| Description: |
A comprehensive hydrological modeling study in the drainage area of a hydropower reservoir in central Switzerland is presented. Two models were tested to reproduce the measured discharge dynamics: (1) a detailed energy-balance model primarily designed for snow simulations; (2) a conceptual runoff model system, including a distributed temperature-index snow and ice melt model. The research suggest a shift of spring peak-flow by almost two months for the end of the century. [Source: Applied Geochemistry]
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