Using orbiting carbon observatory-2 (oco-2) column co retrievals to rapidly detect and estimate biospheric surface carbon flux anomalies

HIGHLIGHTS

SUMMARY

A large contribution to the variability and trends of these CO2 concentrations is the uptake of carbon by the terrestrial biosphere (Ahlström et_al, 2015; Poulter et_al, 2014). The terrestrial biosphere typically acts as a sink but can become a strong source, or CO2 efflux, under climatic anomalies (Biederman et_al, 2017; Zscheischler et_al, 2014). Atmospheric transport model assimilation efforts and land surface models are often used to quantify and monitor global carbon sources and sinks (Ott et_al, 2015; Peters et_al, 2007). Specifically, such a method could allow for near real-time monitoring of the . . .

 



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