This simulation was performed with the first version of the coupled global model CGCMI with the standard concentration of CO2. Details of the model and an analysis of the simulation are given in Flato
This simulation was performed with the first version of the coupled global model CGCMI. The model is forced by an effective greenhouse forcing corresponding to that observed from 1850 to the present,
(member 1 of 3 ensemble simulations, the original) This ensemble of 3 simulations was performed with the first version of the coupled global model CGCMI. The model is forced by an effective greenhouse
(member 2 of 3 ensemble simulations, the original) This ensemble of 3 simulations was performed with the first version of the coupled global model CGCMI. The model is forced by an effective greenhouse
(member 3 of 3 ensemble simulations, the original) This ensemble of 3 simulations was performed with the first version of the coupled global model CGCMI. The model is forced by an effective greenhouse
The control integration, in which the atmospheric forcing is kept constant, simulates a period over 240 years (1860-2099) in length. Control experiment (CTL): The control integration, in which the atmospheric
Here the greenhouse gas forcing is increased gradually to represent the observed changes in forcing due to all the greenhouse gases from 1881 to 1990. From 1990 to 2100 it uses an increase in concentrations
The forcing includes not only the greenhouse gas forcing described with the "greenhouse run" but also the direct radiative effect of sulphate aerosol concentrations. The direct aerosol effect was included
The atmosphere-ocean general circulation model ECHAM3/LSG is used for climate change and climate variability studies. The control integration, in which the atmospheric forcing is kept constant, simulates
The atmosphere-ocean general circulation model ECHAM3/LSG is used for climate change and climate variability studies. For this climate change integration, the CO2 concentration from 1880 to 2084 were
The atmosphere-ocean general circulation model ECHAM3/LSG is used for climate change and climate variability studies. Up to 1985 the concentration followswere taken from observation (Schoenwiese et al.,
The atmosphere-ocean general circulation model ECHAM3/LSG is used for climate change and climate variability studies. Up to 1985 the concentration followswere taken from observation (Schoenwiese et al.,
The control integration, in which the atmospheric forcing is kept constant, simulates a period of 1000 years. The value of CO2 in the whole run is approximately equal to the value observed in 1958 (this
The control integration, in which the atmospheric forcing is kept constant, simulates a period of 100 years. The value of CO2 in the whole run is approximately equal to the value observed in 1958 (this
The value of CO2 increases gradually from the initial value (approximately equal to the value observed in 1958). The rate of 1% per year increase in CO2 is approximately equal to the rate of total radiative