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Estimates of future discharges of the river Rhine using two scenario methodologies: direct versus delta approach

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Academic year: 2021

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Figure

Fig. 1. Basin of the river Rhine, with the locations of five gauging stations.
Fig. 2: (a) Time series of the maximum discharge in a water-year at Lobith as simulated by RhineFlow driven by observed
Fig. 3. Bias of the HadRM3H simulation in mean winter (DJF) and summer (JJA) temperature (in K), and precipitation (in %).
Fig. 4. Area-mean (a) temperature, (b) PET, (c) precipitation, and (d) precipitation after bias correction, as a function of 10-day period
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