September

Figure 7. Difference of the 10-year mean simulated 2m air temperature, in °C, for September between the ECHAM-4 simulation with modified soil water capacity based on the fAPAR assimilation with the BETHY land surface and vegetation model minus the ECHAM-4 control simulation using standard soil water capacity. Changes in southern Arctic due to a high variability of sea ice cover are not significant

Figure 7. Difference of the 10-year mean simulated 2m air temperature, in °C, for September between the ECHAM-4 simulation with modified soil water capacity based on the fAPAR assimilation with the BETHY land surface and vegetation model minus the ECHAM-4 control simulation using standard soil water capacity. Changes in southern Arctic due to a high variability of sea ice cover are not significant

Figure 8. Seasonal cycle of 2m air temperature (a) and precipitation (b) for a portion of southern Africa, from the ECHAM-4 control simulation and the simulation with modified soil water capacity, both compared to the climatologies of Legates and Willmott [1990a, b]
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