中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Potential causes of megapluvials in the Yangtze-Huaihe River valley over the last millennium

文献类型:期刊论文

作者Bai, Mengxin; Zheng, Jingyun1,5; Zhang, Liang1,5; Xing, Pei; Wu, Maowei1; Hao, Zhixin1,4,5; Du, Wupeng3
刊名GLOBAL AND PLANETARY CHANGE
出版日期2023-12-01
卷号231页码:104292
关键词Yangtze -Huaihe River valley Megapluvial Last millennium Air -land interaction Teleconnection
DOI10.1016/j.gloplacha.2023.104292
产权排序2
文献子类Article
英文摘要The potential causes of megapluvials over Yangtze-Huaihe River valley (YHRV) during the last millennium were investigated using the Community Earth System Model-Last Millennium Ensemble (CESM-LME) simulation data and multiple proxy data (i.e., reconstruction and paleoclimate assimilation data). Herein, we first depicted the spatial hydroclimatic pattern over the Northern Hemisphere when megapluvials occurred in the YHRV during the last millennium. The proxy and simulation data both showed that megapluvials in YHRV were accompanied by extensive decadal drought in western Asia and northwestern India, also located in mid to low latitudes. Then, by diagnosing the dynamic processes, we found that the baroclinic structure over western Asia and northwestern India caused anomalous geopotential heights, and hence triggered the negative phase of the Circumglobal Teleconnection (CGT). The eastwards wave train at mid-latitudes disturbed by the CGT mode, triggered lower-level northerlies and upper-level southerlies over the northern part of the YHRV and, as a consequence, led to anomalous strong convection near the YHRV. Together with abundant water vapour from the Pacific Northwest, there was a synergistic effect on megapluvial events over the YHRV. Finally, we analysed the linkage of surface temperature in western Asia and northwestern India and megapluvials in the YHRV. Land surface heating over western Asia and northwestern India may largely stimulate the formation of a negative CGT mode through local feedback of air-land interactions and, as a result, affect precipitation anomalies downstream, such as in the YHRV. It is therefore necessary to consider anomalous high surface temperatures in western Asia and northwestern India as important predictors for interdecadal severe floods in the YHRV.
WOS关键词CIRCUMGLOBAL TELECONNECTION ; GRAIN PRODUCTION ; EASTERN CHINA ; PRECIPITATION ; CLIMATE ; VARIABILITY ; CONSUMPTION ; IMPACTS ; MONSOON ; FLOOD
WOS研究方向Physical Geography ; Geology
出版者ELSEVIER
WOS记录号WOS:001114396500001
源URL[http://ir.igsnrr.ac.cn/handle/311030/200981]  
专题陆地表层格局与模拟院重点实验室_外文论文
作者单位1.Beijing Municipal Climate Ctr, Beijing Meteorol Serv, Beijing 100089, Peoples R China
2.44 Zizhuyuan Rd, Beijing, Peoples R China
3.11A Datun Rd, Beijing, Peoples R China
4.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
5.Chinese Acad Sci, Key Lab Land Surface Pattern & Simulat, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China
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GB/T 7714
Bai, Mengxin,Zheng, Jingyun,Zhang, Liang,et al. Potential causes of megapluvials in the Yangtze-Huaihe River valley over the last millennium[J]. GLOBAL AND PLANETARY CHANGE,2023,231:104292.
APA Bai, Mengxin.,Zheng, Jingyun.,Zhang, Liang.,Xing, Pei.,Wu, Maowei.,...&Du, Wupeng.(2023).Potential causes of megapluvials in the Yangtze-Huaihe River valley over the last millennium.GLOBAL AND PLANETARY CHANGE,231,104292.
MLA Bai, Mengxin,et al."Potential causes of megapluvials in the Yangtze-Huaihe River valley over the last millennium".GLOBAL AND PLANETARY CHANGE 231(2023):104292.

入库方式: OAI收割

来源:地理科学与资源研究所

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