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Declining uncertainty in transient climate response as CO2 forcing dominates future climate change

Nature Geoscience volume 8, pages 181185 (2015) | Download Citation

Abstract

Carbon dioxide has exerted the largest portion of radiative forcing and surface temperature change over the industrial era, but other anthropogenic influences have also contributed1,2. However, large uncertainties in total forcing make it difficult to derive climate sensitivity from historical observations3,4,5,6,7. Anthropogenic forcing has increased between the Fourth and Fifth Assessment Reports of the Intergovernmental Panel of Climate Change (IPCC; refs 1, 8), although its relative uncertainty has decreased. Here we show, based on data from the two reports, that this evolution towards lower uncertainty can be expected to continue into the future. Because it is easier to reduce air pollution than carbon dioxide emissions and because of the long lifetime of carbon dioxide, the less uncertain carbon dioxide forcing is expected to become increasingly dominant. Using a statistical model, we estimate that the relative uncertainty in anthropogenic forcing of more than 40% quoted in the latest IPCC report for 2011 will be almost halved by 2030, even without better scientific understanding. Absolute forcing uncertainty will also decline for the first time, provided projected decreases in aerosols occur. Other factors being equal, this stronger constraint on forcing will bring a significant reduction in the uncertainty of observation-based estimates of the transient climate response, with a 50% reduction in its uncertainty range expected by 2030.

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Acknowledgements

G.M. was supported by the Norwegian Research Council project SLAC (208277). Norwegian Research Council project number 230619 supported a personal visit for P.F.

Author information

Affiliations

  1. Center for International Climate and Environmental Research—Oslo (CICERO), Pb. 1129 Blindern, N-0318 Oslo, Norway

    • Gunnar Myhre
  2. Laboratoire de Météorologie Dynamique, IPSL, CNRS/UPMC, 75252 Paris, France

    • Olivier Boucher
  3. Laboratoire des Sciences du Climat et de l’Environnement, IPSL, CEA/CNRS/UVSQ, 91191 Gif sur Yvette, France

    • François-Marie Bréon
  4. School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK

    • Piers Forster
  5. Nicholas School of the Environment, Duke University, Durham, North Carolina 27708, USA

    • Drew Shindell

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Contributions

G.M., F-M.B. and D.S. initiated the study with additional contributions on the design of the study from P.F. and O.B. G.M., O.B., F-M.B., P.F. and D.S. performed the analysis and wrote the paper.

Competing interests

The authors declare no competing financial interests.

Corresponding author

Correspondence to Gunnar Myhre.

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DOI

https://doi.org/10.1038/ngeo2371