Land and ocean carbon cycle feedback effects on global warming in a simpleEarth system model

A simple Earth system model is developed by coupling a box model of the glo bal carbon cycle to an energy-balance approximation of global temperature. The model includes a range of feedback mechanisms between atmospheric CO2, surface temperature and land and ocean carbon cycling. It is used to assess their effect on the global change being driven by anthropogenic CO2 emissi ons from fossil fuel burning and land-use change. When tuned to reach the 1 990 level of atmospheric CO2, the model CO2 predictions for 1832-1990 are r easonably close to ice-core and instrumental records, observed global warmi ng of similar to0.6 K from 1860-1990 is accurately predicted and the land a nd ocean carbon sinks for the 1980s are close to IPCC central estimates. Th e ocean sink is reduced by similar to0.3 GtC yr(-1) when the ocean surface is assumed to warm at the same rate as global surface temperature. Land and oceanic carbon sinks are predicted to be growing at present and hence buff ering the rate of rise of atmospheric CO2. In the basic model, the current land carbon sink is assumed to be due to CO2 fertilisation of photosynthesi s. The slight warming that has occurred enhances soil respiration (carbon l oss) and net primary productivity (carbon uptake) by similar amounts. When the model is forced with a "business as usual" (IS92a) emissions scenario f or 1990-2100 followed by a linear decline in emissions to zero at 2200, CO2 reaches a peak of 985 ppmv in 2170 and temperature peaks at +5.5 K in 2180 . Peak CO2 is similar to 135 ppmv higher than suggested by IPCC for the sam e forcing, principally because global warming first suppresses the land car bon sink then generates a land carbon source. When warming exceeds similar to4.5 K, soil respiration "overtakes" the CO2 fertilisation of NPP, trigger ing a release of similar to 70 GtC from terrestrial ecosystems over similar to 100 years. When the effects of temperature on photosynthesis, respirati on and soil respiration are removed, peak levels of CO2 are reduced by simi lar to 100 ppmv and peak temperature by similar to0.5 K. Distinguishing sep arate soil carbon pools with different residence times does not significant ly alter the timing of the switch to a land carbon source or its effect on peak CO2, but it causes the source to persist for longer. If forest re-grow th or nitrogen deposition are assumed to contribute to the current land car bon sink, this implies a weaker CO2 fertilisation effect on photosynthesis and generates a larger future carbon source. Peak CO2 levels are also sensi tive by about +/- 80 ppmv to upper and lower limits on the temperature resp onses of photosynthesis, plant respiration and soil respiration. By forcing the model with a range of future emission scenarios it is found that the c reation of a significant land carbon source requires rapid warming, exceedi ng similar to4.5 K, and its magnitude increases with the rate of forcing. T he carbon source is greatest for the most rapid burning of the largest rese rve of fossil fuel. It is concluded that carbon loss from terrestrial ecosy stems may significantly(similar to 10%) amplify global warming under "busin ess as usual" or more extreme scenarios.