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Copula based multisite model for daily precipitation simulation

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Fig. 1. The locations of the rain gauge stations indicated by circled dots, around the Black Forest within the German state of  Baden-W¨urttemberg used in this study; shading darkens with increasing altitude above sea level
Fig. 2. Two sample copulas for station pairs 1 and 23, the upper panel (a) for Summer (June to August) and the bottom panel (b) for the relatively wetter Winter (December to February); see Fig
Fig. 4. Copula densities using the v- transform copula model with hidden normal density: (a) k = 4.0, m = 0, ρ = 0.75, (b) k = 1.0, m = 1, ρ = 0.75, and (c) the partitioned version of the  v-transformed copula in Fig
Fig. 6. Division of rainfall amount distribution corresponding to the left arm of the transformation (advective/stratiform precipitation) – red line and to the right arm (convective precipitation) – blue line.
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