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A. Anav, P. Friedlingstein, M. Kidston, L. Bopp, P. Ciais, P. Cox, C. Jones, M. Jung, R. Myneni, and Z. Zhu

[discussed in section 2b(6) ]. To avoid pitfalls arising from weak data constraints, most inversion studies have relied on regularization techniques that include the aggregation of estimate fluxes over large regions ( Engelen et al. 2002 ); as a matter of fact, aggregating the observed regional fluxes in space is one way to lower the uncertainty due to the limited observational constraint ( Kaminski et al. 2001 ; Engelen et al. 2002 ). Therefore, we only evaluate the net CO 2 fluxes simulated by

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