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The importance of terrestrial weathering changes in multimillennial recovery of the global carbon cycle: a two-dimensional perspective

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Figure

Figure 1. Distribution of the six major rock types for the present day. Presented here are (a) the source data from GEM-CO2 (Amiotte Suchetet al., 2003), adapted to the resolution of UVic model, displaying only the dominant lithology in each grid cell, and
Figure 2. Pre-industrial (year 1800 CE) setup for our weathering scheme. (a) Model-simulated annual mean river runoff, which is combinedwith rock type fractions (see Fig
Figure 3. Time series of simulated changes in various globally averaged or summed model outputs for Group A scenarios, compared withpre-industrial steady-state values
Table 2. Description of each experiment carried out in this study. The emission total is the total amount of carbon emissions; the emissiontotal is divided equally among the number of time steps during the emission period
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