@article{fdi:010062080,
  title = {{C}hanges in the spatial structure of strong and moderate {E}l {N}ino events under global warming},
  author = {{Y}eh, {S}. {W}. and {K}im, {H}. and {K}won, {M}. and {D}ewitte, {B}oris},
  editor = {},
  language = {{ENG}},
  abstract = {{I}n this study, we examine how the spatial structures of strong and moderate {E}l{N}ino events have changed due to global warming using the {C}oupled {M}odel {I}ntercomparison {P}roject {P}hase 5 ({CMIP}5) coupled general circulation models ({CGCM}s) based on a historical run and a {R}epresentative {C}oncentration {P}athways ({RCP})4.5 run. {T}he centre of the maximum anomalous sea surface temperature ({SST}) in the moderate {E}l{N}ino has shifted significantly westward from the historical run to the {RCP}4.5 run; however, this is not seen with the strong {E}l{N}ino events. {F}urther analysis indicates that the centre of the maximum anomalous {SST} in the moderate {E}l{N}ino with a negative {P}acific {D}ecadal {O}scillation ({PDO}) phase shifted westward around the international dateline from the historical run to the {RCP}4.5 run. {T}his is in contrast to the moderate {E}l{N}ino, which shows a positive {PDO} phase. {W}e also briefly discuss a possible mechanism on the change in the spatial structure of moderate {E}l{N}ino with a negative phase of {PDO} from the historical run to the {RCP}4.5 run.},
  keywords = {{E}l{N}ino ; {P}acific {D}ecadal {O}scillation ; global warming ; spatial structure ; {PACIFIQUE}},
  booktitle = {},
  journal = {{I}nternational {J}ournal of {C}limatology},
  volume = {34},
  numero = {8},
  pages = {2834--2840},
  ISSN = {0899-8418},
  year = {2014},
  DOI = {10.1002/joc.3876},
  URL = {https://www.documentation.ird.fr/hor/fdi:010062080},
}