Lengaigne Matthieu auteur aut IRD Vecchi G. A. auteur aut IRD text journalArticle eng text/pdf born digital access As in the observed record, the termination of El Nino in the coupled IPCC-AR4 climate models involves meridional processes tied to the seasonal cycle. These meridional processes both precondition the termination of El Nino events in general and lead to a peculiar termination of extreme El Nino events (such as those of 1982-83 and 1997-98), in which the eastern equatorial Pacific warm sea surface temperature anomalies (SSTA) persist well into boreal spring/early-summer. The mechanisms controlling the peculiar termination of extreme El Nino events, which involves to the development of an equatorially centred intertropical convergence zone, are consistent across the four models that exhibit extreme El Ninos and observational record, suggesting that this peculiar termination represents a general feature of extreme El Ninos. Further, due to their unusual termination, extreme El Ninos exhibit an apparent eastward propagation of their SSTA, which can strongly influence estimates of the apparent propagation of ENSO over multi-decadal periods. Interpreting these propagation changes as evidence of changes in the underlying dynamical feedbacks behind El Nino could therefore be misleading, given the strong influence of a single extreme event. specialized El Nino/Southern Oscillation (ENSO) Extreme events IPCC-AR4 climate models Coupled ocean-atmosphere mechanisms Validation 032 021 35 2-3 299-313 2010 0930-7575 https://www.documentation.ird.fr/hor/fdi:010049689 10.1007/s00382-009-0562-3 0930-7575 [F B010049689] https://www.documentation.ird.fr/hor/fdi:010049689 https://www.documentation.ird.fr/intranet/publi/2010/08/010049689.pdf Accès réservé (Intranet de l'IRD) IRD - Base Horizon / Pleins textes 2010-09-03 2017-08-23 fdi:010049689 fre