Global CO<sub>2</sub> fluxes estimated from GOSAT retrievals of total column CO<sub>2</sub>

We present one of the first estimates of the global distribution of CO<sub>2</sub> surface fluxes using total column CO<sub>2</sub> measurements retrieved by the SRON-KIT RemoTeC algorithm from the Greenhouse gases Observing SATellite (GOSAT). We derive optimized fluxes from...

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Main Authors: 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, D. Worthy
Format: Article
Language:English
Published: Copernicus Publications 2013-09-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/13/8695/2013/acp-13-8695-2013.pdf
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author 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
D. Worthy
author_facet 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
D. Worthy
author_sort S. Basu
collection DOAJ
description We present one of the first estimates of the global distribution of CO<sub>2</sub> surface fluxes using total column CO<sub>2</sub> 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 CO<sub>2</sub> measurements to use as baselines for comparing GOSAT data-derived fluxes. Assimilating only GOSAT data, we can reproduce the observed CO<sub>2</sub> time series at surface and TCCON sites in the tropics and the northern extra-tropics. In contrast, in the southern extra-tropics GOSAT X<sub>CO<sub>2</sub></sub> 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<sub>CO<sub>2</sub></sub> 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 CO<sub>2</sub> yields plausible global flux estimates which are more tightly constrained than in an inversion using surface CO<sub>2</sub> data alone. We show that assimilating the bias-corrected GOSAT data on top of surface CO<sub>2</sub> data (a) reduces the estimated global land sink of CO<sub>2</sub>, and (b) shifts the terrestrial net uptake of carbon from the tropics to the extra-tropics. It is concluded that while GOSAT total column CO<sub>2</sub> 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.
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spelling doaj.art-631ac7a731614964b4640a679683bb0d2022-12-21T22:40:11ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242013-09-0113178695871710.5194/acp-13-8695-2013Global CO<sub>2</sub> fluxes estimated from GOSAT retrievals of total column CO<sub>2</sub>S. BasuS. GuerletA. ButzS. HouwelingO. HasekampI. AbenP. KrummelP. SteeleR. LangenfeldsM. TornS. BiraudB. StephensA. AndrewsD. WorthyWe present one of the first estimates of the global distribution of CO<sub>2</sub> surface fluxes using total column CO<sub>2</sub> 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 CO<sub>2</sub> measurements to use as baselines for comparing GOSAT data-derived fluxes. Assimilating only GOSAT data, we can reproduce the observed CO<sub>2</sub> time series at surface and TCCON sites in the tropics and the northern extra-tropics. In contrast, in the southern extra-tropics GOSAT X<sub>CO<sub>2</sub></sub> 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<sub>CO<sub>2</sub></sub> 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 CO<sub>2</sub> yields plausible global flux estimates which are more tightly constrained than in an inversion using surface CO<sub>2</sub> data alone. We show that assimilating the bias-corrected GOSAT data on top of surface CO<sub>2</sub> data (a) reduces the estimated global land sink of CO<sub>2</sub>, and (b) shifts the terrestrial net uptake of carbon from the tropics to the extra-tropics. It is concluded that while GOSAT total column CO<sub>2</sub> 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.http://www.atmos-chem-phys.net/13/8695/2013/acp-13-8695-2013.pdf
spellingShingle 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
D. Worthy
Global CO<sub>2</sub> fluxes estimated from GOSAT retrievals of total column CO<sub>2</sub>
Atmospheric Chemistry and Physics
title Global CO<sub>2</sub> fluxes estimated from GOSAT retrievals of total column CO<sub>2</sub>
title_full Global CO<sub>2</sub> fluxes estimated from GOSAT retrievals of total column CO<sub>2</sub>
title_fullStr Global CO<sub>2</sub> fluxes estimated from GOSAT retrievals of total column CO<sub>2</sub>
title_full_unstemmed Global CO<sub>2</sub> fluxes estimated from GOSAT retrievals of total column CO<sub>2</sub>
title_short Global CO<sub>2</sub> fluxes estimated from GOSAT retrievals of total column CO<sub>2</sub>
title_sort global co sub 2 sub fluxes estimated from gosat retrievals of total column co sub 2 sub
url http://www.atmos-chem-phys.net/13/8695/2013/acp-13-8695-2013.pdf
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