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Global climate simulations at 3000-year intervals for the last 21 000 years with the GENMOM coupled atmosphere–ocean model

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Figure

Table 1. Atmospheric greenhouse gas concentrations for each time185 ppmV and 350 and 200 ppbV for 21 ka
Figure 1. Boundary conditions for the time slice simulations. COconcentrations are relative to the PI concentration of 280 ppmV
Figure 2. Orography for the time slice simulations, with ice sheet height and extent derived from ICE-4G (Peltier, 2002) for the Fennoscan-dian, Cordilleran, and Antarctic, and OSU-LIS (Licciardi et al., 1998) for the Laurentide.
Figure 5. Simulated and reconstructed changes in temperature from 21 ka to present.The 1value rather than the original 1961–1990
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