Abstract
Large differences in climate outcomes are projected by the end of this century depending on whether greenhouse gas emissions continue to increase or are reduced sufficiently to limit total warming to below 2 °C (ref. 1). However, it is generally thought that benefits of mitigation are hidden by internal climate variability until later in the century2. Here we show that if the likelihood of extremely hot seasons is considered, the benefits of mitigation emerge more quickly than previously thought. It takes less than 20 years of emissions reductions in many regions for the likelihood of extreme seasonal warmth to reduce by more than half following initiation of mitigation. Additionally we show that the latest possible date at which the probability of extreme seasonal temperatures will be halved through emissions reductions consistent with the 2 °C target is in the 2040s. Exposure to climate risk is therefore reduced markedly and rapidly with substantial reductions of greenhouse gas emissions, demonstrating that the early mitigation needed to limit eventual warming below potentially dangerous levels benefits societies in the nearer term not just in the longer-term future.
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References
Collins, M. et al. in Climate Change 2013: The Physical Science Basis (eds Stocker, T. F. et al.) Ch. 12, 1029–1136 (IPCC, Cambridge Univ. Press, 2013).
Kirtman, B. et al. in Climate Change 2013: The Physical Science Basis (eds Stocker, T. F. et al.) Ch. 11, 953–1028 (IPCC, Cambridge Univ. Press, 2013).
Allen, M. R. et al. Warming caused by cumulative carbon emissions towards the trillionth tonne. Nature 458, 1163–1166 (2009).
Taylor, K. E., Stouffer, R. J. & Meehl, G. A. An overview of CMIP5 and the experiment design. Bull. Am. Meteorol. Soc. 93, 485–498 (2012).
Meinshausen, M. et al. The RCP greenhouse gas concentrations and their extensions from 1765 to 2300. Climatic Change 109, 213–241 (2011).
Hawkins, E. & Sutton, R. Time of emergence of climate signals. Geophys. Res. Lett. 39, L01702 (2012).
Mahlstein, I., Knutti, R., Solomon, S. & Portmann, R. Early onset of significant local warming in low latitude countries. Environ. Res. Lett. 6, 034009 (2011).
Mahlstein, I., Hegerl, G. & Solomon, S. Emerging local warming signals in observational data. Geophys. Res. Lett. 39, L21711 (2012).
King, A. D. et al. The timing of anthropogenic emergence in simulated climate extremes. Environ. Res. Lett. 10, 094015 (2015).
Diffenbaugh, N. S. & Scherer, M. Observational and model evidence of global emergence of permanent, unprecedented heat in the 20th and 21st centuries. Climatic Change 107, 615–624 (2011).
Tebaldi, C. & Friedlingstein, P. Delayed detection of climate mitigation benefits due to climate inertia and variability. Proc. Natl Acad. Sci. USA 110, 17229–17234 (2013).
IPCC Managing the Risks of Extreme Events and Disasters to Advance Climate Change Adaptation (eds Field, C. B. et al.) (Cambridge Univ. Press, 2012).
Christidis, N., Jones, G. S. & Stott, P. A. Dramatically increasing chance of extremely hot summers since the 2003 European heatwave. Nat. Clim. Change 5, 46–50 (2014).
Russo, S., Sillmann, J. & Fischer, E. M. Top ten European heatwaves since 1950 and their occurrence in the coming decades. Environ. Res. Lett. 10, 124003 (2015).
Sanderson, B. M., Oleson, K. W., Strand, W. G., Lehner, F. & O’Neill, B. C. A new ensemble of GCM simulations to assess avoided impacts in a climate mitigation scenario. Climatic Change http://dx.doi.org/10.1007/s10584-015-1567-z (2015).
Allen, M. R. & Stocker, T. F. Impact of delay in reducing carbon dioxide emissions. Nat. Clim. Change 4, 23–26 (2014).
Allen, M. Liability for climate change. Nature 421, 891–892 (2003).
Herring, S. C., Hoerling, M. P., Peterson, T. C. & Stott, P. A. Explaining extreme events of 2013 from a climate perspective. Bull. Am. Meteorol. Soc. 95, S1–S104 (2014).
Herring, S. C., Hoerling, M. P., Kossin, J. P., Peterson, T. C. & Stott, P. A. Explaining extreme events of 2014 from a climate perspective. Bull. Am. Meteorol. Soc. 96, S1–S172 (2015).
Peters, G. P. et al. The challenge to keep global warming below 2 °C. Nat. Clim. Change 3, 4–6 (2013).
Friedlingstein, P. et al. Persistent growth of CO2 emissions and implications for reaching climate targets. Nat. Geosci. 7, 709–715 (2014).
Lowe, J. A. et al. How difficult is it to recover from dangerous levels of global warming? Environ. Res. Lett. 4, 014012 (2009).
Tebaldi, C., O’Neill, B. & Lamarque, J.-F. Sensitivity of regional climate to global temperature and forcing. Environ. Res. Lett. 10, 074001 (2015).
Jones, P. D. et al. Hemispheric and large-scale land-surface air temperature variations: an extensive revision and an update to 2010. J. Geophys. Res. 117, 1984–2012 (2012).
Morice, C. P., Kennedy, J. J., Rayner, N. A. & Jones, P. D. Quantifying uncertainties in global and regional temperature change using an ensemble of observational estimates: the HadCRUT4 data set. J. Geophys. Res. 117, 1984–2012 (2012).
New, M., Lister, D., Hulme, M. & Makin, I. A high-resolution data set of surface climate over global land areas. Clim. Res. 21, 1–25 (2002).
Jones, G. S., Stott, P. A. & Christidis, N. Attribution of observed historical near-surface temperature variations to anthropogenic and natural causes using CMIP5 simulations. J. Geophys. Res. 118, 4001–4024 (2013).
Hawkins, E. et al. Uncertainties in the timing of unprecedented climates. Nature 511, E3–E5 (2014).
Forster, P. M. Evaluating adjusted forcing and model spread for historical and future scenarios in the CMIP5 generation of climate models. J. Geophys. Res. 118, 1139–1150 (2013).
Acknowledgements
This work was supported by the Joint UK BEIS/Defra Met Office Hadley Centre Climate Programme (GA01101) and by the EUCLEIA project funded by the European Union’s Seventh Framework Programme [FP7/2007–2013] under grant agreement no. 607085. We acknowledge the World Climate Research Programme’s Working Group on Coupled Modelling, which is responsible for CMIP, and we thank the climate modelling groups (listed in Supplementary Table 1) for producing and making available their model output. For CMIP the US Department of Energy’s Program for Climate Model Diagnosis and Intercomparison provides coordinating support and led development of software infrastructure in partnership with the Global Organization for Earth System Science Portals.
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A.C. conducted the research and wrote the first draft of the paper. P.S. initially suggested a study concerning changing extremes under mitigation. Both P.S. and J.L. contributed to discussion of the results and revisions of the paper.
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Ciavarella, A., Stott, P. & Lowe, J. Early benefits of mitigation in risk of regional climate extremes. Nature Clim Change 7, 326–330 (2017). https://doi.org/10.1038/nclimate3259
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DOI: https://doi.org/10.1038/nclimate3259
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