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. 2018 Apr 10;218(4):1462–1477. doi: 10.1111/nph.15100

Figure 5.

Figure 5

Simulated change in global land carbon over the study period in (a, d, g) Ctrl, (b, e, h) Geog and (c, f, i) Geog+Acclim for 22 global climate models (GCMs) as a function of the change in regional land surface temperature over the study period (ΔT). Rows represent regions: tropical (30°N < Lat < 30°S), temperate (60°N > Lat > 30°N and 60°S > Lat > 30°S) and boreal and tundra (60°S < Lat > 60°N). Note the differences in y‐axis scales.