@incollection{fdi:010087066,
  title = {{I}ndian {O}cean {D}ipole influence on {I}ndian summer monsoon and {ENSO} : a review},
  author = {{C}herchi, {A}. and {T}erray, {P}ascal and {R}atna, {S}.{B}. and {S}ankar, {S}. and {S}ooraj, {K}.{P}. and {B}ehera, {S}.},
  editor = {},
  language = {{ENG}},
  abstract = {{T}he {I}ndian {O}cean {D}ipole ({IOD}) is one of the dominant modes of variability of the tropical {I}ndian {O}cean and it has been suggested to have a crucial role in the teleconnection between the {I}ndian summer monsoon and {E}l {N}iño {S}outhern {O}scillation ({ENSO}). {T}he 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 {I}ndia, as well as the opposite, and also that it may produce a remote forcing on {ENSO} itself. {I}n the future, the {IOD} is projected to increase in frequency and amplitude with mean conditions mimicking the characteristics of its positive phase. {S}till, 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. {H}owever, the characteristics of the {IOD} and {ENSO} are likely to continue in a future warmer world, with persistence of their linkage.},
  keywords = {{OCEAN} {INDIEN}},
  booktitle = {{I}ndian summer monsoon variability : {E}l-{N}iño teleconnections and beyond},
  numero = {},
  pages = {157--182},
  address = {{A}msterdam},
  publisher = {{E}lsevier},
  series = {},
  year = {2021},
  DOI = {10.1016/{B}978-0-12-822402-1.00011-9},
  ISBN = {978-0-12-822402-1},
  URL = {https://www.documentation.ird.fr/hor/fdi:010087066},
}