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Large rainfall changes consistently projected over substantial areas of tropical land

Abstract

Many tropical countries are exceptionally vulnerable to changes in rainfall patterns, with floods or droughts often severely affecting human life and health, food and water supplies, ecosystems and infrastructure1. There is widespread disagreement among climate model projections of how and where rainfall will change over tropical land at the regional scales relevant to impacts2,3,4, with different models predicting the position of current tropical wet and dry regions to shift in different ways5,6. Here we show that despite uncertainty in the location of future rainfall shifts, climate models consistently project that large rainfall changes will occur for a considerable proportion of tropical land over the twenty-first century. The area of semi-arid land affected by large changes under a higher emissions scenario is likely to be greater than during even the most extreme regional wet or dry periods of the twentieth century, such as the Sahel drought of the late 1960s to 1990s. Substantial changes are projected to occur by mid-century—earlier than previously expected2,7—and to intensify in line with global temperature rise. Therefore, current climate projections contain quantitative, decision-relevant information on future regional rainfall changes, particularly with regard to climate change mitigation policy.

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Figure 1: Tropical land precipitation changes in two climate models, and observations of Sahel drought.
Figure 2: Tropical land precipitation change.
Figure 3: Relationship between area of tropical land with large precipitation change and global mean temperature change.
Figure 4: Regions most likely to experience large precipitation changes.

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References

  1. IPCC Summary for Policymakers in Climate Change 2014: Impacts, Adaptation, and Vulnerability (eds Field, C. B. et al.) (Cambridge Univ. Press, 2014).

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

    Google Scholar 

  3. McSweeney, C. F. & Jones, R. G. No consensus on consensus: The challenge of finding a universal approach to measuring and mapping ensemble consistency in GCM projections. Climatic Change 119, 617–629 (2013).

    Article  Google Scholar 

  4. Neelin, J. D., Munnich, M., Su, H., Meyerson, J. E. & Holloway, C. E. Tropical drying trends in global warming models and observations. Proc. Natl Acad. Sci. USA 103, 6110–6115 (2006).

    Article  CAS  Google Scholar 

  5. Chadwick, R., Boutle, I. & Martin, G. Spatial patterns of precipitation change in CMIP5: Why the rich do not get richer in the tropics. J. Clim. 26, 3803–3822 (2013).

    Article  Google Scholar 

  6. Kent, C., Chadwick, R. & Rowell, D. P. Understanding uncertainties in future projections of regional precipitation. J. Clim. 28, 4390–4413 (2015).

    Article  Google Scholar 

  7. Mora, C. et al. The projected timing of climate departure from recent variability. Nature 502, 183–187 (2014).

    Article  Google Scholar 

  8. Chou, C. & Neelin, J. D. Mechanisms of global warming impacts on regional tropical precipitation. J. Clim. 17, 2688–2701 (2004).

    Article  Google Scholar 

  9. Held, I. M. & Soden, B. J. Robust responses of the hydrological cycle to global warming. J. Clim. 19, 5686–5699 (2006).

    Article  Google Scholar 

  10. Seager, R., Naik, N. & Vecchi, G. A. Thermodynamic and dynamic mechanisms for large-scale changes in the hydrological cycle in response to global warming. J. Clim. 23, 4651–4668 (2010).

    Article  Google Scholar 

  11. Chou, C., Neelin, J. D., Chao-An, C. & Jien-Yi, T. Evaluating the “Rich-Get-Richer” mechanism in tropical precipitation change under global warming. J. Clim. 22, 1982–2005 (2009).

    Article  Google Scholar 

  12. Solomon, S., Plattner, G-K., Knutti, R. & Friedlingstein, P. Irreversible climate change due to carbon dioxide emissions. Proc. Natl Acad. Sci. USA 106, 1704–1709 (2009).

    Article  CAS  Google Scholar 

  13. Liu, C. & Allan, R. P. Observed and simulated precipitation responses in wet and dry regions 1850–2100. Environ. Res. Lett. 8, 034002 (2013).

    Article  Google Scholar 

  14. Durack, P. J., Wijffels, S. E. & Matear, R. J. Ocean salinities reveal strong global water cycle intensification during 1950 to 2000. Science 336, 455–458 (2012).

    Article  CAS  Google Scholar 

  15. Xie, S.-P. et al. Global warming pattern formation: Sea surface temperature and rainfall. J. Clim. 23, 966–986 (2010).

    Article  Google Scholar 

  16. Greve, P. et al. Global assessment of trends in wetting and drying over land. Nature Geosci. 7, 716–721 (2014).

    Article  CAS  Google Scholar 

  17. Roderick, M. L., Sun, F., Lim, W. H. & Farquhar, G. D. A general framework for understanding the response of the water cycle to global warming over land and ocean. Hydrol. Earth Syst. Sci. 18, 1575–1589 (2014).

    Article  Google Scholar 

  18. Rowell, D. P. Sources of uncertainty in future changes in local precipitation. Clim. Dynam. 39, 1929–1950 (2012).

    Article  Google Scholar 

  19. Good, P. & Lowe, J. Emergent behaviour and uncertainty in multimodel climate projections of precipitation trends at small spatial scales. J. Clim. 19, 5554–5569 (2006).

    Article  Google Scholar 

  20. Ackerley, D. et al. Sensitivity of twentieth-century Sahel rainfall to sulfate aerosol and CO2 forcing. J. Clim. 24, 4999–5014 (2011).

    Article  Google Scholar 

  21. Rotstayn, L. D. et al. Have Australian rainfall and cloudiness increased due to the remote effects of Asian anthropogenic aerosols? J. Geophys. Res. 112, D09202 (2007).

    Article  Google Scholar 

  22. Allen, M. R. & Ingram, W. J. Constraints on future changes in climate and the hydrological cycle. Nature 419, 224–232 (2002).

    CAS  Google Scholar 

  23. Giorgi, F. & Bi, X. Time of emergence (TOE) of GHG-forced precipitation change hot-spots. Geophys. Res. Lett. 36, L06709 (2009).

    Article  Google Scholar 

  24. Bayr, T. & Dommenget, D. The tropospheric land–sea warming contrast as the driver of tropical sea level pressure changes. J. Clim. 26, 1387–1402 (2013).

    Article  Google Scholar 

  25. Giannini, A. Mechanisms of climate change in the Semiarid African Sahel: The local view. J. Clim. 23, 743–756 (2010).

    Article  Google Scholar 

  26. Fasullo, J. A mechanism for land–ocean contrasts in global monsoon trends in a warming climate. Clim. Dynam. 39, 1137–1147 (2012).

    Article  Google Scholar 

  27. Seo, J., Kang, S. M. & Frierson, D. M. W. Sensitivity of intertropical convergence zone movement to the latitudinal position of thermal forcing. J. Clim. 27, 3035–3042 (2014).

    Article  Google Scholar 

  28. Hwang, Y.-T., Frierson, D. M. W. & Kang, S. M. Anthropogenic sulphate aerosol and the southward shift of tropical precipitation in the late 20th century. Geophys. Res. Lett. 40, 2845–2850 (2013).

    Article  Google Scholar 

  29. Cao, L., Bala, G. & Caldeira, K. Climate response to changes in atmospheric carbon dioxide and solar irradiance on the time scale of days to weeks. Environ. Res. Lett. 7, 034015 (2012).

    Article  Google Scholar 

  30. Levine, R. C., Turner, A. G., Marathayil, D. & Martin, G. M. The role of northern Arabian Sea surface temperature biases in CMIP5 model simulations and future predictions of Indian summer monsoon rainfall. Clim. Dynam. 41, 155–172 (2012).

    Article  Google Scholar 

  31. Kutzbach, J. E. & Liu, Z. Response of the African monsoon to orbital forcing and ocean feedbacks in the middle Holocene. Science 278, 440–443 (1997).

    Article  CAS  Google Scholar 

  32. Harris, I., Jones, P. D., Osborn, T. J. & Lister, D. H. Updated high-resolution grids of monthly climatic observations-the CRU TS3.10 dataset. Int. J. Climatol. 34, 623–642 (2013).

    Article  Google Scholar 

  33. Adler, R. F. The Version 2 Global Precipitation Climatology Project (GPCP) monthly precipitation analysis (1979-Present). J. Hydrometeorol. 4, 1147–1167 (2003).

    Article  Google Scholar 

  34. Arid Zone Forestry: A Guide for Field Technicians Ch. 1 (FAO Corporate Document Repository, 1989); http://www.fao.org/docrep/t0122e/t0122e03.htm#chapter%20i.%20the%20arid%20environments

  35. Mahli, Y. & Wright, J. Spatial patterns and recent trends in the climate of tropical rainforest regions. Phil. Trans. R. Soc. Lond. B 359, 311–329 (2004).

    Article  Google Scholar 

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Acknowledgements

All authors were supported by the Joint UK DECC/Defra Met Office Hadley Centre Climate Programme (GA01101). 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 thank G. J. van Oldenborgh for making the CMIP5 data easily available via the KNMI Climate Explorer tool.

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R.C. conceived the original idea for the study, and performed the analysis. All authors provided additional ideas, helped to refine the methodology, and contributed towards writing the manuscript.

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Correspondence to Robin Chadwick.

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The authors declare no competing financial interests.

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Chadwick, R., Good, P., Martin, G. et al. Large rainfall changes consistently projected over substantial areas of tropical land. Nature Clim Change 6, 177–181 (2016). https://doi.org/10.1038/nclimate2805

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