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The effectiveness of polder systems on peak discharge capping of floods along the middle reaches of the Elbe River in Germany

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Fig. 1 and have been presented in Lindenschmidt (accepted).One of the first and few applications using this approachwas modeling the flood propagation through the Mekong
Fig. 2. Variants of polders that have been proposed to be constructedalong the middle reach of the Elbe River in Germany between Tor-gau and Lutherstadt Wittenberg (source: IWK, 2004).
Table 1. Discharge statistics for the gages at Torgau and Lutherstadt Wittenberg (MQ – mean discharge, MHQ – mean maximum annualflood, HQ – highest recorded flood event); source: Gew¨asserk¨undliches Jahrbuch, Elbegebiet Teil 1, 2003
Table 2. Morphological characteristics of polders P1, P3 and P4.
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