Figure: Change in annual mean surface temperature (K) (a) in simulation with a completely deforested world (GRASS) relative to a simulation with the current forest area (FOREST) and (b) reconstructed as the sum of the effects of change in albedo, evapotranspiration efficiency and roughness.
Reference: E. Davin and N. de Noblet-Ducoudré, 2010. Climatic impact of global-scale deforestation: radiative versus non-radiative processes. Journal of Climate, 23:97-112.