IPCC Antarctic GCM scenarios

Emission scenarios developed by the Intergovernmental Panel on Climate Change (IPCC) contain a set of climate forcing factors that can be used for coupled ocean-atmosphere simulations of 20th, 21st and 22nd century climate. The forcing is given in terms of solar irradiance, volcanic aerosol optical depth, anthropogenic aerosols, and atmospheric concentrations of ozone, carbon dioxide, and other well mixed greenhouse gases.

The Intergovernmental Panel on Climate Change recommends modeling groups contributing to the IPCC Fourth Assessment Report (4AR) include the following scenarios of climate forcing:

Documentation for this particular set of climate forcing factors may be found in Ammann, C.M., G.A. Meehl, W.M. Washington, and C. Zender, 2003: A monthly and latitudinally varying volcanic forcing dataset in simulations of 20th century climate. Geophys. Res. Lett., 30, doi:10.1029/2003GL016875RR, and Dai, A., T.M.L. Wigley, B.A. Boville, J.T. Kiehl, and L.E. Buja, 2001: Climates of the twentieth and twenty-first centuries simulated by the NCAR Climate System Model. J. Climate, 14, 485-519.

CO2 forcingCH4 forcing
Volcanic aerosolsSolar constant

We include output for the Antarctic region from these IPCC 4AR scenarios below:


Surface air temperature

sfc. air temperature (all models; SRESA1B)SRESAB1 sfc. air temperatures

choose an IPCC scenario below
SRESA1B composite surface air temperature

IPCC SRESA1B projected sfc. air temperature

choose a GCM below
NCAR Community Climate System Model, CCSM 3.0
Meteo-France, Centre National de Recherches Meteorolo giques, CM3 Model
NOAA Geophysical Fluid Dynamics Laboratory, CM2.0 Model
NASA Goddard Institute for Space Studies, ModelE20/Russell
CCSR/NIES/FRCGC, MIROC Model V3.2, medium resolution
Meteorological Research Institute, Japan, CGCM2.3.2a
Parallel Climate Model (Version 1)
Institute for Numerical Mathematics, Russia, INMCM3.0 Model
Max Planck Institute for Meteorology, Germany, ECHAM5 / MPI OM
Hadley Centre for Climate Prediction, Met Office, UK, HadCM3 Model
IPSL/LMD/LSCE, France, CM4 V1 Model



Precipitation

choose an IPCC scenario below
SRESA1B composite precipitation

IPCC SRESA1B projected precipitation

choose a GCM below
NCAR Community Climate System Model, CCSM 3.0
Meteo-France, Centre National de Recherches Meteorolo giques, CM3 Model
NOAA Geophysical Fluid Dynamics Laboratory, CM2.0 Model
NASA Goddard Institute for Space Studies, ModelE20/Russell
CCSR/NIES/FRCGC, MIROC Model V3.2, medium resolution
Meteorological Research Institute, Japan, CGCM2.3.2a
Parallel Climate Model (Version 1)
Institute for Numerical Mathematics, Russia, INMCM3.0 Model
Max Planck Institute for Meteorology, Germany, ECHAM5 / MPI OM
Hadley Centre for Climate Prediction, Met Office, UK, HadCM3 Model
IPSL/LMD/LSCE, France, CM4 V1 Model


Sea Level Pressure

choose an IPCC scenario below
SRESA1B composite sea level pressure

IPCC SRESA1B projected sea level pressure

choose a GCM below
NCAR Community Climate System Model, CCSM 3.0
Meteo-France, Centre National de Recherches Meteorolo giques, CM3 Model
NOAA Geophysical Fluid Dynamics Laboratory, CM2.0 Model
NASA Goddard Institute for Space Studies, ModelE20/Russell
CCSR/NIES/FRCGC, MIROC Model V3.2, medium resolution
Meteorological Research Institute, Japan, CGCM2.3.2a
Parallel Climate Model (Version 1)
Institute for Numerical Mathematics, Russia, INMCM3.0 Model
Max Planck Institute for Meteorology, Germany, ECHAM5 / MPI OM
Hadley Centre for Climate Prediction, Met Office, UK, HadCM3 Model
IPSL/LMD/LSCE, France, CM4 V1 Model


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This work supported by the National Science Foundation's Office of Polar Programs through grant OPP-02289430. This website does not necessarily reflect the views of the National Science Foundation.

Department of Atmospheric Sciences University of Illinois
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