- P. Braconnot : MISSTERRE, CMIP5 et « issue spéciale climate dynamics »
- A. Voldoire : The CNRM‐CM5 global climate model: description and basic evaluation?
- J.L. Dufresne : The IPSL‐CM5A Earth System Model: general description and climate change projections
- C. Cassou : Synthèse exercice en cours dans les 2 groupes + premiers résultats CERFACS
- S. Denvil : Diffusion des données (cmor, base de données, accès, etc.)
- D. Salas y Melia: The impact of the inclusion of new sea ice processes on the simulation of sea ice by CNRM‐CM5 global coupled model
- F. Cheruy : Day‐to‐day evaluation with respect Sirta measurements of the various physics of the LMDZ model with a streched grid and nudging
- A. Gainusa-Bogdan : Model‐data comparison of Heat and momentum fluxes over tropical oceans
- S. Fermepin : Evaluation of the LMDZ/IPSL climate model in a weather prediction mode; Comparison with single column model evaluations
- C. Rio : On the control of deep convection by subcloud processes in the LMDZNP model through the Available Lifting Power
- F. Hourdin : LMDZ5 « New Physics » : principles and impact on the climate of theIPSL coupled model of a complete refundation of the boundary layer/convection/cloud parameterization
- S. Szopa: Changes in tropospheric aerosoland reactive gases burdens and concentrations under IPCC‐AR5 emission scenarios for1850‐2100
- F. Brient : Analysis of the physical mechanisms controlling tropical low‐cloud feedbacks in the IPSL climate model through a hierarchy of model configurations
- K. Kamala : ENSO‐Indian monsoon teleconnection in the CNRMand IPSL historical simulations
- P. Maury : Tropical variability and stratospheric equatorial waves in the IPSLCM5 model
- J. Cattiaux : North‐Atlantic weather regimes and European temperatures in the IPSL model: sensitivity to atmospheric resolution
- F. Codron : Impact of horizontal resolution on the eddy‐driven jets: mean state and variability
- R. Escudier : Multidecadal variability and air‐sea interactions in the subpolar North Atlantic
- D. Swingedouw : Initialisation and predictability of the AMOC in the IPSLCM5 model over the last 60 years
- A. Persechino : Perfect model predictability with IPSLCM5
- A. Persechino : Decadal predictability in the thermohaline circulation and climate in the IPSLCM5 model
- G. Gastineau : Atmospheric response to the North Atlantic oceanic variability on seasonal to decadal time scale
- S. Parouty : High southern latitudes and Antarctic atmospheric circulation / climate in the IPSL‐CM5 model
- O. Geoffroy : Climate sensitivity and radiative feedbacks in the CNRM‐CM5 climate model
- S. Bony : Analysis of the tropical precipitation response to climate change predicted by the IPSL climate model
- M. Kageyama : Mid‐Holocene and Last Glacial Maximum climate simulations with the IPSL model: new features with the IPSL_CM5 version
- J. Cattiaux : Present‐day biases and future changes in European temperatures: a pilot study with CNRM and IPSL models
- P. Cadule : Carbon-climate feedbacks: comparison bewteen IPSL-CM4-LOOP and IPSLCM5A-C
- R. Seferian : Simulating marine biogeochemitry in coupled climate models: evaluation and intercomparison of IPSL‐CM and CNRM‐CM
- J.C. Orr : Differences between anthropogenic perturbations in heat, CO2, and CFC in the IPSL‐CM and CNRM‐CM earth system models
- B. Guenet : Does the integration of dynamic N cycle in land surface model improve the long‐term trend of LAI and the land surface CO2 exchange in the atmosphere?
- A. Colette: Performance of LMDz global CMIP5 historical climate simulations versus downscaled regional simulations using WRF
- A. Ribes : Detection attribution in the mediteranean basin
- S. Somot : Simulations CORDEX CNRM
- Simulations CORDEX IPSL
CMIP5 experiment results – internships
- A. Dehecq : Changement climatique: quels rythmes d’évolution du climat en fonction des scénarios
- G. Drouot : Variabilité des pluies de moussons dans le modèle CM5
- R. Waldman : Varaibilité saisonnière de la circulation méridienne de retournement dans l’Atlantique: comparaison modèle IPSL_CM5A et données à 26°N