Author
Listed:
- Shujun Li
(Ocean University of China
Ocean University of China
Laoshan Laboratory)
- Lixin Wu
(Ocean University of China
Laoshan Laboratory)
- Yiting Wang
(Ocean University of China)
- Tao Geng
(Laoshan Laboratory)
- Wenju Cai
(Ocean University of China
Laoshan Laboratory
Chinese Academy of Sciences
Xiamen University)
- Bolan Gan
(Ocean University of China
Laoshan Laboratory)
- Zhao Jing
(Ocean University of China
Laoshan Laboratory)
- Yun Yang
(Beijing Normal University)
Abstract
The Atlantic multidecadal variability (AMV) is a basin-scale mode of sea surface temperature (SST) variability in the North Atlantic, exerting a global impact, including contribution to the multidecadal Sahel drought and subsequent recovery and the post-1998 global warming hiatus. How greenhouse warming affects AMV remains unclear. Here, using models with multicentury-long outputs of future climate, we find an intensified AMV under greenhouse warming. Surface warming and freshwater input from sea-ice melt increase surface buoyancy, leading to a slowdown of the Atlantic meridional overturning circulation (AMOC). Reduced vertical mixing associated with suppressed oceanic deep convection results in a thinned mixed layer and its variability, favouring stronger AMV SST variability. Further, a weakened AMOC and the associated northward heat transport prolong the lifespan of the AMV, providing a long time for the AMV to grow. Thus, multidecadal global surface fluctuations and the associated climate extremes are likely to be more intense.
Suggested Citation
Shujun Li & Lixin Wu & Yiting Wang & Tao Geng & Wenju Cai & Bolan Gan & Zhao Jing & Yun Yang, 2025.
"Intensified Atlantic multidecadal variability in a warming climate,"
Nature Climate Change, Nature, vol. 15(3), pages 293-300, March.
Handle:
RePEc:nat:natcli:v:15:y:2025:i:3:d:10.1038_s41558-025-02252-x
DOI: 10.1038/s41558-025-02252-x
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