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The impact of carbon–climate feedback on carbon storage. (a) Difference in column inventory of dissolved inorganic carbon between experiments A2_ROL and A2_OL due to effects of changing ocean circulation and ocean biogeochemistry. The inventories are averaged over times when the atmospheric CO2 mixing ratio is 765 ppmv (i.e., 2094–2098 AD in A2_ROL and 2096–2100 in A2_OL). (b) Like a, but for terrestrial carbon inventory. Unit is gC/m2.
