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

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

doi:10.1007/s10584-006-9226-z

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Journal article

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

Beniston, Martin Climate Research, University of Geneva, Switzerland
Stephenson, David B. Department of Meteorology, University of Reading, UK
Christensen, Ole B. Danish Meteorological Institute, Copenhagen, Denmark
Ferro, Christopher A. T. Department of Meteorology, University of Reading, UK
Frei, Christoph Swiss Federal Institute of Technology (ETH), Zurich, Switzerland
Goyette, Stéphane Climate Research, University of Geneva, Switzerland
Halsnaes, Kirsten Risoe National Laboratory, Roskilde, Denmark
Holt, Tom Climatic Research Unit, University of East Anglia, Norwich, UK
Jylhä, Kirsti Finnish Meteorological Institute, Helsinki, Finland
Koffi, Brigitte University of Fribourg, Fribourg, Switzerland
Palutikof, Jean Climatic Research Unit, University of East Anglia, Norwich, UK
Schöll, Regina Swiss Federal Institute of Technology (ETH), Zurich, Switzerland
Semmler, Tido Met Eireann, Dublin, Ireland
Woth, Katja GKSS Research Center, Geesthacht, Germany

22.03.2007

Published in:

Climatic Change. - 2007, vol. 81, no. Supl. 1, p. 71-95

English 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.

Faculty

Faculté des sciences et de médecine

Department

Département de Géosciences

Language