We upscaled AmeriFlux tower data to the conterminous United Stateswith and without considering the atmospheric CO2.
GPP/NEE difference between two models exhibits a great spatial and seasonal variability and an annual difference of 200 g C m−2 yr−1.
Air temperature played an important role in determining the atmospheric CO2 effects on carbon fluxes.
The simulation without considering CO2 effects failed to detect ecosystem responses to droughts in part of the US in 2006.
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