Skip to main content

Thank you for visiting nature.com. You are using a browser version with limited support for CSS. To obtain the best experience, we recommend you use a more up to date browser (or turn off compatibility mode in Internet Explorer). In the meantime, to ensure continued support, we are displaying the site without styles and JavaScript.

  • Letter
  • Published:

Pace of shifts in climate regions increases with global temperature

Subjects

Abstract

Human-induced climate change causes significant changes in local climates1,2, which in turn lead to changes in regional climate zones. Large shifts in the world distribution of Köppen–Geiger climate classifications by the end of this century have been projected3. However, only a few studies have analysed the pace of these shifts in climate zones4,5, and none has analysed whether the pace itself changes with increasing global mean temperature. In this study, pace refers to the rate at which climate zones change as a function of amount of global warming. Here we show that present climate projections suggest that the pace of shifting climate zones increases approximately linearly with increasing global temperature. Using the RCP8.5 emissions pathway, the pace nearly doubles by the end of this century and about 20% of all land area undergoes a change in its original climate. This implies that species will have increasingly less time to adapt to Köppen zone changes in the future, which is expected to increase the risk of extinction5.

This is a preview of subscription content, access via your institution

Access options

Buy this article

Prices may be subject to local taxes which are calculated during checkout

Figure 1: Amount of land area affected by climatic shifts and its pace.
Figure 2: Percentage change in Köppen zones.
Figure 3: Map of changes in Köppen zones.
Figure 4: Analysis of the driving factor.

Similar content being viewed by others

References

  1. Mahlstein, I., Knutti, R., Solomon, S. & Portmann, R. W. Early onset of significant local warming in low latitude countries. Environ. Res. Lett. 6, 034009 (2011).

    Article  Google Scholar 

  2. Mahlstein, I., Portmann, R. W., Daniel, J. S., Solomon, S. & Knutti, R. Perceptible changes in regional precipitation in a future climate. Geophys. Res. Lett. 39, L05701 (2012).

    Google Scholar 

  3. Rubel, F. & Kottek, M. Observed and projected climate shifts 1901–2100 depicted by world maps of the Köppen–Geiger climate classification. Meteorol. Z. 19, 135–141 (2010).

    Article  Google Scholar 

  4. Burrows, M. T. et al. The pace of shifting climate in marine and terrestrial ecosystems. Science 334, 652–655 (2011).

    Article  CAS  Google Scholar 

  5. Sandel, B. et al. The influence of late quaternary climate-change velocity on species endemism. Science 334, 660–664 (2011).

    Article  CAS  Google Scholar 

  6. Williams, J. W., Jackson, S. T. & Kutzbacht, J. E. Projected distributions of novel and disappearing climates by 2100 AD. Proc. Natl Acad. Sci. USA 104, 5738–5742 (2007).

    Article  CAS  Google Scholar 

  7. Gnanadesikan, A. & Stouffer, R. J. Diagnosing atmosphere-ocean general circulation model errors relevant to the terrestrial biosphere using the Köppen climate classification. Geophys. Res. Lett. 33, L22701 (2006).

    Article  Google Scholar 

  8. Köppen, W. The thermal zones of the Earth according to the duration of hot, moderate and cold periods and to the impact of heat on the organic world. Meteorol. Z. 20, 351–360 (2011).

    Article  Google Scholar 

  9. Taylor, K. E., Stouffer, R. J. & Meehl, G. A. An overview of CMIP5 and the experiment design. Bull. Am. Meteorol. Soc. 93, 485–498 (2011).

    Article  Google Scholar 

  10. Van Vuuren, D. P. et al. The representative concentration pathways: An overview. Climatic Change 109, 5–31 (2011).

    Article  Google Scholar 

  11. Rogelj, J., Meinshausen, M. & Knutti, R. Global warming under old and new scenarios using IPCC climate sensitivity range estimates. Nature Clim. Change 2, 248–253 (2012).

    Article  Google Scholar 

  12. Hansen, J. E. A slippery slope: How much global warming constitutes ‘dangerous anthropogenic interference’? Climatic Change 68, 269–279 (2005).

    Article  Google Scholar 

  13. Randalls, S. History of the 2 °C climate target. WIRes Climatic Change 1, 598–605 (2010).

    Article  Google Scholar 

  14. Richard, S. J. T. Europe’s long term climate target: A critical evaluation. Energy Policy 35, 424–434 (2005).

    Google Scholar 

  15. Noake, K., Polson, D., Hegerl, G. & Zhang, X. Changes in seasonal land precipitation during the latter twentieth-century. Geophys. Res. Lett. 39, L03706 (2012).

    Article  Google Scholar 

  16. Zhang, X. B. et al. Detection of human influence on twentieth-century precipitation trends. Nature 448, 461–464 (2007).

    Article  CAS  Google Scholar 

  17. Liu, C., Allan, R. P. & Huffman, G. J. Co-variation of temperature and precipitation in CMIP5 models and satellite observations. Geophys. Res. Lett. 39, L13803 (2012).

    Google Scholar 

  18. Sherwood, S. C. & Huber, M. An adaptability limit to climate change due to heat stress. Proc. Natl Acad. Sci. USA 107, 9552–9555 (2010).

    Article  CAS  Google Scholar 

  19. Meinshausen, M. et al. The RCP greenhouse gas concentrations and their extensions from 1765 to 2300. Climatic Change 109, 213–241 (2011).

    Article  CAS  Google Scholar 

  20. Kottek, M., Grieser, J., Beck, C., Rudolf, B. & Rubel, F. World map of the Köppen–Geiger climate classification updated. Meteorol. Z. 15, 259–263 (2006).

    Article  Google Scholar 

  21. Rienecker, M. M. et al. MERRA: NASA’s modern-era retrospective analysis for research and applications. J. Clim. 24, 3624–3648 (2011).

    Article  Google Scholar 

  22. Xie, P. P. & Arkin, P. A. Global precipitation: A 17-year monthly analysis based on gauge observations, satellite estimates, and numerical model outputs. Bull. Am. Meteorol. Soc. 78, 2539–2558 (1997).

    Article  Google Scholar 

  23. IPCC Climate Change 2007: The Physical Science Basis (eds Solomon, S. et al.) (Cambridge Univ. Press, 2007).

Download references

Acknowledgements

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 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. We also thank U. Beyerle, J. Sedlacek and T. Corti for downloading and regridding the model data.

Author information

Authors and Affiliations

Authors

Contributions

I.M., J.S.D. and S.S. designed the study; I.M. did all the analysis shown in the study; I.M., J.S.D. and S.S. wrote the paper.

Corresponding author

Correspondence to Irina Mahlstein.

Ethics declarations

Competing interests

The authors declare no competing financial interests.

Supplementary information

Rights and permissions

Reprints and permissions

About this article

Cite this article

Mahlstein, I., Daniel, J. & Solomon, S. Pace of shifts in climate regions increases with global temperature. Nature Clim Change 3, 739–743 (2013). https://doi.org/10.1038/nclimate1876

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1038/nclimate1876

This article is cited by

Search

Quick links

Nature Briefing

Sign up for the Nature Briefing newsletter — what matters in science, free to your inbox daily.

Get the most important science stories of the day, free in your inbox. Sign up for Nature Briefing