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Attribution of Arctic temperature change to greenhouse-gas and aerosol influences

Abstract

The Arctic has warmed significantly more than global mean surface air temperature over recent decades1, as expected from amplification mechanisms2,3. Previous studies have attributed the observed Arctic warming to the combined effect of greenhouse gases and other anthropogenic influences4. However, given the sensitivity of the Arctic to external forcing and the intense interest in the effects of aerosols on its climate5,6, it is important to examine and quantify the effects of individual groups of anthropogenic forcing agents. Here we quantify the separate contributions to observed Arctic land temperature change from greenhouse gases, other anthropogenic forcing agents (which are dominated by aerosols) and natural forcing agents. We show that although increases in greenhouse-gas concentrations have driven the observed warming over the past century, approximately 60% of the greenhouse-gas-induced warming has been offset by the combined response to other anthropogenic forcings, which is substantially greater than the fraction of global greenhouse-gas-induced warming that has been offset by these forcings7,8. The climate models considered on average simulate the amplitude of response to anthropogenic forcings well, increasing confidence in their projections of profound future Arctic climate change.

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Figure 1: Simulated and observed 1913–2012 temperature trends over the Arctic.
Figure 2: Simulated and observed Arctic temperature anomalies.
Figure 3: Scaling factors by which the simulated Arctic temperature response to GHG, OANT and NAT should be multiplied to best match observations and corresponding attributable temperature trends.

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References

  1. Christensen, J. H. et al. in Climate Change 2013: The Physical Science Basis (eds Stocker, T. F. et al.) Ch. 14 (IPCC, Cambridge Univ. Press, 2013).

    Google Scholar 

  2. Cohen, J. L., Furtado, J. C., Barlow, M. A., Alexeev, V. A. & Cherry, J. E. Arctic warming, increasing snow cover and widespread boreal winter cooling. Environ. Res. Lett. 7, 014007 (2012).

    Article  Google Scholar 

  3. Screen, J. A. & Simmonds, I. The central role of diminishing sea ice in recent Arctic temperature amplification. Nature 464, 1334–1337 (2010).

    Article  CAS  Google Scholar 

  4. Gillett, N. P. et al. Attribution of polar warming to human influence. Nature Geosci. 1, 750–754 (2008).

    Article  CAS  Google Scholar 

  5. Arctic Council Task Force on Short-Lived Climate Forcers Recommendations to Reduce Black Carbon and Methane Emissions to Slow Arctic Climate Change (Arctic Council, 2013).

    Google Scholar 

  6. Shindell, D. Estimating the potential for twenty-first century sudden climate change. Phil. Trans. R. Soc. A 365, 2675–2694 (2007).

    Article  CAS  Google Scholar 

  7. Bindoff, N. L. et al. in Climate Change 2013: The Physical Science Basis (eds Stocker, T. F. et al.) Ch. 10 (IPCC, Cambridge Univ. Press, 2013).

    Google Scholar 

  8. 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. Atmos. 118, 4001–4024 (2013).

    Article  Google Scholar 

  9. Jones, P. et al. Hemispheric and large-scale land-surface air temperature variations: An extensive revision and an update to 2010. J. Geophys. Res. 117, D05127 (2012).

    Google Scholar 

  10. Flato, G. et al. in Climate Change 2013: The Physical Science Basis (eds Stocker, T. F. et al.) Ch. 9 (IPCC, Cambridge Univ. Press, 2013).

    Google Scholar 

  11. Fyfe, J. C. et al. One hundred years of Arctic surface temperature variation due to anthropogenic influence. Sci. Rep. 3, 2645 (2013).

    Article  Google Scholar 

  12. Hansen, J., Ruedy, R., Sato, M. & Lo, K. Global surface temperature change. Rev. Geophys. 48, RG4004 (2010).

    Article  Google Scholar 

  13. Myhre, G. et al. in Climate Change 2013: The Physical Science Basis (eds Stocker, T. F. et al.) Ch. 8 (IPCC, Cambridge Univ. Press, 2013).

    Google Scholar 

  14. Allen, M. & Stott, P. Estimating signal amplitudes in optimal fingerprinting, Part I: Theory. Clim. Dynam. 21, 477–491 (2003).

    Article  Google Scholar 

  15. Ribes, A., Planton, S. & Terray, L. Application of regularised optimal fingerprinting to attribution. Part I: Method, properties and idealised analysis. Clim. Dynam. 41, 2817–2836 (2013).

    Article  Google Scholar 

  16. Smith, T. M., Reynolds, R. W., Peterson, T. C. & Lawrimore, J. Improvements to NOAA’s historical merged land–ocean surface temperature analysis (1880–2006). J. Clim. 21, 2283–2296 (2008).

    Article  Google Scholar 

  17. Hartmann, D. L. et al. in Climate Change 2013: The Physical Science Basis (eds Stocker, T. F. et al.) Ch. 2 (IPCC, Cambridge Univ. Press, 2013).

    Google Scholar 

  18. Stieglitz, M., DĂ©ry, S., Romanovsky, V. & Osterkamp, T. The role of snow cover in the warming of arctic permafrost. Geophys. Res. Lett. 30, 1721 (2003).

    Article  Google Scholar 

  19. Kay, J. E., Holland, M. M. & Jahn, A. Inter-annual to multi-decadal Arctic sea ice extent trends in a warming world. Geophys. Res. Lett. 38, L15708 (2011).

    Article  Google Scholar 

  20. Parkinson, C. L. & Comiso, J. C. On the 2012 record low Arctic sea ice cover: Combined impact of preconditioning and an August storm. Geophys. Res. Lett. 40, 1356–1361 (2013).

    Article  Google Scholar 

  21. Shepherd, A. et al. A reconciled estimate of ice-sheet mass balance. Science 338, 1183–1189 (2012).

    Article  CAS  Google Scholar 

  22. Gillett, N. P. & Von Salzen, K. The role of reduced aerosol precursor emissions in driving near-term warming. Environ. Res. Lett. 8, 034008 (2013).

    Article  Google Scholar 

  23. Collins, M. et al. in Climate Change 2013: The Physical Science Basis (eds Stocker, T. F. et al.) Ch. 12 (Cambridge Univ. Press, 2013).

    Google Scholar 

  24. Hasselmann, K. Multi-pattern fingerprint method for detection and attribution of climate change. Clim. Dynam. 13, 601–611 (1997).

    Article  Google Scholar 

Download references

Acknowledgements

We acknowledge the Program for Climate Model Diagnosis and Intercomparison and the World Climate Research Programme’s Working Group on Coupled Modelling for their roles in making the WCRP CMIP5 multi-model data sets available. This work is supported by the NSERC Canadian Sea Ice and Snow Evolution (CanSISE) Network.

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M.R.N., F.W.Z. and N.P.G. designed analysis. M.R.N. conducted the analysis and wrote the initial draft. F.W.Z. and N.P.G. helped with the analysis and edited the manuscript.

Corresponding author

Correspondence to Mohammad Reza Najafi.

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The authors declare no competing financial interests.

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Najafi, M., Zwiers, F. & Gillett, N. Attribution of Arctic temperature change to greenhouse-gas and aerosol influences. Nature Clim Change 5, 246–249 (2015). https://doi.org/10.1038/nclimate2524

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