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Holocene land-cover reconstructions for studies on land cover-climate feedbacks

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Figure

Fig. 1. Decrease in mean global temperature over the Northern Hemisphere due to the biophysical feedback (increased albedo) of anGaillard et al
Fig. 2. Reconstructions of the spatial extent of permanent and non-permanent agriculture for seven time slices of the Holocene (modified from Olofsson and Hickler, 2008)
Fig. 3. Fractional crop cover at 5000 BC (left) and 2000 BC (right) simulated by the Global Land use and Technological Evolution Simulator(GLUES, Lemmen, 2009).
Fig. 4. Anthropogenic land use in Europe and surrounding areas at AD 800 simulated by four different modelling approaches:Environment] database version 3.1 (Klein Goldewijk et al., 2010);Kaplan et al
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