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Effect of meteorological forcing and snow model complexity on hydrological simulations in the Sieber catchment (Harz Mountains, Germany)

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Figure

Figure 1. Map of the study area including the Sieber catch-ment (watershed boundary is magenta colored) located in theHarz Mountains, northern Germany
Figure 2. WRF domains of the study area. The resolution of thefirst (outer) domain is 30 km, the fourth and final (inner) domain’sresolution is 1.1 km.
Figure 3. Conceptualization of hydrological processes in the hy-drological modeling system PANTA RHEI (adapted from LWI-HYWAG and IfW, 2012)
Figure 4. Comparison of simulated SWE and observed snow depth time series at the Torfhaus meteorological station: (a) winter season2005–2006, (b) winter season 2010–2011
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