Future runoff from a partly glacierized watershed in Central Switzerland: A two-model approach

► We investigate the response of a glacio-nival watershed to a changing climate. ► We used both a conceptual and a physically based hydrological model. ► Both models consistently predicted future seasonal runoff dynamics. ► However, the models disagreed regarding the evolution of glacier melt rates. ► The study highlights the benefits of multi-model approaches. We present a comprehensive hydrological modeling study in the drainage area of a hydropower reservoir in central Switzerland. To investigate the response of this 95km2 alpine watershed to a changing climate, we used both a conceptual and a physically based hydrological model approach. The multi-model approach enabled detailed insights into the uncertainties associated with model projections of future runoff based on climate scenarios. Both hydrological models consistently predicted changes of the seasonal runoff dynamics, including the timing of snowmelt and peak-flow in summer as well as the future spread between high and low flow years. However the models disagreed regarding the evolution of glacier melt rates thus leading to a considerable difference in predicted annual runoff figures. The findings suggest that snow-glacier feedbacks require particular attention when predicting future runoff from glacio-nival watersheds.