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East Asian summer monsoon precipitation variability since the last deglaciation

文献类型:期刊论文

作者Chen, Fahu1; Xu, Qinghai2; Chen, Jianhui1; Birks, H. John B.3,4,5; Liu, Jianbao1; Zhang, Shengrui2; Jin, Liya1; An, Chengbang1; Telford, Richard J.3,4; Cao, Xianyong2
刊名SCIENTIFIC REPORTS
出版日期2015-06-18
卷号5
DOI10.1038/srep11186
文献子类Article
英文摘要The lack of a precisely-dated, unequivocal climate proxy from northern China, where precipitation variability is traditionally considered as an East Asian summer monsoon (EASM) indicator, impedes our understanding of the behaviour and dynamics of the EASM. Here we present a well-dated, pollen-based, similar to 20-yr-resolution quantitative precipitation reconstruction (derived using a transfer function) from an alpine lake in North China, which provides for the first time a direct record of EASM evolution since 14.7 ka (ka = thousands of years before present, where the "present" is defined as the year AD 1950). Our record reveals a gradually intensifying monsoon from 14.7-7.0 ka, a maximum monsoon (30% higher precipitation than present) from similar to 7.8-5.3 ka, and a rapid decline since similar to 3.3 ka. These insolation-driven EASM trends were punctuated by two millennial-scale weakening events which occurred synchronously to the cold Younger Dryas and at similar to 9.5-8.5 ka, and by two centennial-scale intervals of enhanced (weakened) monsoon during the Medieval Warm Period (Little Ice Age). Our precipitation reconstruction, consistent with temperature changes but quite different from the prevailing view of EASM evolution, points to strong internal feedback processes driving the EASM, and may aid our understanding of future monsoon behaviour under ongoing anthropogenic climate change.
WOS关键词CHINESE LOESS PLATEAU ; NORTH-ATLANTIC CLIMATE ; ICE-AGE ; OXYGEN ISOTOPES ; HIGH-RESOLUTION ; INDIAN MONSOON ; COLD EVENT ; LAKE AREA ; EL-NINO ; HOLOCENE
WOS研究方向Science & Technology - Other Topics
语种英语
WOS记录号WOS:000356527000001
资助机构National Natural Science Foundation of China(41130102) ; National Natural Science Foundation of China(41130102) ; Chinese 111 Project(B06026) ; Chinese 111 Project(B06026) ; MOE SRFDP Project(20120211130001) ; MOE SRFDP Project(20120211130001) ; National Basic Research Program of China(2010CB950202) ; National Basic Research Program of China(2010CB950202) ; National Natural Science Foundation of China(41130102) ; National Natural Science Foundation of China(41130102) ; Chinese 111 Project(B06026) ; Chinese 111 Project(B06026) ; MOE SRFDP Project(20120211130001) ; MOE SRFDP Project(20120211130001) ; National Basic Research Program of China(2010CB950202) ; National Basic Research Program of China(2010CB950202)
源URL[http://ir.iggcas.ac.cn/handle/132A11/62360]  
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
作者单位1.Lanzhou Univ, MOE Key Lab Western Chinas Environm Syst, Lanzhou 730000, Peoples R China
2.Hebei Normal Univ, Coll Resources & Environm, Inst Nihewan Archaeol Res, Shijiazhuang 050024, Peoples R China
3.Univ Bergen, Dept Biol, N-5020 Bergen, Norway
4.Univ Bergen, Bjerknes Ctr Climate Res, N-5020 Bergen, Norway
5.UCL, Environm Change Res Ctr, London WC1E 6BT, England
6.Univ Oxford, Sch Geog & Environm, Oxford OX1 3QY, England
7.Xiamen Univ, State Key Lab Marine Environm Sci, Xiamen 361005, Peoples R China
8.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China
9.Sun Yat Sen Univ, Dept Earth Sci, Guangzhou 510275, Guangdong, Peoples R China
10.Univ Liverpool, Dept Geog & Planning, Liverpool L69 3BX, Merseyside, England
推荐引用方式
GB/T 7714
Chen, Fahu,Xu, Qinghai,Chen, Jianhui,et al. East Asian summer monsoon precipitation variability since the last deglaciation[J]. SCIENTIFIC REPORTS,2015,5.
APA Chen, Fahu.,Xu, Qinghai.,Chen, Jianhui.,Birks, H. John B..,Liu, Jianbao.,...&Rao, Zhiguo.(2015).East Asian summer monsoon precipitation variability since the last deglaciation.SCIENTIFIC REPORTS,5.
MLA Chen, Fahu,et al."East Asian summer monsoon precipitation variability since the last deglaciation".SCIENTIFIC REPORTS 5(2015).

入库方式: OAI收割

来源:地质与地球物理研究所

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