Suborbital- and millennial-scale monsoon variability during Pleistocene interglacials

Y Youbin Sun (State Key Laboratory of Loess Science, Institute of Earth Environment, Chinese Academy of Sciences) T Ting Wang (Department of Radiation Oncology The Affiliated Cancer Hospital of Zhengzhou University and Henan Cancer Hospital Zhengzhou China) Q Qiuzhen Yin (Earth and Climate Research Center, Earth and Life Institute, Université catholique de Louvain) S Steven C. Clemens (Department of Earth, Environmental, and Planetary Sciences, Brown University) X Xingxing Liu (State Key Laboratory of Loess Science, Institute of Earth Environment, Chinese Academy of Sciences) L Li Ai (State Key Laboratory of Loess Science, Institute of Earth Environment, Chinese Academy of Sciences) Z Zhipeng Wu (Earth and Climate Research Center, Earth and Life Institute, Université catholique de Louvain) X Xiaoke Qiang (State Key Laboratory of Loess Science, Institute of Earth Environment, Chinese Academy of Sciences) X Xulong Wang (State Key Laboratory of Loess Science, Institute of Earth Environment, Chinese Academy of Sciences) H Hong Chang (State Key Laboratory of Loess Science, Institute of Earth Environment, Chinese Academy of Sciences) Y Yougui Song (State Key Laboratory of Loess Science, Institute of Earth Environment, Chinese Academy of Sciences) H Hendrik Vogel (Institute of Geological Sciences & Oeschger Centre for Climate Change Research, University of Bern) J John Dodson (State Key Laboratory of Loess Science, Institute of Earth Environment, Chinese Academy of Sciences) A Andre Berger (Earth and Climate Research Center, Earth and Life Institute, Université catholique de Louvain) Z Zhisheng An (State Key Laboratory of Loess Science, Institute of Earth Environment, Chinese Academy of Sciences)

Abstract

Observational and modeling results show that the frequency and amplitude of extreme climatic events have increased significantly in the context of global warming. However, whether abrupt climate changes intensified during past warm periods remains poorly constrained due to the lack of high-resolution geological records. Here, we report a 512-m predominantly lacustrine sedimentary record from the Weihe Basin (North China), revealing that lake levels fluctuated significantly on suborbital (half- and quarter-precession) and millennial timescales over the last 2 Ma. Grain-size results reveal that magnitudes of rapid lake level fluctuations increased dramatically during Pleistocene interglacials, differing from glacial amplification of abrupt climate events recorded in North Atlantic marine sediments. Model results indicate that summer insolation maxima in low-latitude region of both hemispheres can lead to intensified monsoon precipitation in East Asia. Our proxy-model comparison highlights the importance of low-latitude bihemispheric insolation maxima in driving millennial-scale hydroclimatic variability in a warming future.

Article Details

Volume / Issue Vol. 122, Issue 23
Published June 10, 2025
ISSN 0027-8424
Publisher National Academy of Sciences

Authors (15)

Y

Youbin Sun

State Key Laboratory of Loess Science, Institute of Earth Environment, Chinese Academy of Sciences

T

Ting Wang

Department of Radiation Oncology The Affiliated Cancer Hospital of Zhengzhou University and Henan Cancer Hospital Zhengzhou China

Q

Qiuzhen Yin

Earth and Climate Research Center, Earth and Life Institute, Université catholique de Louvain

S

Steven C. Clemens

Department of Earth, Environmental, and Planetary Sciences, Brown University

X

Xingxing Liu

State Key Laboratory of Loess Science, Institute of Earth Environment, Chinese Academy of Sciences

L

Li Ai

State Key Laboratory of Loess Science, Institute of Earth Environment, Chinese Academy of Sciences

Z

Zhipeng Wu

Earth and Climate Research Center, Earth and Life Institute, Université catholique de Louvain

X

Xiaoke Qiang

State Key Laboratory of Loess Science, Institute of Earth Environment, Chinese Academy of Sciences

X

Xulong Wang

State Key Laboratory of Loess Science, Institute of Earth Environment, Chinese Academy of Sciences

H

Hong Chang

State Key Laboratory of Loess Science, Institute of Earth Environment, Chinese Academy of Sciences

Y

Yougui Song

State Key Laboratory of Loess Science, Institute of Earth Environment, Chinese Academy of Sciences

H

Hendrik Vogel

Institute of Geological Sciences & Oeschger Centre for Climate Change Research, University of Bern

J

John Dodson

State Key Laboratory of Loess Science, Institute of Earth Environment, Chinese Academy of Sciences

A

Andre Berger

Earth and Climate Research Center, Earth and Life Institute, Université catholique de Louvain

Z

Zhisheng An

State Key Laboratory of Loess Science, Institute of Earth Environment, Chinese Academy of Sciences