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We quantify the water level variations for high and low roughness in the main channel when considering or not the feedback mechanism between the discharge at the bifurcation and the water levels.
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Wij kwantificeren de waterstandsvariaties voor hoge en lage ruwheid in de hoofdgeul wanneer al dan niet rekening wordt gehouden met het terugkoppelingsmechanisme tussen de afvoer bij de bifurcatie en de waterstanden.
SubsiteConference proceedingsPublication open access journal