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Showing content from https://doi.org/10.5194/acp-13-8695-2013 below:

Global CO2 fluxes estimated from GOSAT retrievals of total column CO2

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03 Sep 2013

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S. Basu, S. Guerlet, A. Butz, S. Houweling, O. Hasekamp, I. Aben, P. Krummel, P. Steele, R. Langenfelds, M. Torn, S. Biraud, B. Stephens, A. Andrews, and D. Worthy

We present one of the first estimates of the global distribution of CO₂ surface fluxes using total column CO₂ measurements retrieved by the SRON-KIT RemoTeC algorithm from the Greenhouse gases Observing SATellite (GOSAT). We derive optimized fluxes from June 2009 to December 2010. We estimate fluxes from surface CO₂ measurements to use as baselines for comparing GOSAT data-derived fluxes. Assimilating only GOSAT data, we can reproduce the observed CO₂ time series at surface and TCCON sites in the tropics and the northern extra-tropics. In contrast, in the southern extra-tropics GOSAT X_CO2 leads to enhanced seasonal cycle amplitudes compared to independent measurements, and we identify it as the result of a land–sea bias in our GOSAT X_CO2 retrievals. A bias correction in the form of a global offset between GOSAT land and sea pixels in a joint inversion of satellite and surface measurements of CO₂ yields plausible global flux estimates which are more tightly constrained than in an inversion using surface CO₂ data alone. We show that assimilating the bias-corrected GOSAT data on top of surface CO₂ data (a) reduces the estimated global land sink of CO₂, and (b) shifts the terrestrial net uptake of carbon from the tropics to the extra-tropics. It is concluded that while GOSAT total column CO₂ provide useful constraints for source–sink inversions, small spatiotemporal biases – beyond what can be detected using current validation techniques – have serious consequences for optimized fluxes, even aggregated over continental scales.

Received: 30 Nov 2012 – Discussion started: 18 Feb 2013 – Revised: 16 Jun 2013 – Accepted: 09 Jul 2013 – Published: 03 Sep 2013

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