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Parameter uncertainty assessment for a conceptual hydrological model in a snow-dominated catchment combining streamflow records and MODIS snow cover maps

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Parameter uncertainty assessment for a conceptual hydrological model in a snow-dominated

catchment combining streamflow records and MODIS snow cover maps

Nicola Di Marco1, Diego Avesani1, Maurizio Righetti1, Mattia Zaramella2, Bruno Majone3, Marco Borga2

1 Free University of Bozen/Bolzano, Bozen/Bolzano, Italy 2 TESAF, Legnaro, Italy

3 DICAM, Trento, Italy

Conceptual hydrological models describe the different hydrological processes through empirical relationships, driven by several, often non-physical, parameters. The estimation of such model parameters introduces significant uncertainty on the prediction of both streamflow and the other components of the hydrological balance. In this work, we propose a multi-objective parameter uncertainty analysis, combining streamflow records and MODIS-derived snow-covered area (SCA) images, based on the well-known GLUE procedure in order to quantify the predictive parametric uncertainty of streamflow, SCA and mean areal snow water equivalent. This procedure was tested at Passirio river catchment, a mountainous catchment ranging from 360 m to 3500 m with a contributing area of about 400 km2 placed in the upper Adige river basin (South Tyrol, Italy). Firstly it was evaluated at the catchment

scale and secondly it was applied in an upstream sub-catchment, to spatially validate the proposed approach. Conditioning the hydrological model with the multi-objective approach instead of using only streamflow data show that: both SCA and mean areal SWE predicted uncertainty bands reduce up to 30%; the streamflow uncertainty range shrinks up to 11% at the outlet section and up to 17% in the upstream sub-catchment. These results suggest that the presented procedure might be appealing for inferring uncertainty bounds of streamflow and snow-related predictive variables at different, perhaps poorly gauged, locations across the catchment.

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