Orchestrated decline of Asian summer monsoon and Atlantic meridional overturning circulation in global warming period

Jingyao Zhao; Hai Cheng; Jie Cao; Ashish Sinha; Xiyu Dong; Liangkang Pan; Carlos Pérez-Mejías; Haiwei Zhang; Hanying Li; Jian Wang; Kexin Wang; Jiahui Cui; Yan Yang

doi:10.59717/j.xinn-geo.2023.100011

The Innovation Geoscience > 2023 Vol. 1 > No. 1 > 1-9

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Orchestrated decline of Asian summer monsoon and Atlantic meridional overturning circulation in global warming period

1.
Institute of Global Environmental Change, Xi’an Jiaotong University, Xi’an 710054, China
2.
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710061, China
3.
Department of Atmospheric Sciences, Yunnan University, Kunming 650500, China
4.
Department of Earth Science, California State University Dominguez Hills, Carson, CA 90747, USA
5.
Chongqing Key Laboratory of Karst Environment & School of Geographical Sciences, Southwest University, Chongqing 400715, China

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Corresponding authors: cheng021@xjtu.edu.cn (H.C.); caoj@ynu.edu.cn (J.C.)
Received Date: 03 May 2023

Accepted Date: 26 May 2023

Published Online: 06 June 2023

The Innovation Geoscience 1(1), https://doi.org/10.59717/j.xinn-geo.2023.100011 | Cite this article

GRAPHICAL ABSTRACT

GRAPHICAL ABSTRACT

PUBLIC SUMMARY

PUBLIC SUMMARY
1. We present a high-quality speleothem δ¹⁸O record from the Shandong Peninsula, covering the global warming period.
  
  The trend of the enriched speleothem δ¹⁸O in global warming period mainly reflects dynamic facet of Asian summer monsoon.
  
  Decline of the Atlantic Meridional Overturning Circulation in global warming period may play a crucial role in the ASM weakening.

ABSTRACT

ABSTRACT

The anthropogenic warming of the Earth’s atmosphere is causing dynamical and thermodynamical changes in the ocean and atmosphere circulation, including the Asian summer monsoon (ASM) and the oxygen isotope compositions of its precipitation. Here we present a high-resolution speleothem δ¹⁸O record from the Shandong Peninsula, eastern China with an age precision of ± 3 years, which in conjunction with five other existing high-resolution speleothem records from the ASM domain, reveals a robust weakening trend in the ASM during the global warming period, particularly since around the 1970s. During this period, both the decline of the Atlantic Meridional Overturning Circulation inferred from existing model-empirical records and the spatially heterogeneous pattern of global warming inferred from the coupled reanalysis of the 20^th century (CERA-20C) product result in broadly similar changes in moisture flux pattern in the ASM domain. This, in turn, leads to the ASM weakening trend in terms of dynamics, as suggested by the speleothem δ¹⁸O records.

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Zhao J., Cheng H., Cao J., et al., (2023). Orchestrated decline of Asian summer monsoon and Atlantic meridional overturning circulation in global warming period. The Innovation Geoscience 1(1),. https://doi.org/10.59717/j.xinn-geo.2023.100011

Zhao J., Cheng H., Cao J., et al., (2023). Orchestrated decline of Asian summer monsoon and Atlantic meridional overturning circulation in global warming period. The Innovation Geoscience 1(1),. https://doi.org/10.59717/j.xinn-geo.2023.100011

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Orchestrated decline of Asian summer monsoon and Atlantic meridional overturning circulation in global warming period

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