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Biogeosciences An interactive open-access journal of the European Geosciences Union
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Volume 12, issue 3
Biogeosciences, 12, 835–844, 2015
https://doi.org/10.5194/bg-12-835-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: 9th International Carbon Dioxide Conference (ICDC9) (ESD/ACP/AMT/BG...

Biogeosciences, 12, 835–844, 2015
https://doi.org/10.5194/bg-12-835-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 11 Feb 2015

Research article | 11 Feb 2015

Recent changes in the global and regional carbon cycle: analysis of first-order diagnostics

P. J. Rayner1, A. Stavert2, M. Scholze3, A. Ahlström3, C. E. Allison2, and R. M. Law2 P. J. Rayner et al.
  • 1School of Earth Sciences, University of Melbourne, Melbourne, Australia
  • 2CSIRO Oceans and Atmosphere Flagship, Melbourne, Australia
  • 3Department of Physical Geography and Ecosystem Science, Lund University, Sweden

Abstract. We analyse global and regional changes in CO2 fluxes using two simple models, an airborne fraction of anthropogenic emissions and a linear relationship with CO2 concentrations. We show that both models are able to fit the non-anthropogenic (hereafter natural) flux over the length of the atmospheric concentration record. Analysis of the linear model (including its uncertainties) suggests no significant decrease in the response of the natural carbon cycle. Recent data points rather to an increase. We apply the same linear diagnostic to fluxes from atmospheric inversions. Flux responses show clear regional and seasonal patterns driven by terrestrial uptake in the northern summer. Ocean fluxes show little or no linear response. Terrestrial models show clear responses, agreeing globally with the inversion responses, however the spatial structure is quite different, with dominant responses in the tropics rather than the northern extratropics.

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Recent papers suggest a slow-down in the natural uptake of anthropogenic CO2. We analyse recent trends in atmospheric concentration and known inputs to test for such a slow-down. We see, rather, an increase in uptake compared to a simple response to changing CO2 concentration. Using atmospheric models and statistical techniques we isolate this increased uptake to the northern temperate and boreal continents during summer, suggesting a stronger growing season.
Recent papers suggest a slow-down in the natural uptake of anthropogenic CO2. We analyse recent...
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