Table 2.
List of CMIP5 GCMs that have been used to provide boundary conditions for the RCA4 runs presented here. Transient climate response (TCR) is defined as the immediate temperature change after a doubling of atmospheric CO2 (Cubash et al., 2001). The rightmost column indicates which RCP scenarios that have been run (2 – RCP4.5 and 8.5, 3 – RCP 2.6, 4.5 and 8.5).
| No | Modelling centre | Model name | References | TCR (°C) | RCP |
|---|---|---|---|---|---|
| 1 | Canadian Centre for Climate Modelling and Analysis | CanESM2 | Chylek et al. (2011) | 2.4 | 2 |
| 2 | Centre National de Recherches Météorologiques/Centre Européen de Recherche et Formation Avancée en Calcul Scientifique | CNRM-CM5 | Voldoire et al. (2012) | 2.1 | 2 |
| 3 | EC-EARTH consortium | EC-EARTH | Hazeleger et al. (2010) | 2.0 | 3 |
| 4 | NOAA Geophysical Fluid Dynamics Laboratory | GFDL-ESM2M | Dunne et al. (2012) | 1.3 | 2 |
| 5 | Met Office Hadley Centre | HadGEM2-ES | Collins et al. (2011) | 2.5 | 3 |
| 6 | Institut Pierre-Simon Laplace | IPSL-CM5A-MR | Dufresne et al. (2013) | 2.0 | 2 |
| 7 | Atmosphere and Ocean Research Institute (The University of Tokyo), National Institute for Environmental Studies and Japan Agency for Marine-Earth Science and Technology | MIROC5 | Watanabe et al. (2011) | 1.5 | 2 |
| 8 | Max Planck Institute for Meteorology | MPI-ESM-LR | Popke et al. (2013) | 2.0 | 3 |
| 9 | Norwegian Climate Centre | NorESM1-M | Bentsen et al. (2013) | 1.4 | 2 |