The fast response of Sahel precipitation to climate change allows effective mitigation action

Abstract Climate change will drive major perturbations of the West African summer monsoon. A zonal contrast in precipitation will develop at the end of the century, with an increase in precipitation over the central Sahel and a decrease in precipitation over the western Sahel. Such a zonal contrast...

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Main Authors: Paul-Arthur Monerie, Benjamin Pohl, Marco Gaetani
Format: Article
Language:English
Published: Nature Publishing Group 2021-04-01
Series:npj Climate and Atmospheric Science
Online Access:https://doi.org/10.1038/s41612-021-00179-6
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spelling doaj-a31bb69e7a44452d9268ce8af5b03c242021-04-11T11:10:08ZengNature Publishing Groupnpj Climate and Atmospheric Science2397-37222021-04-01411810.1038/s41612-021-00179-6The fast response of Sahel precipitation to climate change allows effective mitigation actionPaul-Arthur Monerie0Benjamin Pohl1Marco Gaetani2National Centre for Atmospheric Science (NCAS), Department of Meteorology, University of ReadingCentre de Recherches de Climatologie, UMR 6282 Biogéosciences, CNRS/Université de Bourgogne Franche-ComtéScuola Universitaria Superiore IUSSAbstract Climate change will drive major perturbations of the West African summer monsoon. A zonal contrast in precipitation will develop at the end of the century, with an increase in precipitation over the central Sahel and a decrease in precipitation over the western Sahel. Such a zonal contrast results from the antagonist effects of the fast (due to enhanced radiative warming over land, and over the North Hemisphere, relative to the South Hemisphere) and slow (associated with long-term changes in oceanic circulation) responses of precipitation to increasing greenhouse gases. While such changes have already been assessed, less attention has been given to their temporality, an issue of major importance to promote efficient mitigation and adaptation measures. Here, we analyse the future evolution of precipitation changes decomposed into a fast and a slow response, showing that the fast response dominates the slow one. From this evidence, we highlight that mitigation strategies may be successful at reducing the effect of climate change on Sahel precipitation within a few decades, by muting the fast response. This decomposition also allows for a better understanding of the uncertainty of climate model predictions in Africa.https://doi.org/10.1038/s41612-021-00179-6
collection DOAJ
language English
format Article
sources DOAJ
author Paul-Arthur Monerie
Benjamin Pohl
Marco Gaetani
spellingShingle Paul-Arthur Monerie
Benjamin Pohl
Marco Gaetani
The fast response of Sahel precipitation to climate change allows effective mitigation action
npj Climate and Atmospheric Science
author_facet Paul-Arthur Monerie
Benjamin Pohl
Marco Gaetani
author_sort Paul-Arthur Monerie
title The fast response of Sahel precipitation to climate change allows effective mitigation action
title_short The fast response of Sahel precipitation to climate change allows effective mitigation action
title_full The fast response of Sahel precipitation to climate change allows effective mitigation action
title_fullStr The fast response of Sahel precipitation to climate change allows effective mitigation action
title_full_unstemmed The fast response of Sahel precipitation to climate change allows effective mitigation action
title_sort fast response of sahel precipitation to climate change allows effective mitigation action
publisher Nature Publishing Group
series npj Climate and Atmospheric Science
issn 2397-3722
publishDate 2021-04-01
description Abstract Climate change will drive major perturbations of the West African summer monsoon. A zonal contrast in precipitation will develop at the end of the century, with an increase in precipitation over the central Sahel and a decrease in precipitation over the western Sahel. Such a zonal contrast results from the antagonist effects of the fast (due to enhanced radiative warming over land, and over the North Hemisphere, relative to the South Hemisphere) and slow (associated with long-term changes in oceanic circulation) responses of precipitation to increasing greenhouse gases. While such changes have already been assessed, less attention has been given to their temporality, an issue of major importance to promote efficient mitigation and adaptation measures. Here, we analyse the future evolution of precipitation changes decomposed into a fast and a slow response, showing that the fast response dominates the slow one. From this evidence, we highlight that mitigation strategies may be successful at reducing the effect of climate change on Sahel precipitation within a few decades, by muting the fast response. This decomposition also allows for a better understanding of the uncertainty of climate model predictions in Africa.
url https://doi.org/10.1038/s41612-021-00179-6
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