IPCC-AR3 LUGANO T106 TIME-SLICE INTEGRATION 1*CO2 of Deutsches Klimarechenzentrum. Based on the greenhouse gas experiment (GHG) which used the modified scenario IS92a ("IS95a"), two 10 year periods were
IPCC-AR3 LUGANO T106 TIME-SLICE INTEGRATION 2*CO2 of Deutsches Klimarechenzentrum Based on the greenhouse gas experiment (GHG) which used the modified scenario IS92a ("IS95a"), two 10 year periods were
Simulation of long-term anthropogenic climate change with the MPI/UW earth system model. The model was driven with emissions corresponding to the SRES A1B scenario with an exponential decay with a time-constant
Simulation of long-term anthropogenic climate change with the MPI/UW earth system model. The model was driven with emissions corresponding to the SRES A1B scenario with an exponential decay with a time-constant
Simulation of long-term anthropogenic climate change with the MPI/UW earth system model. The model was driven with emissions corresponding to the SRES A1B scenario with an exponential decay with a time-constant
Simulation of long-term anthropogenic climate change with the MPI/UW earth system model. The model was driven with emissions corresponding to the SRES A1B scenario with an exponential decay with a time-constant
Simulation of long-term anthropogenic climate change with the MPI/UW earth system model. The model was driven with emissions corresponding to the SRES A2 scenario with an exponential decay with a time-constant
Simulation of long-term anthropogenic climate change with the MPI/UW earth system model. The model was driven with emissions corresponding to the SRES A2 scenario with an exponential decay with a time-constant
Simulation of long-term anthropogenic climate change with the MPI/UW earth system model. The model was driven with emissions corresponding to the SRES A2 scenario with an exponential decay with a time-constant
Simulation of long-term anthropogenic climate change with the MPI/UW earth system model. The model was driven with emissions corresponding to the SRES B1 scenario with an exponential decay with a time-constant
Simulation of long-term anthropogenic climate change with the MPI/UW earth system model. The model was driven with emissions corresponding to the SRES B1 scenario with an exponential decay with a time-constant
Simulation of long-term anthropogenic climate change with the MPI/UW earth system model. The model was driven with emissions corresponding to the SRES B1 scenario with an exponential decay with a time-constant
Simulation of long-term anthropogenic climate change with the MPI/UW earth system model. Long-term stabilization of the atmospheric pCO2 simulations. The atmospheric pCO2 is prescribed to rise exponentially