Model Name | Modelling Centre | |
ACCESS-CM2 | CSIRO-ARCCSS (Commonwealth Scientific and Industrial Research Organisation, Aspendale, Victoria 3195, Australia, Australian Research Council Centre of Excellence for Climate System Science) | Australian Community Climate and Earth System Simulator Climate Model Version 2 |
ACCESS-ESM1-5 | CSIRO | Australian Community Climate and Earth System Simulator Earth System Model Version 1.5 |
AWI-CM-1-1-MR | AWI |
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AWI-ESM-1-1-LR | AWI |
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BCC-CSM2-MR | BCC |
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BCC-ESM1 | BCC |
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CAMS-CSM1-0 | CAMS |
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CanESM5 | CCCma |
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CanESM5-CanOE | CCCma |
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CAS-ESM2-0 | CAS |
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CESM2 | NCAR | The Community Earth System Model version 2 (CESM2) is a state-of-the-art coupled model that includes ocean, wave, land, land-ice, sea-ice, and river runoff models as well as both low-top and high-top full chemistry versions of atmopsheric models. The model also includes biogeochemistry. |
CESM2-FV2 | NCAR |
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CESM2-WACCM | NCAR |
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CESM2-WACCM-FV2 | NCAR |
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CIESM | THU |
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CMCC-CM2-SR5 | CMCC |
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CNRM-CM6-1 | CNRM-CERFACS |
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CNRM-CM6-1-HR | CNRM-CERFACS |
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CNRM-ESM2-1 | CNRM-CERFACS |
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E3SM-1-0 | E3SM-Project LLNL |
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E3SM-1-1 | E3SM-Project RUBISCO | E3SM 1.1 (Energy Exascale Earth System Model) |
E3SM-1-1-ECA | E3SM-Project | E3SM 1.1 (Energy Exascale Earth System Model) with an experimental land BGC ECA configuration |
EC-Earth3 | EC-Earth-Consortium | The atmosphere-ocean general circulation model is described by Doescher-et-al-2020. The atmosphere is a modified version of IFS cycle 36r4, and includes the land-surface scheme H-TESSEL. The ocean and sea-ice model is NEMO-LIM3 version 3.6 with a few modifications. The OASIS3-MCT coupler version 3.0 is used to exchange fields between the atmosphere and ocean components. |
EC-Earth3-LREC-Earth3-LR | EC-Earth-Consortium |
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EC-Earth3-Veg | EC-Earth-Consortium |
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EC-Earth3-Veg-LR | EC-Earth-Consortium |
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FGOALS-f3-L | CAS |
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FGOALS-g3 | CAS |
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FIO-ESM-2-0 | FIO-QLNM |
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GFDL-AM4 | NOAA-GFDL | GFDL-CM4 | NOAA-GFDL | GFDL-ESM4 | NOAA-GFDL | This is the Atmosphere and Land component (AM4.0.1) of GFDL coupled model CM4.0 for use in CMIP6. The Atmospheric component is identifical to the AM4.0 model documented in Zhao et. al (2018a, 2018b). The vegetation, land and glacier models differ from AM4.0 in the following aspects: 1) dynamical vegetation was used instead the static vegetation used in AM4.0. 2) glacier albedo is retuned. 3) other minor tuning in the land model. |
GFDL-CM4 | NOAA-GFDL | This is the GFDL physical coupled model CM4.0 for use in CMIP6. The model is documented in Held et al (2019) |
GFDL-ESM4 | NOAA-GFDL |
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GISS-E2-1-G | GISS-E2-1-G | NASA-GISS |
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GISS-E2-1-H | NASA-GISS |
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GISS-E2-2-G | NASA-GISS |
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HadGEM3-GC31-LL | MOHC NERC | HadGEM3Aerosol2: UKCA-GC31-MM | MOHC | IITM-ESM | CCCR-IITM | INM-CM4-8 | INM | INM-CM5-0 | INM | IPSL-CM6A-LR | IPSL | KACE-1-0-G | NIMS-KMA | KIOST-ESM | KIOST | MCM-UA-1-0 | UA | GLOMAP-mode, atmos: MetUM-HadGEM3-GA7.1 (N96;192 x 144 longitude/latitude; 85 levels; top level 85km), atmosChem: none, land: JULES-HadGEM3-GL7.1, landIce: none, ocean: NEMO-HadGEM3-GO6.0 (ORCA1 tripolar primarily 1 deg latitude/longitude with meridional refinement down to 1/3 deg in tropics; 400 x 180 longitude/latitude; 75 levels; top grid cell 0-1m), ocnBgchem: none, seaIce: CICE-HadGEM3-GSI8 (ORCA1 tripolar primarily 1 deg; 360 x 180 longitude/latitude). |
HadGEM3-GC31-MM | MOHC |
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IITM-ESM | CCCR-IITM |
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INM-CM4-8 | INM |
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INM-CM5-0 | INM |
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IPSL-CM6A-LR | IPSL |
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KACE-1-0-G | NIMS-KMA |
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KIOST-ESM | KIOST |
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MCM-UA-1-0 | UA | R30 spectral atmosphere coupled to MOM1 ocean using simple Manabe land model and simple Bryan sea ice model. |
MIROC6 | MIROC | MIROC6 is a physical climate model mainly composed of three sub-models: atmosphere, land, and sea ice-ocean. The atmospheric model is based on the CCSR-NIES atmospheric general circulation model. The horizontal resolution is a T85 spectral truncation that is an approximately 1.4° grid interval for both latitude and longitude. The vertical grid coordinate is a hybrid σ-p coordinate. The model top is placed at 0.004 hPa, and there are 81 vertical levels. The Spectral Radiation-Transport Model for Aerosol Species (SPRINTARS) is used as an aerosol module for MIROC6 to predict the mass mixing ratios of the main tropospheric aerosols. By coupling the radiation and cloud-precipitation schemes, SPRINTARS calculates not only the aerosol transport processes but also the aerosol-radiation and aerosol-cloud interactions.The land surface model is based on Minimal Advanced Treatments of Surface Interaction and Runoff (MATSIRO), which includes a river routing model based on a kinematic wave flow equation and a lake module where one-dimensional thermal diffusion and mass conservation are considered. The horizontal resolution of the land surface model is the same as that of the atmopheric component. There are a three-layers snow and a six-layers soil down to a 14 m depth.The sea ice-ocean model is based on the CCSR Ocean Component model (COCO). The tripolar horizontal coordinate system is adopted, and the longitudinal grid spacing is 1° and the meridional grid spacing varies from about 0.5° near the equator to 1° in the mid-latitudes. There are 62 vertical levels in a hybrid σ-z coordinate system. A coupler system calculates heat and freshwater fluxes between the sub-models in order to ensure that all fluxes are conserved within machine precision and then exchanges the fluxes among the sub-models. No flux adjustments are used in MIROC6. |
MIROC-ES2L | MIROC | MIROC-AGCM is the atmospheric component of a climate model, the Model for Interdisciplinary Research on Climate version 6 (MIROC6). The MIROC-AGCM employs a spectral dynamical core, and standard physical parameterizations for cumulus convections, radiative transfer, cloud microphysics, turbulence, and gravity wave drag. It also has an aerosol module. The model is cooperatively developed by the Japanese modeling community including the Atmosphere and Ocean Research Institute, the University of Tokyo, the Japan Agency for Marine-Earth Science and Technology, and the National Institute for Environmental Studies. |
MPI-ESM-1-2-HAM | HAMMOZ-Consortium |
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MPI-ESM1-2-HR | MPI-M DWD DKRZ |
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MPI-ESM1-2-LR | MPI-M AWI |
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MRI-ESM2-0 | MRI |
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NESM3 | NUIST |
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NorCPM1 | NCC |
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NorESM1-F | NCC |
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NorESM2-LM | NCC |
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NorESM2-MM | NCC |
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SAM0-UNICON | SNU | The atmospheric component of SEM0 is the Seoul National University Atmospheric Model Version 0 with a Unified Convection Scheme (SAM0-UNICON, Park et al. 2019, Park 2014a,b), which replaces CAM5's shallow and deep convection schemes and revises CAM5's cloud macrophysics scheme (Park et al. 2017). The other components of SEM0 (i.e., ocean, land, land-ice, sea-ice, and coupler) are identical to those of the Community Earth System Model version 1.2 (CESM1.2). | MIROC6 | MIROC | MIROC-ES2L | MIROC | MPI-ESM-1-2-HAM | HAMMOZ-Consortium | MPI-ESM1-2-HR | MPI-M DWD DKRZ | MPI-ESM1-2-LR | MPI-M AWI | MRI-ESM2-0 | MRI | NESM3 | NUIST | NorCPM1 | NCC | NorESM1-F | NCC | NorESM2-LM | NCC | NorESM2-MM | NCC | SAM0-UNICON | SNU |
TaiESM1 | AS-RCEC |
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UKESM1-0-LL | MOHC, NERC, NIMS-KMA, NIWA |
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