Recent pause in the growth rate of atmospheric CO2 due to enhanced terrestrial carbon uptake

Terrestrial ecosystems play a significant role in the global carbon cycle and offset a large fraction of anthropogenic CO 2 emissions. The terrestrial carbon sink is increasing, yet the mechanisms responsible for its enhancement, and implications for the growth rate of atmospheric CO 2 , remain uncl...

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Published inNature communications Vol. 7; no. 1; p. 13428
Main Authors Keenan, Trevor F, Prentice, I. Colin, Canadell, Josep G, Williams, Christopher A, Wang, Han, Raupach, Michael, Collatz, G. James
Format Journal Article
LanguageEnglish
Published London Nature Publishing Group UK 08.11.2016
Nature Publishing Group
Nature Portfolio
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Summary:Terrestrial ecosystems play a significant role in the global carbon cycle and offset a large fraction of anthropogenic CO 2 emissions. The terrestrial carbon sink is increasing, yet the mechanisms responsible for its enhancement, and implications for the growth rate of atmospheric CO 2 , remain unclear. Here using global carbon budget estimates, ground, atmospheric and satellite observations, and multiple global vegetation models, we report a recent pause in the growth rate of atmospheric CO 2 , and a decline in the fraction of anthropogenic emissions that remain in the atmosphere, despite increasing anthropogenic emissions. We attribute the observed decline to increases in the terrestrial sink during the past decade, associated with the effects of rising atmospheric CO 2 on vegetation and the slowdown in the rate of warming on global respiration. The pause in the atmospheric CO 2 growth rate provides further evidence of the roles of CO 2 fertilization and warming-induced respiration, and highlights the need to protect both existing carbon stocks and regions, where the sink is growing rapidly. Year-to-year variability in atmospheric CO 2 is strongly influenced by the terrestrial biosphere. Despite increasing anthropogenic emissions, Keenan et al . report a recent pause in the growth rate of atmospheric CO 2 using observations and vegetation models, attributed to an enhanced terrestrial carbon sink.
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AC02-05CH11231; FG02-04ER63917; FG02-04ER63911; SC0006708
USDOE Office of Science (SC), Biological and Environmental Research (BER)
Deceased.
ISSN:2041-1723
2041-1723
DOI:10.1038/ncomms13428