刊名GLOBAL AND PLANETARY CHANGE
出版日期2020-12-01
卷号195页码:8
关键词Pollen Speleothem East Asian monsoon La Nina El Nino Land-ocean interactions
ISSN号0921-8181
DOI10.1016/j.gloplacha.2020.103324
英文摘要Although the summer monsoon is the dominant source of precipitation in the East Asian monsoon region (EAMR), there is long-standing uncertainty about the spatial and temporal variability of precipitation on the centennial time scale. In this study we analyzed two well-dated, high-resolution, published paleoclimatic records in order to determine the variability of precipitation in the EAMR during the Holocene. One record is a decadal-resolution pollen record from an annually-laminated Maar lake in Northeast (NE) China, and the other is a UeTh dated, multi-decadal-resolution speleothem record from Central China. Advanced time-series analysis of the two records provides unambiguous evidence for asynchronous summer monsoon rainfall variability on centennial to millennial time scales in the EAMR. The pollen and speleothem records indicate long-term and similar to 500-yr quasi periodic changes in humid/dry climatic shifts against the background of an insolation-forced climatic trend throughout the past 8580 years. Phases of wetter climate (during similar to 7000-5500 cal yr BP) and drier climate (during similar to 1400-300 cal yr BP) in NE China are closely related to different climatic phases in Central China. However, the similar to 500-yr cyclic rainfall changes in Central China lag those in NE China by several decades to almost two centuries. During the similar to 500-yr periodic changes in the monsoon, a climatic pattern encapsulated as "Northern drought, southern flooding" prevailed during an El Nino-like phase, whereas the opposite pattern "Southern drought, northern flooding" occurred during a La Nina-like phase. The asynchronous pattern of similar to 500yr climatic cyclicity between the northern and southern EAMR may have been caused by the El Nino-Southern Oscillation, linked to low-latitude oceanic and atmospheric interactions.
WOS关键词EMPIRICAL MODE DECOMPOSITION ; CLIMATE-CHANGE ; SOUTH CHINA ; EAST ; OCEAN ; PRECIPITATION ; VEGETATION ; SEDIMENTS ; DROUGHT ; RECORDS
资助项目National Key Research and Development Program of China[2017YFA0603403] ; Strategic Priority Research Program of Chinese Academy of Sciences[XDA2007010103] ; National Natural Science Foundation of China[41471166] ; National Natural Science Foundation of China[42071103] ; National Natural Science Foundation of China[41830322] ; National Natural Science Foundation of China[41888101] ; National Natural Science Foundation of China[41372191] ; Yunnan Project for the Introduction of Advanced Talents[2013HA024]
WOS研究方向Physical Geography ; Geology
语种英语
WOS记录号WOS:000592360800005
出版者ELSEVIER
资助机构National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Yunnan Project for the Introduction of Advanced Talents ; Yunnan Project for the Introduction of Advanced Talents ; Yunnan Project for the Introduction of Advanced Talents ; Yunnan Project for the Introduction of Advanced Talents ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Yunnan Project for the Introduction of Advanced Talents ; Yunnan Project for the Introduction of Advanced Talents ; Yunnan Project for the Introduction of Advanced Talents ; Yunnan Project for the Introduction of Advanced Talents ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Yunnan Project for the Introduction of Advanced Talents ; Yunnan Project for the Introduction of Advanced Talents ; Yunnan Project for the Introduction of Advanced Talents ; Yunnan Project for the Introduction of Advanced Talents ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Yunnan Project for the Introduction of Advanced Talents ; Yunnan Project for the Introduction of Advanced Talents ; Yunnan Project for the Introduction of Advanced Talents ; Yunnan Project for the Introduction of Advanced Talents
源URL[http://ir.iggcas.ac.cn/handle/132A11/98734]  
专题地质与地球物理研究所_中国科学院新生代地质与环境重点实验室
通讯作者Xu, Deke; Lu, Houyuan
作者单位1.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing 100029, Peoples R China
2.Yunnan Normal Univ, Coll Tourism & Geog Sci, Yunnan Key Lab Plateau Geog Proc & Environm Chang, Kunming 650500, Yunnan, Peoples R China
3.CAS Ctr Excellence Life & Paleoenvironm, Beijing 100044, Peoples R China
4.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
5.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
6.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714		 Xu, Deke,Lu, Houyuan,Chu, Guoqiang,et al. Asynchronous 500-year summer monsoon rainfall cycles between Northeast and Central China during the Holocene[J]. GLOBAL AND PLANETARY CHANGE,2020,195:8.
APA Xu, Deke.,Lu, Houyuan.,Chu, Guoqiang.,Shen, Caiming.,Li, Fengjiang.,...&Wu, Naiqin.(2020).Asynchronous 500-year summer monsoon rainfall cycles between Northeast and Central China during the Holocene.GLOBAL AND PLANETARY CHANGE,195,8.
MLA Xu, Deke,et al."Asynchronous 500-year summer monsoon rainfall cycles between Northeast and Central China during the Holocene".GLOBAL AND PLANETARY CHANGE 195(2020):8.

入库方式： OAI收割

来源：地质与地球物理研究所

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