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  author = {{Marti}, O. and {Braconnot}, P. and {Dufresne}, J.-L. and {Bellier}, J. and 
	{Benshila}, R. and {Bony}, S. and {Brockmann}, P. and {Cadule}, P. and 
	{Caubel}, A. and {Codron}, F. and {de Noblet}, N. and {Denvil}, S. and 
	{Fairhead}, L. and {Fichefet}, T. and {Foujols}, M.-A. and {Friedlingstein}, P. and 
	{Goosse}, H. and {Grandpeix}, J.-Y. and {Guilyardi}, E. and 
	{Hourdin}, F. and {Idelkadi}, A. and {Kageyama}, M. and {Krinner}, G. and 
	{Lévy}, C. and {Madec}, G. and {Mignot}, J. and {Musat}, I. and 
	{Swingedouw}, D. and {Talandier}, C.},
  title = {{Key features of the IPSL ocean atmosphere model and its sensitivity to atmospheric resolution}},
  journal = {Climate Dynamics},
  keywords = {Climate, Simulations, Ocean, Atmosphere, Coupling, Circulation, El Ni{\~n}o/Southern oscillation, North-Atlantic oscillation, Storm-tracks, Resolution},
  year = 2010,
  month = jan,
  volume = 34,
  pages = {1-26},
  abstract = {{This paper presents the major characteristics of the Institut Pierre
Simon Laplace (IPSL) coupled ocean-atmosphere general circulation model.
The model components and the coupling methodology are described, as well
as the main characteristics of the climatology and interannual
variability. The model results of the standard version used for IPCC
climate projections, and for intercomparison projects like the
Paleoclimate Modeling Intercomparison Project (PMIP 2) are compared to
those with a higher resolution in the atmosphere. A focus on the North
Atlantic and on the tropics is used to address the impact of the
atmosphere resolution on processes and feedbacks. In the North Atlantic,
the resolution change leads to an improved representation of the
storm-tracks and the North Atlantic oscillation. The better
representation of the wind structure increases the northward salt
transports, the deep-water formation and the Atlantic meridional
overturning circulation. In the tropics, the ocean-atmosphere dynamical
coupling, or Bjerknes feedback, improves with the resolution. The
amplitude of ENSO (El Ni{\~n}o-Southern oscillation) consequently
increases, as the damping processes are left unchanged.
  doi = {10.1007/s00382-009-0640-6},
  adsurl = {https://ui.adsabs.harvard.edu/abs/2010ClDy...34....1M},
  adsnote = {Provided by the SAO/NASA Astrophysics Data System}
  author = {{Hourdin}, F. and {Musat}, I. and {Guichard}, F. and {Ruti}, P.~M. and 
	{Favot}, F. and {Filiberti*}, M.-A. and {Pham}, M. and {Grandpeix}, J.-Y. and 
	{Polcher}, J. and {Marquet}, P. and {Boone}, A. and {Lafore}, J.-P. and 
	{Redelsperger}, J.-L. and {Dell'Aquila}, A. and {Doval}, T.~L. and 
	{Traore}, A.~K. and {Gallée}, H.},
  title = {{AMMA-Model Intercomparison Project}},
  journal = {Bulletin of the American Meteorological Society},
  year = 2010,
  volume = 91,
  pages = {95},
  doi = {10.1175/2009BAMS2791.1},
  adsurl = {https://ui.adsabs.harvard.edu/abs/2010BAMS...91...95H},
  adsnote = {Provided by the SAO/NASA Astrophysics Data System}