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Fourth Study Conference on BALTEX Scala Cinema Gudhjem

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c<strong>on</strong>diti<strong>on</strong>s even more challenging than previously expected.<br />

Benist<strong>on</strong> (2004) extended a similar analysis to different<br />

parts of Europe and found that in the latter half of this<br />

century, summer temperatures would increase across much<br />

of the c<strong>on</strong>tinent leading to a “northward shift” in climatic<br />

z<strong>on</strong>es. This implies that Switzerland could, by the end of<br />

this century, have a climate similar to that currently found in<br />

the South of France, i.e., a “Mediterranean-type” of climate<br />

with l<strong>on</strong>g, dry summers and a winter rainy seas<strong>on</strong>, see e.g.<br />

Figure 2.<br />

Figure 2. Gaussian distributi<strong>on</strong>s fitted to the mean summer<br />

maximum temperature data at Basel, Switzerland, for the<br />

1961-1990 reference period (A: Observati<strong>on</strong>s; A':<br />

HIRHAM4 model results), the 2071-2100 A2 scenario<br />

simulati<strong>on</strong> (B) and the 2003 heat wave (C). This shows that<br />

the smoothed probability density functi<strong>on</strong> (PDF) for<br />

maximum temperatures in 2003 fits entirely within the PDF<br />

projected to occur in the latter part of the 21st century, and is<br />

well out of the range of the 1961-1990 summer maximum<br />

temperature PDF. (Courtesy of M. Benist<strong>on</strong>)<br />

5. The Nordic regi<strong>on</strong><br />

In PRUDENCE, the ideas already proposed in Christensen<br />

et al. (2001) for the Nordic regi<strong>on</strong> will be repeated, but at a<br />

much greater scale with a total of 9 participating RCMs.<br />

Preliminary results indicate that although with this greatly<br />

increased sampling size and even better coordinated<br />

modeling efforts, there is still a surprisingly big scatter<br />

between modeled climate change, even when <strong>on</strong>ly<br />

addressing standard variables such as 2 meter temperature<br />

and precipitati<strong>on</strong>. In this paper these preliminary findings<br />

will be substantiated and the analyses <strong>on</strong> extreme events,<br />

like those described previously, will be carried out for a<br />

larger ensemble of simulati<strong>on</strong>s than has been the case so far.<br />

References<br />

M. Benist<strong>on</strong>: The 2003 heat wave in Europe: A shape of<br />

things to come? An analysis based <strong>on</strong> Swiss<br />

climatological data and model simulati<strong>on</strong>s, Geophys.<br />

Res. Lett. 31, L02202, 2004.<br />

Christensen, J.H. and O.B. Christensen: Severe summertime<br />

flooding in Europe, Nature, 421, 805-806, 2003.<br />

- 161 -<br />

Christensen J.H., J. Räisänen, T. Iversen, D. Bjørge, O.B.<br />

Christensen, and M. Rummukainen: A synthesis of<br />

regi<strong>on</strong>al climate change simulati<strong>on</strong>s - A Scandinavian<br />

perspective. Geoph. Res. Lett., 28, 1003-1006, 2001.<br />

Schär, C., P.L. Vidale, D. Lüthi, C. Frei, C. Häberli, M.A,<br />

Liniger, and C. Appenzeller: The role of increasing<br />

temperature variability in European summer<br />

heatwaves, Nature, 427, 332-336, 2004.

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