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Assessing winter storm flow generation by means of permeability of the lithology and hydrological soil processes

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Academic year: 2021

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Table 1. C-values and standard deviations of the 16 sub-basins of the Nahe basin for a period from 1972 until 2002 and basin size.
Table 3. Residuals of the three Nahe models: the five worst performing basins of each model are given in bold.
Fig. 1. Permeability map of the Rhineland Palatinate and the Grand Duchy of Luxembourg.
Fig. 2a. Permeability map of the substratum of the Nahe basin and its 16 sub-basins. For the basin numbers see Table 1.
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