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Increased El Niño frequency in a climate model forced by future greenhouse warming

Naturevolume 398pages694–697 (1999)Cite this article

Abstract

The El Niño/Southern Oscillation (ENSO) phenomenon is the strongest natural interannual climate fluctuation1. ENSO originates in the tropical Pacific Ocean and has large effects on the ecology of the region, but it also influences the entire global climate system and affects the societies and economies of manycountries2. ENSO can be understood as an irregular low-frequency oscillation between a warm (El Niño) and a cold (La Niña) state. The strong El Niños of 1982/1983 and 1997/1998, along with the more frequent occurrences of El Niños during the past few decades, raise the question of whether human-induced ‘greenhouse’ warming affects, or will affect, ENSO3. Several global climate models have been applied to transient greenhouse-gas-induced warming simulations to address this question4,6, but the results have been debated owing to the inability of the models to fully simulate ENSO (because of their coarse equatorial resolution)7. Here we present results from a global climate model with sufficient resolution in the tropics to adequately represent the narrow equatorial upwelling and low-frequency waves. When the model is forced by a realistic future scenario of increasing greenhouse-gas concentrations, more frequent El-Niño-like conditions and stronger cold events in the tropical Pacific Ocean result.

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Figure 1: Simulated temperature trends in equatorial waters.
Figure 2: Simulated sea-surface-temperature anomalies.
Figure 3: Interannual variability of observed and simulated SST anomalies.
Figure 4: Atmospheric and oceanic model sensitivity.

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References

  1. Philander, S. G. H.El Niño, La Niña, and the Southern Oscillation (Academic, San Diego, 1990).

    Google Scholar 

  2. Glantz, M. H., Katz, R. W. & Nicholls, N.Teleconnections Linking Worldwide Climate Anomalies (Cambridge Univ. Press, 1991).

    Google Scholar 

  3. Trenberth, K. & Hoar, T. The 1990–1995 El Niño–Southern Oscillation event: Longest on record.Geophys. Res. Lett.23, 57–60 (1996).

    Article ADS  Google Scholar 

  4. Knutson, T. R., Manabe, S. & Gu, D. Simulated ENSO in a global coupled ocean–atmosphere model: multidecadal amplitude modulation and CO2sensitivity.J. Clim.10, 138–161 (1997).

    Article ADS  Google Scholar 

  5. Tett, S. Simulation of El Niño-Southern Oscillation-like variability in a global AOGCM and its response to CO2increase.J. Clim.8, 1473–1502 (1995).

    Article ADS  Google Scholar 

  6. Meehl, G. A., Brantstator, G. W. & Washington, W. M. Tropical Pacific interannual variability and CO2climate change.J. Clim.6, 42–63 (1993).

    Article ADS  Google Scholar 

  7. Cane, M. A. et al. Twentieth-century sea surface temperature trends.Science275, 957–960 (1997).

    Article CAS  Google Scholar 

  8. Roeckner, E., Oberhuber, J. M., Bacher, A., Christoph, M. & Kirchner, I. ENSO variability and atmospheric response in a global atmosphere-ocean GCM.Clim. Dynam.12, 737–754 (1996).

    Article ADS  Google Scholar 

  9. Bacher, A., Oberhuber, J. M. & Roeckner, E. ENSO dynamics and seasonal cycle in the tropical Pacific as simulated by the ECHAM4/OPYC3 coupled general circulation model.Clim. Dynam.14, 431–450 (1997).

    Article ADS  Google Scholar 

  10. Oberhuber, J. M., Roeckner, E., Christoph, M., Esch, M. & Latif, M. Predicting the '97 El Niño event with a global climate model.Geophys. Res. Lett.25, 2273–2276 (1998).

    Article ADS  Google Scholar 

  11. Houghton, J. T., Callander, B. A. & Varney, S. K. V. (eds)IPCC Climate Change 1992. The Supplementary Report to the IPCC Scientific Assessment (Cambridge Univ. Press, 1992).

    Google Scholar 

  12. Meehl, G. A. & Washington, W. M. El Niño-like climate change in a model with increased atmospheric CO2concentrations.Nature382, 56–60 (1996).

    Article ADS CAS  Google Scholar 

  13. Ramanathan, V. & Collins, W. Thermodynamic regulation of ocean warming by cirrus clouds deduced from observations of the 1987 El Niño.Nature351, 27–32 (1991).

    Article ADS  Google Scholar 

  14. Roeckner, E., Bengtsson, L., Feichter, J., Lelieveld, J. & Rodhe, H. Transient climate change simulations with a coupled atmosphere-ocean GCM including the sulfur cycle.J. Clim.(in the press).

  15. Battisti, D. S. & Hirst, A. C. Interannual variability in the tropical atmosphere/ocean system: Influence of the basic state, ocean geometry and non-linearity.J. Atmos. Sci.46, 1687–1712 (1989).

    Article ADS  Google Scholar 

  16. Münnich, M., Cane, M. A. & Zebia, S. E. Astudy of self-excited oscillations of the tropical ocean–atmosphere system, Part II: Nonlinear cases.J. Atmos. Sci.48, 1238–1248 (1991).

    Article ADS  Google Scholar 

  17. Tziperman, E., Stone, L., Cane, M. A. & Jarosh, H. El Niño chaos: overlapping of resonances between the seasonal cycle and the Pacific Ocean–Atmosphere Oscillator.Science264, 72–74 (1994).

    Article ADS CAS  Google Scholar 

  18. Stone, L., Saparin, P. I., Huppert, A. & Price, C. El Niño chaos: The potential role of noise and stochastic resonance on the ENSO cycle.Geophys. Res. Lett.25, 175–178 (1998).

    Article ADS  Google Scholar 

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Acknowledgements

We thank T. P. Barnett for discussion and M. Münnich for help with data processing. This work was sponsored by the German government under its programme ‘Klimavariabilität und Signalanalyse’ and by the European Union through its ‘SINTEX’ programme. The climate model integrations were performed at the Deutsches Klimarechenzentrum.

Author information

Authors and Affiliations

  1. Max-Planck-Institut fr Meteorologie,

    A. Timmermann, A. Bacher, M. Esch, M. Latif & E. Roeckner

  2. Deutsches Klimarechenzentrum, Bundesstrasse 55, D-20146, Hamburg, Germany

    J. Oberhuber

Authors
  1. A. Timmermann

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  2. J. Oberhuber

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  3. A. Bacher

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  4. M. Esch

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  5. M. Latif

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  6. E. Roeckner

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Corresponding author

Correspondence toM. Latif.

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Timmermann, A., Oberhuber, J., Bacher, A.et al. Increased El Niño frequency in a climate model forced by future greenhouse warming.Nature398, 694–697 (1999). https://doi.org/10.1038/19505

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