Tropical volcanism enhanced the East Asian summer monsoon during the last millennium.


Journal

Nature communications
ISSN: 2041-1723
Titre abrégé: Nat Commun
Pays: England
ID NLM: 101528555

Informations de publication

Date de publication:
14 06 2022
Historique:
received: 21 11 2021
accepted: 20 05 2022
entrez: 14 6 2022
pubmed: 15 6 2022
medline: 18 6 2022
Statut: epublish

Résumé

Extreme East Asian summer monsoon (EASM) rainfall frequently induces floods that threaten millions of people, and has been generally attributed to internal climate variability. In contrast to the hydrological weakening theory of volcanic eruptions, here we present convergent empirical and modeling evidence for significant intensification of EASM rainfall in response to strong tropical volcanic eruptions. Our multi-proxy analyses show a significantly increased EASM in the first summer after tropical eruptions from 1470 AD to the present, and the more frequent occurrence of El Niños in the first boreal winter after eruptions is necessary for the enhanced EASM. Model simulation ensembles show that a volcano-induced El Niño and the associated stronger than non-volcanic El Niño warm pool air-sea interaction intensify EASM precipitation, overwhelming volcanic-induced moisture deficiency. This work sheds light on the intertwined relationship between external forcing and internal climate variability and potential flood disasters resulting from tropical volcanic eruptions.

Identifiants

pubmed: 35701455
doi: 10.1038/s41467-022-31108-7
pii: 10.1038/s41467-022-31108-7
pmc: PMC9197930
doi:

Types de publication

Journal Article Research Support, Non-U.S. Gov't Research Support, U.S. Gov't, Non-P.H.S.

Langues

eng

Sous-ensembles de citation

IM

Pagination

3429

Informations de copyright

© 2022. The Author(s).

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Auteurs

Fei Liu (F)

School of Atmospheric Sciences Sun Yat-Sen University, Key Laboratory of Tropical Atmosphere-Ocean System Ministry of Education, and Southern Marine Science and Engineering Guangdong Laboratory, Zhuhai, 519082, China.

Chaochao Gao (C)

College of Environmental and Resource Sciences, Zhejiang University, Hangzhou, 310058, China. gaocc@zju.edu.cn.

Jing Chai (J)

Plateau Atmosphere and Environment Key Laboratory of Sichuan Province, School of Atmospheric Sciences, Chengdu University of Information Technology, Chengdu, 610225, China.
State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, 100029, China.

Alan Robock (A)

Department of Environmental Sciences, Rutgers University, New Brunswick, NJ, 08901, USA.

Bin Wang (B)

Department of Atmospheric Sciences and International Pacific Research Center, University of Hawaii at Manoa, Honolulu, HI, 96822, USA. wangbin@hawaii.edu.
Earth System Modeling Center and Climate Dynamics Research Center, Nanjing University of Information Science & Technology, Nanjing, 210044, China. wangbin@hawaii.edu.

Jinbao Li (J)

Department of Geography, University of Hong Kong, Hong Kong SAR, China.

Xu Zhang (X)

Alpine Paleoecology and Human Adaptation Group (ALPHA), State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment (TPESRE), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China.

Gang Huang (G)

State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, 100029, China.

Wenjie Dong (W)

School of Atmospheric Sciences Sun Yat-Sen University, Key Laboratory of Tropical Atmosphere-Ocean System Ministry of Education, and Southern Marine Science and Engineering Guangdong Laboratory, Zhuhai, 519082, China.

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