Cherchi A. auteur aut IRD Terray Pascal auteur aut IRD Ratna S.B. auteur aut IRD Sankar S. auteur aut IRD Sooraj K.P. auteur aut IRD Behera S. auteur aut IRD text bookSection eng text/pdf born digital access The Indian Ocean Dipole (IOD) is one of the dominant modes of variability of the tropical Indian Ocean and it has been suggested to have a crucial role in the teleconnection between the Indian summer monsoon and El Niño Southern Oscillation (ENSO). The main ideas at the base of the influence of the IOD on the ENSO-monsoon teleconnection include the possibility that it may strengthen summer rainfall over India, as well as the opposite, and also that it may produce a remote forcing on ENSO itself. In the future, the IOD is projected to increase in frequency and amplitude with mean conditions mimicking the characteristics of its positive phase. Still, state-of-the-art global climate models have large biases in representing the mean state and variability of both IOD and ISM, with potential consequences for their future projections. However, the characteristics of the IOD and ENSO are likely to continue in a future warmer world, with persistence of their linkage. specialized OCEAN INDIEN 032 021 Chowdary J.S. ed. edt IRD Parekh A. ed. edt IRD Gnanaseelan C. ed. edt IRD 157-182 Amsterdam Elsevier 2021 https://www.documentation.ird.fr/hor/fdi:010087066 10.1016/B978-0-12-822402-1.00011-9 978-0-12-822402-1 [F B010087066] https://www.documentation.ird.fr/hor/fdi:010087066 https://www.documentation.ird.fr/intranet/publi/2023-01/010087066.pdf Accès réservé (Intranet de l'IRD) IRD - Base Horizon / Pleins textes 2023-01-05 2025-02-24 fdi:010087066 fre