lmd_Bony1998.bib

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@article{1998CRASE.326..677B,
  author = {{Barthelet}, P. and {Bony}, S. and {Braconnot}, P. and {Braun}, A. and 
	{Cariolle}, D. and {Cohen-Solal}, E. and {Dufresne}, J.-L. and 
	{Delecluse}, P. and {Déqué}, M. and {Fairhead}, L. and 
	{Filiberti}, M.-A. and {Forichon}, M. and {Grandpeix}, J.-Y. and 
	{Guilyardi}, E. and {Hqussais}, M.-N. and {Imbard}, M. and {Le Treut}, H. and 
	{Lévy}, C. and {Xin Li}, Z. and {Madec}, G. and {Marquet}, P. and 
	{Marti}, O. and {Planton}, S. and {Terray}, L. and {Thual}, O. and 
	{Valcke}, S.},
  title = {{Simulations couplées globales des changements climatiques associés {\`a} une augmentation de la teneur atmosphérique en CO $_{2}$}},
  journal = {Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science},
  year = 1998,
  month = may,
  volume = 326,
  pages = {677-684},
  abstract = {{Two transient CO $_{2}$ experiments using two coupled general
circulation models developed by the French GASTON group have been
realized using the same methodology. No flux corrections at the air-sea
interface were used in these experiments. The main features of the
present climate are reasonably well captured by both coupled models in
the control simulations, although the biases are not the same, The
transient CO $_{2}$ simulations show a global warming, ranging
between 1.6 and 2.0 {\deg}C at the time of CO $_{2}$ doubling (+ 70
years). These values, and the main geographical characteristics of
climate change, are in agreement with previous studies published by
other research groups, using either flux corrected or non-flux corrected
models.
}},
  doi = {10.1016/S1251-8050(98)80178-X},
  adsurl = {http://adsabs.harvard.edu/abs/1998CRASE.326..677B},
  adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}