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. 2005 Oct 24;360(1463):2049–2065. doi: 10.1098/rstb.2005.1739

Figure 12.

Figure 12

Changes in terrestrial carbon storage simulated over the twenty-first century and the implications for CO2 rise and climate change, from simulations with the HadCM3LC coupled climate–carbon cycle model driven by the IS92a emissions scenario (Cox et al. 2000). (a) Time-series of changes in global mean vegetation carbon (black) and soil carbon (grey) (Gt C) relative to 1860, in the fully coupled climate–carbon cycle simulation. (b) CO2 rise (ppmv) simulated as a result of the IS92a emissions scenario, with the effects of climate change on land and ocean carbon fluxes included (black) and excluded (grey). (c) Global land mean temperature rise (°C) relative to 1860, with CO2 simulated including climate–carbon cycle feedbacks (black) and with CO2 imposed from projections which exclude climate–carbon cycle feedbacks (grey).