“…Top-down methods infer quantitative information on surface CO 2 fluxes from variations in atmospheric CO 2 concentrations through inverse modeling with atmospheric tracer transport models (Ciais et al, 2011), and may include isotope composition measurements to identify fossil fuel sources (Levin et al, 2003;Miller et al, 2012;Turnbull et al, 2015;Basu et al, 2016). Uncertainties in atmospheric transport models (Peylin et al, 2002;Lauvaux et al, 2009;Peylin et al, 2011;Isaac et al, 2014), limited density of atmospheric measurements (Gerbig et al, 2009;Turner et al, 2016) and uncertainties in prior fluxes (Peylin et al, 2005;Carouge et al, 2010;Lauvaux et al, 2016) all constitute sources of error in this method (Engelen et al, 2002).…”