Reinterpreting precipitation isotope records from Asian monsoon region through the hidden role of atmospheric updraft

Abstract Speleothem oxygen isotope records (δ 18 O s ) from the Asian monsoon region provide valuable insights into past hydroclimate variability, yet their interpretation relies on understanding the controls on modern precipitation isotopes (δ 18 O p ). Although numerous explanations for the spatiotemporal variability of δ 18 O p across this region have been proposed, the primary controls remain unresolved. Here we propose a hypothesis to explain δ 18 O p variability from δ 18 O p records at 46 sites along a transect spanning the Asian monsoon region. Our results show that seasonally low δ 18 O p values migrate gradually westward along the east–west transect. We further demonstrate that the corresponding westward migration of atmospheric updraft, particularly convection, controls δ 18 O p variations along the transect. In contrast to previous interpretations emphasizing monsoon moisture advection, our findings highlight atmospheric updraft as an important control on δ 18 O p variations across the Asian monsoon region. These findings provide an alternative perspective on interpreting the climate signals preserved in Asian δ 18 O s records.

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Journal
Nature Communications
Published
2026-09-11
DOI
https://doi.org/10.1038/s41467-026-77635-5
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
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article

Reinterpreting precipitation isotope records from Asian monsoon region through the hidden role of atmospheric updraft

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Nature Communications
Geology and Paleoclimatology Research
article

Reinterpreting precipitation isotope records from Asian monsoon region through the hidden role of atmospheric updraft

Rong Guo, Hong‐Chun Li, Kei Yoshimura, Supriyo Chakraborty, Hai Cheng, M. Midhun, Zhaowei Jing, Stephen Lewis, Lonnie G. Thompson, Wusheng Yu, Pengjie Ren, Antonios Mamalakis, Qiaoyi Wang, Liangcheng Tan, Deliang Chen, Neha Trivedi, Zhuanxia Zhang, Ziran Lei, Jingyi Zhang, R. K. Trivedi, Oliver Kracht
article en

Abstract

Abstract Speleothem oxygen isotope records (δ 18 O s ) from the Asian monsoon region provide valuable insights into past hydroclimate variability, yet their interpretation relies on understanding the controls on modern precipitation isotopes (δ 18 O p ). Although numerous explanations for the spatiotemporal variability of δ 18 O p across this region have been proposed, the primary controls remain unresolved. Here we propose a hypothesis to explain δ 18 O p variability from δ 18 O p records at 46 sites along a transect spanning the Asian monsoon region. Our results show that seasonally low δ 18 O p values migrate gradually westward along the east–west transect. We further demonstrate that the corresponding westward migration of atmospheric updraft, particularly convection, controls δ 18 O p variations along the transect. In contrast to previous interpretations emphasizing monsoon moisture advection, our findings highlight atmospheric updraft as an important control on δ 18 O p variations across the Asian monsoon region. These findings provide an alternative perspective on interpreting the climate signals preserved in Asian δ 18 O s records.

Nature Communications
Yunnan Normal University (CN), International Atomic Energy Agency (AT), Indian Institute of Tropical Meteorology (IN), National Taiwan University (TW), Chinese Academy of Sciences (CN), Cochin University of Science and Technology (IN), Beijing Forestry University (CN), Institute of Tibetan Plateau Research (CN), Institute of Earth Environment (CN), University of Chinese Academy of Sciences (CN), University of Virginia (US), The Ohio State University (US), The University of Tokyo (JP), Henan Normal University (CN), James Cook University (AU), Xi'an Jiaotong University (CN), Dr. Hari Singh Gour University (IN), Tsinghua University (CN)
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Geology and Paleoclimatology Research
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