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ABSTRACTS 'Extreme Discharges' - CHR-KHR

ABSTRACTS 'Extreme Discharges' - CHR-KHR

ABSTRACTS 'Extreme Discharges' - CHR-KHR

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Mutlivariate statistical analysis of flood generation in the<br />

Meuse catchment<br />

Paul Torfs<br />

Wageningen University, Water Resources Department<br />

Nieuwe Kanaal 11, NL 6709 PA Wageningen, the Netherlands<br />

paul.torfs@wur.nl<br />

Within the framework of a larger program, a hydrological model of the whole Meuse catchment was made by<br />

RIZA, the ministry responsible for the flood prediction and management in the Netherlands. This model is<br />

based build on the well known HSB model, and is semi-distributied. The KNMI, the meteorlogical institute of<br />

the Netherlands, has made by statistitical long artificial series of rainfall series as input for this model. A combination<br />

of both generates artificial but unusual long statitistical stationary series of discharges.<br />

The research focused on the spatial analysis of these series for extremes.<br />

Entropy was used as a method to analyse uniformity. Large extremes proved to be consistently uniform distributed,<br />

both in space and time.<br />

Next a multivariate statisitical analysis of extremes was tried. Classical univariate analysis results in discharges<br />

and return periods for each of the subcatchments seperately. Bivariate analysis is more complicated, but results<br />

in insight in the statistical dependency of these extremes. Nearby catchments proved to be significantly stronger<br />

dependend than combinations of catchents further seperated.<br />

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