@article{fdi:010071935,
  title = {{T}entative reconstruction of the 1998-2012 hiatus in global temperature warming using the {IPSL}-{CM}5{A}-{LR} climate model},
  author = {{S}wingedouw, {D}. and {M}ignot, {J}uliette and {G}uilyardi, {E}. and {N}guyen, {S}. and {O}rmieres, {L}.},
  editor = {},
  language = {{ENG}},
  abstract = {{T}he period running from 1998 to 2012 has experienced a slower increase in global temperature at the surface of the {E}arth than the decades before. {S}everal explanations have been proposed, ranging from internal variability of the climate system to a contribution of the natural external forcing. {I}n this study, we use the {IPSL}-{CM}5{A}-{LR} climate model to test these different hypotheses. {W}e consider historical simulations, including observed external forcing, in which nudging towards observed sea surface temperature has been applied to different regions of the ocean to phase the decadal variability of large-scale modes in the {A}tlantic and the {P}acific to observations. {W}e find that phasing the tropical {P}acific is reducing the warming trend detected in historical simulations by a factor of two, but the remaining trend is still twice as large as the observed one. {C}ombining the tropical {P}acific phasing and the potential effect of recent eruptions allows us to fully reproduce the observed hiatus. {C}onversely, nudging the {A}tlantic does not drive any hiatus in this model.},
  keywords = {{C}limate and ocean dynamics ; {G}lobal warming ; {H}iatus ; {P}acemaker experiments ; {C}limate models ; {S}urface nudging ; {G}lobal temperature trends ; {ATLANTIQUE} ; {PACIFIQUE} ; {ZONE} {TROPICALE}},
  booktitle = {},
  journal = {{C}omptes {R}endus {G}eoscience},
  volume = {349},
  numero = {8},
  pages = {369--379},
  ISSN = {1631-0713},
  year = {2017},
  DOI = {10.1016/j.crte.2017.09.014},
  URL = {https://www.documentation.ird.fr/hor/fdi:010071935},
}