Impacts of AMOC Collapse on Monsoon Rainfall: A Multi‐Model Comparison

Abstract A collapse of the Atlantic Meridional Overturning Circulation (AMOC) would have substantial impacts on global precipitation patterns, especially in the vulnerable tropical monsoon regions. We assess these impacts in experiments that apply the same freshwater hosing to four state‐of‐the‐art climate models with bistable AMOC. As opposed to previous results, we find that the spatial and seasonal patterns of precipitation change are remarkably consistent across models. We focus on the South American Monsoon (SAM), the West African Monsoon (WAM), the Indian Summer Monsoon (ISM) and the East Asian Summer Monsoon (EASM). Models consistently suggest substantial disruptions for WAM, ISM, and EASM with shorter wet and longer dry seasons (−29.07%, −18.76%, and −3.78% ensemble mean annual rainfall change, respectively). Models also agree on changes for the SAM, suggesting rainfall increases overall, in contrast to previous studies. These are more pronounced in the southern Amazon (+43.79%), accompanied by decreasing dry‐season length. Consistently across models, our results suggest a robust and major rearranging of all tropical monsoon systems in response to an AMOC collapse.

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Publication Details

Journal
Earth s Future
Published
2024-09-01
DOI
https://doi.org/10.1029/2023ef003959
Citations
21
Primary Topic
Flood Risk Assessment and Management
Type
article
Field-Weighted Citation Impact
5.94

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Impacts of AMOC Collapse on Monsoon Rainfall: A Multi‐Model Comparison

Niklas Boers, Maya Ben‐Yami, Aixue Hu, Didier Swingedouw et al.
21 citations
Earth s Future
Flood Risk Assessment and Management
5.94
article

Impacts of AMOC Collapse on Monsoon Rainfall: A Multi‐Model Comparison

Niklas Boers, Maya Ben‐Yami, Aixue Hu, Didier Swingedouw, Laura Jackson, Peter Good, Oleg A. Saenko, Michel Crucifix
article en
21 citations

Abstract

Abstract A collapse of the Atlantic Meridional Overturning Circulation (AMOC) would have substantial impacts on global precipitation patterns, especially in the vulnerable tropical monsoon regions. We assess these impacts in experiments that apply the same freshwater hosing to four state‐of‐the‐art climate models with bistable AMOC. As opposed to previous results, we find that the spatial and seasonal patterns of precipitation change are remarkably consistent across models. We focus on the South American Monsoon (SAM), the West African Monsoon (WAM), the Indian Summer Monsoon (ISM) and the East Asian Summer Monsoon (EASM). Models consistently suggest substantial disruptions for WAM, ISM, and EASM with shorter wet and longer dry seasons (−29.07%, −18.76%, and −3.78% ensemble mean annual rainfall change, respectively). Models also agree on changes for the SAM, suggesting rainfall increases overall, in contrast to previous studies. These are more pronounced in the southern Amazon (+43.79%), accompanied by decreasing dry‐season length. Consistently across models, our results suggest a robust and major rearranging of all tropical monsoon systems in response to an AMOC collapse.

Earth s FutureVol. 12(9)
NSF National Center for Atmospheric Research (US), Met Office (GB), Université de Bordeaux (FR), University of Victoria (CA), University of Exeter (GB), Environnements et Paléoenvironnements Océaniques et Continentaux (FR), NSF NCAR Climate and Global Dynamics Laboratory (US), Potsdam Institute for Climate Impact Research (DE), Technical University of Munich (DE), UCLouvain (BE)
European Commission, Met Office, Volkswagen Foundation, Bundesministerium für Bildung und Forschung, Horizon 2020 Framework Programme, H2020 Marie Skłodowska-Curie Actions
Climate action
Openalex Percentile: Top 3%
Flood Risk Assessment and Management
5.94
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