Climatic Change

, Volume 81, Supplement 1, pp 71–95 | Cite as

Future extreme events in European climate: an exploration of regional climate model projections

  • Martin BenistonEmail author
  • David B. Stephenson
  • Ole B. Christensen
  • Christopher A. T. Ferro
  • Christoph Frei
  • Stéphane Goyette
  • Kirsten Halsnaes
  • Tom Holt
  • Kirsti Jylhä
  • Brigitte Koffi
  • Jean Palutikof
  • Regina Schöll
  • Tido Semmler
  • Katja Woth


This paper presents an overview of changes in the extreme events that are most likely to affect Europe in forthcoming decades. A variety of diagnostic methods are used to determine how heat waves, heavy precipitation, drought, wind storms, and storm surges change between present (1961–90) and future (2071–2100) climate on the basis of regional climate model simulations produced by the PRUDENCE project. A summary of the main results follows. Heat waves – Regional surface warming causes the frequency, intensity and duration of heat waves to increase over Europe. By the end of the twenty first century, countries in central Europe will experience the same number of hot days as are currently experienced in southern Europe. The intensity of extreme temperatures increases more rapidly than the intensity of more moderate temperatures over the continental interior due to increases in temperature variability. Precipitation – Heavy winter precipitation increases in central and northern Europe and decreases in the south; heavy summer precipitation increases in north-eastern Europe and decreases in the south. Mediterranean droughts start earlier in the year and last longer. Winter storms – Extreme wind speeds increase between 45°N and 55°N, except over and south of the Alps, and become more north-westerly than cuurently. These changes are associated with reductions in mean sea-level pressure, leading to more North Sea storms and a corresponding increase in storm surges along coastal regions of Holland, Germany and Denmark, in particular. These results are found to depend to different degrees on model formulation. While the responses of heat waves are robust to model formulation, the magnitudes of changes in precipitation and wind speed are sensitive to the choice of regional model, and the detailed patterns of these changes are sensitive to the choice of the driving global model. In the case of precipitation, variation between models can exceed both internal variability and variability between different emissions scenarios.


Heat Wave Regional Climate Model Emission Scenario Storm Surge Heavy Precipitation 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.


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Copyright information

© Springer Science+Business Media, B.V. 2007

Authors and Affiliations

  • Martin Beniston
    • 1
    Email author
  • David B. Stephenson
    • 2
  • Ole B. Christensen
    • 3
  • Christopher A. T. Ferro
    • 2
  • Christoph Frei
    • 4
  • Stéphane Goyette
    • 1
  • Kirsten Halsnaes
    • 5
  • Tom Holt
    • 6
  • Kirsti Jylhä
    • 7
  • Brigitte Koffi
    • 8
  • Jean Palutikof
    • 6
  • Regina Schöll
    • 4
  • Tido Semmler
    • 9
  • Katja Woth
    • 10
  1. 1.Climate ResearchUniversity of GenevaGenevaSwitzerland
  2. 2.Department of MeteorologyUniversity of ReadingReadingUK
  3. 3.Danish Meteorological InstituteCopenhagenDenmark
  4. 4.Swiss Federal Institute of Technology (ETH)ZurichSwitzerland
  5. 5.Risoe National LaboratoryRoskildeDenmark
  6. 6.Climatic Research UnitUniversity of East AngliaNorwichUnited Kingdom
  7. 7.Finnish Meteorological InstituteHelsinkiFinland
  8. 8.University of FribourgFribourgSwitzerland
  9. 9.Met EireannDublinIreland
  10. 10.GKSS Research CenterGeesthachtGermany

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