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Early-Holocene warming in Beringia and its mediation by sea-level and vegetation changes

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Figure

Figure 1. Spatial domain of RegCM for this study showing elevations and coastlines for 0 ka (a) and 11 ka (b)
Figure 2. Monthly insolation at present (0 ka), 6 and 11 ka afterBerger (1978; upper); insolation differences between present and 6and 11 ka (middle); month-length differences between present and 6and 11 ka (lower)
Table 1. Simulation boundary conditions and land cover.
Figure 4. combines all three experimental land-cover changes. Eachland-cover map is linked to a RegCM simulation; an additional simulation was made using modern land cover with 11 ka continental outlines200 400 800  11 ka All (f) 6 ka simulation; there are
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