Contributions from photosynthesis and other natural components of the carbon
cycle present the largest uncertainties in our understanding of carbon dioxide
(CO$_2$) sources and sinks. While the global spatiotemporal distribution of the
net flux (the sum of all contributions) can be inferred from atmospheric CO$_2$
concentrations through flux inversion, attributing the net flux to its
individual components remains challenging. The advent of solar-induced
fluorescence (SIF) satellite observations provides an opportunity to isolate
natural components by anchoring gross primary productivity (GPP), the
photosynthetic component of the net flux. Here, we introduce a novel
statistical flux-inversion framework that simultaneously assimilates
observations of SIF and CO$_2$ concentration, extending WOMBAT v2.0 (WOllongong
Methodology for Bayesian Assimilation of Trace-gases, version 2.0) with a
hierarchical model of spatiotemporal dependence between GPP and SIF processes.
We call the new framework WOMBAT v2.S, and we apply it to SIF and CO$_2$ data
from NASA's Orbiting Carbon Observatory-2 (OCO-2) satellite and other
instruments to estimate natural fluxes over the globe during a recent six-year
period. In a simulation experiment that matches OCO-2's retrieval
characteristics, the inclusion of SIF improves accuracy and uncertainty
quantification of component flux estimates. Comparing estimates from WOMBAT
v2.S, v2.0, and the independent FLUXCOM initiative, we observe that linking GPP
to SIF has little effect on net flux, as expected, but leads to spatial
redistribution and more realistic seasonal structure in natural flux
components.<p></p>