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Coupled Pacific Rim megadroughts contributed to the fall of the Ming Dynasty's capital in 1644 CE

文献类型：期刊论文

作者Chen, Feng4,5; Wang, Tao6,7; Zhao, Xiaoen4,5; Esper, Jan8,9; Ljungqvist, Fredrik Charpentier10,11,12; Buntgen, Ulf9,13,14; Linderholm, Hans W.15; Meko, David16; Xu, Hongna17; Yue, Weipeng4
刊名SCIENCE BULLETIN
出版日期2024-10-15
卷号69期号:19页码:3106-3114
关键词Paleoclimate Beijing Precipitation reconstruction Climate-society interactions Tree rings Ming Dynasty
ISSN号2095-9273
DOI10.1016/j.scib.2024.04.029
产权排序16
英文摘要Historical documents provide evidence for regional droughts preceding the political turmoil and fall of Beijing in 1644 CE, when more than 20 million people died in northern China during the late Ming famine period. However, the role climate and environmental changes may have played in this pivotal event in Chinese history remains unclear. Here, we provide tree-ring evidence of persistent megadroughts from 1576 to 1593 CE and from 1628 to 1644 CE in northern China, which coincided with exceptionally cold summers just before the fall of Beijing. Our analysis reveals that these regional hydroclimatic extremes are part of a series of megadroughts along the Pacific Rim, which not only impacted the ecology and society of monsoonal northern China, but likely also exacerbated external geopolitical and economic pressures. This finding is corroborated by last millennium reanalysis data and numerical climate model simulations revealing internally driven Pacific sea surface temperature variations and the predominance of decadal scale La Ni & ntilde;a-like conditions to be responsible for precipitation decreases over northern China, as well as extensive monsoon regions in the Americas. These teleconnection patterns provide a mechanistic explanation for reoccurring drought spells during the late Ming Dynasty and the environ- mental framework fostering the fall of Beijing in 1644 CE, and the subsequent demise of the Ming Dynasty. (c) 2024 Science China Press. Published by Elsevier B.V. and Science China Press. All rights are reserved, including those for text and data mining, AI training, and similar technologies.
WOS关键词LAST MILLENNIUM ; CLIMATIC-CHANGE ; EXTREME EVENTS ; EASTERN CHINA ; VARIABILITY ; RESPONSES ; COLLAPSE ; DROUGHTS ; EMPIRE
资助项目Basic Science Center for Tibe-tan Plateau Earth System (BSCTPES)[41988101] ; National Natural Science Foundation of China[32061123008] ; ERC[AdG 882727] ; Czech Science Foundation[23-08049S] ; Swedish Research Council (Vetenskapsradet)[2018-01272] ; Marianne and Marcus Wallenberg Foundation[MMW 2022-0114] ; Swedish Collegium for Advanced Study through the Riksbankens Jubileumsfond
WOS研究方向Science & Technology - Other Topics
语种英语
WOS记录号WOS:001368343800001
出版者ELSEVIER
资助机构Basic Science Center for Tibe-tan Plateau Earth System (BSCTPES) ; National Natural Science Foundation of China ; ERC ; Czech Science Foundation ; Swedish Research Council (Vetenskapsradet) ; Marianne and Marcus Wallenberg Foundation ; Swedish Collegium for Advanced Study through the Riksbankens Jubileumsfond
源URL[http://ir.igsnrr.ac.cn/handle/311030/211570]  
专题陆地表层格局与模拟院重点实验室_外文论文
通讯作者Chen, Feng
作者单位1.Chinese Acad Sci, Inst Tibetan Plateau Res, State Key Lab Tibetan Plateau Earth Syst, ALPHA, Beijing 100101, Peoples R China
2.Univ Chinese Acad Sci, Coll Resources & Environm, Beijing 100049, Peoples R China
3.Lanzhou Univ, MOE Key Lab Western Chinas Environm Syst, Lanzhou 730000, Peoples R China
4.Yunnan Univ, Inst Int Rivers & Ecosecur, Yunnan Key Lab Int Rivers & Transboundary Ecosecur, Kunming 650504, Peoples R China
5.Southwest United Grad Sch, Kunming 650504, Peoples R China
6.Chinese Acad Sci, Climate Change Res Ctr, Beijing 100029, Peoples R China
7.Chinese Acad Sci, Inst Atmospher Phys, Nansen Zhu Int Res Ctr, Beijing 100029, Peoples R China
8.Johannes Gutenberg Univ Mainz, Dept Geog, D-55099 Mainz, Germany
9.Czech Acad Sci, Global Change Res Inst CzechGlobe, Brno 60300, Czech Republic
10.Stockholm Univ, Dept Hist, SE-10691 Stockholm, Sweden
推荐引用方式
GB/T 7714		 Chen, Feng,Wang, Tao,Zhao, Xiaoen,et al. Coupled Pacific Rim megadroughts contributed to the fall of the Ming Dynasty's capital in 1644 CE[J]. SCIENCE BULLETIN,2024,69(19):3106-3114.
APA Chen, Feng.,Wang, Tao.,Zhao, Xiaoen.,Esper, Jan.,Ljungqvist, Fredrik Charpentier.,...&Chen, Fahu.(2024).Coupled Pacific Rim megadroughts contributed to the fall of the Ming Dynasty's capital in 1644 CE.SCIENCE BULLETIN,69(19),3106-3114.
MLA Chen, Feng,et al."Coupled Pacific Rim megadroughts contributed to the fall of the Ming Dynasty's capital in 1644 CE".SCIENCE BULLETIN 69.19(2024):3106-3114.

入库方式： OAI收割

来源：地理科学与资源研究所

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