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clipped from www.agu.org
The growth of crops represents a sink of atmospheric CO2, whereas biomass is consumed by humans and housed animals, yielding respiratory sources of CO2. This process induces a lateral displacement of carbon and creates geographic patterns of CO2 sources and sinks at the surface of the globe.
The CO2 flux maps show regional dipoles of sources and sinks in Asia and North America.
The mean latitudinal CO2 gradients induced by the displacement of crop products are fairly small
indicating that this process has a only a small influence in explaining the latitudinal distribution of CO2 fluxes.
On the other hand, the simulated longitudinal mean atmospheric CO2 gradients at northern midlatitudes (≈ up to 0.5 ppm) are comparable to the ones measured between atmospheric stations, suggesting that CO2 fluxes from crop products trade are an important component of continental- and regional-scale CO2 budgets.
Thus they should be accounted for as prior information in regional inversions.
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