Abstract
The El Niño–Southern Oscillation (ENSO) — describing shifts between warm El Niño and cold La Niña phases — has a substantial effect on the global climate. In this Review, we outline the mechanisms and climate impacts of ENSO in Africa, focusing on rainfall. ENSO’s influence varies strongly by season, region, phase, event and decade, highlighting complex dynamics and asymmetries. Although difficult to generalize, key characteristics include: anomalies across the Sahel in July–September, related to the tropospheric temperature mechanism; a strong dipole in anomalies between eastern and southern Africa during October–December (the short rain reason) and December–February, linked to interactions with the Indian Ocean Dipole and Indian Ocean Basin mode, respectively; and anomalies over southern Africa (with possible indications of opposite anomalies over East Africa) during March–May (the long rain season), associated with continuation of the Indian Ocean Basin mode. These teleconnections tend to be most pronounced for East Pacific El Niño and Central Pacific La Niña events, as well as during decades when interbasin interactions are strongest. Although challenging to simulate, climate models suggest that these impacts will strengthen in the future, manifesting as an increased frequency of ENSO-related dry and wet extremes. Given the reliance of much of Africa on rain-fed agriculture, resolving these relationships is vital, necessitating realistic simulation of regional circulations, ENSO and its interbasin interactions.
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Acknowledgements
The authors are grateful to J. Gan and the team from the Centre for Ocean Research, Hong Kong University of Science and Technology, for hosting the workshop on “Climate Variability and Impact on Africa” and for providing travel support. This project is supported by SKLLQGYS01. H.C.N was supported by Deutsche Forschungsgemeinschaft (DFG) grant 456490637. N.K. was supported by the research council of Norway (grant no. 328935). E.M. and B.R.-F. received funding from the Spanish Ministry of Science and Innovation projects (PID2021-125806NB-I00 and TED2021-130106B-I00). G.W., B.N., A.S.T. and X.Z. are supported by the Climate Systems Hub of the Australian Government’s National Environment Science Program. S.L. was supported by the National Natural Science Foundation of China (NSFC) projects 42376198 and 42006173. PMEL contribution no. 5586. The authors acknowledge the World Climate Research Programme’s Working Group on Coupled Modelling, which is responsible for CMIP, and they thank the climate modelling groups for producing and making available their model output, and the US Department of Energy Program for Climate Model Diagnosis and Intercomparison for coordinating support and leading development of software infrastructure in partnership with the Global Organization for Earth System Science Portals. The authors are grateful to various reanalysis groups for making the datasets available.
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W.C. and M.J.M. conceived the article. The manuscript was written as a group effort through participation in several “Climate Impact on Africa” workshops held online and at Hong Kong University of Science and Technology. W.C. designed the article and coordinated the writing. A.S. synthesized workshop key points. J.M. led Box 1. C.R., E.M. and B.R.-F. led discussion and revision of content synthesized into the ‘Dynamical connections of ENSO to Africa’ and ‘ENSO effects on the African climate’ sections. W.C. led other sections. Xichen. L., B.N., Y.L. and T.G. performed analyses and created the figures. All authors contributed to the manuscript preparation, interpretation and discussions.
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Cai, W., Reason, C., Mohino, E. et al. Climate impacts of the El Niño–Southern Oscillation in Africa. Nat Rev Earth Environ 6, 503–520 (2025). https://doi.org/10.1038/s43017-025-00705-7
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DOI: https://doi.org/10.1038/s43017-025-00705-7
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