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. 2017 Oct 19;7:13567. doi: 10.1038/s41598-017-13459-0

Table 1.

Global total CO2 fluxes used in the 3 ACTM simulations (column 2–6), and estimated flux corrections (column 7–10) for different time windows given in column 1 (Units: PgC). Note here that these values are not strictly mass balanced as the XCO2 differences are weighted by area of the 3 latitude bands, without knowing whether the mismatches at high latitudes in particular extend to the poles on either side.

Time window A priori CO2 fluxes used for ACTM simulations Patra et al.# (2005b) CO2 flux corrections from OCO-2 – ACTM differences$
FFC CYC64 IAV84 IAV84 + GFAS GFAS CYC64 IAV84 IAV84 + GFAS
Oct 2014–Sep 2015 9.93 −2.86 −6.24 −4.27 1.97 2.67–2.73 −0.1–0.23 1.17–2.04 0.41–0.71
Oct 2015–Sep 2016 10.12 −2.86 −6.24 −5.57 0.67 −0.75–1.10 1.00–1.16 0.53–0.67
Jul 2015–Jun 2016 (main El Niño period) 10.08 −2.86 −6.24 −4.77 1.46 −0.18–0.29 1.50–2.18 0.77–1.09

#Range estimated from two different fits, with (Flux anomaly = 0.3539 + 1.4935 × MEI amplitude change) or without (=−1.0756 + 2.4579 × MEI amplitude change) the La Niña years.

$Range of estimation using two different approximations on area coverage (lower: latitudes covered by measurements; higher: global; refer to the main text for details).