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Fourth Study Conference on BALTEX Scala Cinema Gudhjem

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- 169 -<br />

Extreme Precipitati<strong>on</strong> <strong>on</strong> a Sub-Daily Scale Simulated with an RCM:<br />

Present Day and Future Climate<br />

O.B. Christensen 2 , A. Guldberg 2 , A.T. Jørgensen 1 , R.M. Johansen 1 , M. Grum 1 , J.J. Linde 1 and J.H.<br />

Christensen 2<br />

1 Technical University of Denmark<br />

2 Danish Meteorological Institute (obc@dmi.dk)<br />

An analysis has been performed <strong>on</strong> hourly precipitati<strong>on</strong><br />

output from the regi<strong>on</strong>al climate model (RCM) HIRHAM.<br />

As part of the EU 5th FP project PRUDENCE, this model<br />

has been run in 25 km resoluti<strong>on</strong> over an area covering<br />

Europe and the eastern Atlantic with boundary c<strong>on</strong>diti<strong>on</strong>s<br />

from the atmospheric high-resoluti<strong>on</strong> global model<br />

HadAM3H using sea-surface temperatures (SSTs) from<br />

observati<strong>on</strong>s for present day c<strong>on</strong>diti<strong>on</strong>s. A sec<strong>on</strong>d<br />

experiment uses SST observati<strong>on</strong>s plus anomalies based <strong>on</strong><br />

a climate change simulati<strong>on</strong> with the coupled global model<br />

HadCM3.<br />

Two time slices corresp<strong>on</strong>ding to 1961-90 and 2071-2100<br />

have been simulated. Hourly precipitati<strong>on</strong> for the whole year<br />

over Denmark has been analyzed. A comparis<strong>on</strong> is made<br />

between simulated grid point values and observati<strong>on</strong>-based<br />

values aggregated over a comparable area. The model<br />

somewhat underestimates the very extreme precipitati<strong>on</strong>.<br />

But appropriate scaling indicates that the model reproduces<br />

the observed shape near the tail of the precipitati<strong>on</strong> intensity<br />

distributi<strong>on</strong> functi<strong>on</strong> reas<strong>on</strong>ably well.<br />

The modeled climate change exhibits an increase of 30-40%<br />

for precipitati<strong>on</strong> for return periods of less than about 4 years.<br />

For larger return periods there is a higher increase of up to<br />

80%.<br />

In the paper we also assess the role of model resoluti<strong>on</strong>, as<br />

the same experimental setup has been applied at 50 km<br />

resoluti<strong>on</strong>, while preliminary analyses of a 12 km simulati<strong>on</strong><br />

also will be presented.

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