Khodri Myriam auteur aut IRD Izumo Takeshi auteur aut IRD Vialard Jérôme auteur aut IRD Janicot Serge auteur aut IRD Cassou C. auteur aut IRD Lengaigne Matthieu auteur aut IRD Mignot Juliette auteur aut IRD Gastineau G. auteur aut IRD Guilyardi E. auteur aut IRD Lebas N. auteur aut IRD Robock A. auteur aut IRD McPhaden M. J. auteur aut IRD text journalArticle eng text/pdf reformatted digital access Stratospheric aerosols from large tropical explosive volcanic eruptions backscatter shortwave radiation and reduce the global mean surface temperature. Observations suggest that they also favour an El Nino within 2 years following the eruption. Modelling studies have, however, so far reached no consensus on either the sign or physical mechanism of El Nino response to volcanism. Here we show that an El Nino tends to peak during the year following large eruptions in simulations of the Fifth Coupled Model Intercomparison Project (CMIP5). Targeted climate model simulations further emphasize that Pinatubo-like eruptions tend to shorten La Ninas, lengthen El Ninos and induce anomalous warming when occurring during neutral states. Volcanically induced cooling in tropical Africa weakens the West African monsoon, and the resulting atmospheric Kelvin wave drives equatorial westerly wind anomalies over the western Pacific. This wind anomaly is further amplified by air-sea interactions in the Pacific, favouring an El Nino-like response. specialized AFRIQUE PACIFIQUE 032 066 8 art. no 778 [13 + Correction art.no 855, 1 p.] 2017 2041-1723 https://www.documentation.ird.fr/hor/fdi:010071053 10.1038/s41467-017-00755-6 2041-1723 [F B010071053] https://www.documentation.ird.fr/hor/fdi:010071053 https://horizon.documentation.ird.fr/exl-doc/pleins_textes/divers17-10/010071053.pdf IRD - Base Horizon / Pleins textes 2017-10-31 2023-07-11 fdi:010071053 fre