Interstadial diversity of East Asian summer monsoon linked to changes of the Northern Westerlies
Dong, Xiyu ORCID: https://orcid.org/0000-0002-7611-0244; Zhang, Xu
ORCID: https://orcid.org/0000-0003-1833-9689; Zhang, Haiwei
ORCID: https://orcid.org/0000-0002-0855-1283; Zhang, Yuao; Rasmussen, Sune O.
ORCID: https://orcid.org/0000-0002-4177-3611; Zhang, Rui
ORCID: https://orcid.org/0009-0005-4526-5832; Cai, Yanjun
ORCID: https://orcid.org/0000-0001-7063-5050; Huang, Shouyi; Kathayat, Gayatri; Pérez-Mejías, Carlos
ORCID: https://orcid.org/0000-0002-8370-9271; Zong, Baoyun; Liu, Dianbing; Duan, Pengzhen; Svensson, Anders
ORCID: https://orcid.org/0000-0002-4364-6085; Spötl, Christoph
ORCID: https://orcid.org/0000-0001-7167-4940; Li, Youwei; Niu, Xiaowen
ORCID: https://orcid.org/0009-0002-7092-4930; Wang, Jian
ORCID: https://orcid.org/0000-0002-3606-0318; Li, Hanying; Ning, Youfeng; Xu, Yao; Wang, Xianfeng
ORCID: https://orcid.org/0000-0002-8614-5627; Stríkis, Nicolás M.
ORCID: https://orcid.org/0000-0003-4721-3380; Cruz, Francisco W.
ORCID: https://orcid.org/0000-0002-4030-4581; Sinha, Ashish
ORCID: https://orcid.org/0000-0001-5700-2451; Werner, Martin
ORCID: https://orcid.org/0000-0002-6473-0243; Lawrence Edwards, R.; Cheng, Hai
ORCID: https://orcid.org/0000-0002-5305-9458.
2025
Interstadial diversity of East Asian summer monsoon linked to changes of the Northern Westerlies.
Nature Communications, 16, 7765.
14, pp.
10.1038/s41467-025-63057-2
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© The Author(s) 2025. s41467-025-63057-2.pdf - Published Version Available under License Creative Commons Attribution 4.0. Download (2MB) | Preview |
Abstract/Summary
During the last glacial period, the iconic Greenland ice-core records provide evidence of interstadial warmings with various durations ranging from a century to millennia. However, whether differences in interstadial duration are mirrored by distinct hydroclimate responses in the tropics remains unclear. Here we present four speleothem δ 18 O records from the Indian summer monsoon (ISM) and East Asian summer monsoon (EASM) regions, spanning both short and long interstadials during the last glacial period. Greenland and ISM records show broadly similar isotopic responses across events, however, the EASM records exhibit markedly different δ 18 O depletions between short and long interstadials. Using an isotope-enabled climate model, we attribute these differences to a further northward shift of the Northern Westerlies during short interstadials, driven by intensified high-latitude warming. This shift promoted the northwestward expansion of Western Pacific Subtropical High and hence the delivery of isotopically enriched near-sourced vapor to eastern China, dampening δ 18 O depletion during stadial-to-interstadial transitions. Our findings highlight a previously unrecognized sensitivity of EASM precipitation δ 18 O to nuanced meridional shifts in the Northern Westerlies in contrast to the uniform responses of the ISM during interstadials.
Item Type: | Publication - Article |
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Digital Object Identifier (DOI): | 10.1038/s41467-025-63057-2 |
ISSN: | 2041-1723 |
Date made live: | 26 Aug 2025 10:06 +0 (UTC) |
URI: | https://nora.nerc.ac.uk/id/eprint/540140 |
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