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).