Atmospheric verification of anthropogenic CO2 emission trends

Author:  ["Roger J. Francey","Cathy M. Trudinger","Marcel van der Schoot","Rachel M. Law","Paul B. Krummel","Ray L. Langenfelds","L. Paul Steele","Colin E. Allison","Ann R. Stavert","Robert J. Andres","Christian Rödenbeck"]

Publication:  Nature Climate Change

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Tags:     Climate environment

Abstract

International efforts to limit global warming and ocean acidification aim to slow the growth of atmospheric CO2, guided primarily by national and industry estimates of production and consumption of fossil fuels. Atmospheric verification of emissions is vital but present global inversion methods are inadequate for this purpose. We demonstrate a clear response in atmospheric CO2 coinciding with a sharp 2010 increase in Asian emissions but show persisting slowing mean CO2 growth from 2002/03. Growth and inter-hemispheric concentration difference during the onset and recovery of the Global Financial Crisis support a previous speculation that the reported 2000–2008 emissions surge is an artefact, most simply explained by a cumulative underestimation (∼ 9 Pg C) of 1994–2007 emissions; in this case, post-2000 emissions would track mid-range of Intergovernmental Panel on Climate Change emission scenarios. An alternative explanation requires changes in the northern terrestrial land sink that offset anthropogenic emission changes. We suggest atmospheric methods to help resolve this ambiguity. There is a widespread assumption that changes in reported anthropogenic global CO2 emissions are indicative of changes in climate and ocean chemistry. However, examination of atmospheric CO2 measurements from the past two decades challenges this idea. A new study develops and advocates use of CO2 measurement practices that reduce uncertainty in atmospheric verification of emissions, and identifies modelling inadequacies.

Cite this article

Francey, R., Trudinger, C., van der Schoot, M. et al. Atmospheric verification of anthropogenic CO2 emission trends. Nature Clim Change 3, 520–524 (2013). https://doi.org/10.1038/nclimate1817

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