A comparative study in modelling runoff and its components in two mountainous catchments

Authors

  • Joachim Gurtz,

    Corresponding author
    1. Institute for Atmosphere and Climate Science, Swiss Federal Institute of Technology (ETH) Zurich, Winterthurerstr. 190, CH-8057 Zurich, Switzerland
    • Institute for Atmosphere and Climate Science, Swiss Federal Institute of Technology, Winterthurerstr. 190, CH-8057, Zurich, Switzerland.
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  • Massimiliano Zappa,

    1. Institute for Atmosphere and Climate Science, Swiss Federal Institute of Technology (ETH) Zurich, Winterthurerstr. 190, CH-8057 Zurich, Switzerland
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  • Karsten Jasper,

    1. Institute for Atmosphere and Climate Science, Swiss Federal Institute of Technology (ETH) Zurich, Winterthurerstr. 190, CH-8057 Zurich, Switzerland
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  • Herbert Lang,

    1. Institute for Atmosphere and Climate Science, Swiss Federal Institute of Technology (ETH) Zurich, Winterthurerstr. 190, CH-8057 Zurich, Switzerland
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  • Mark Verbunt,

    1. Institute for Atmosphere and Climate Science, Swiss Federal Institute of Technology (ETH) Zurich, Winterthurerstr. 190, CH-8057 Zurich, Switzerland
    2. Department of Environmental Sciences, Sub-department Water Resources, Wageningen University, De Nieuwlanden, Nieuwe Kanaal 11, 6709 PA Wageningen, The Netherlands
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  • Alexandre Badoux,

    1. Swiss Federal Institute for Forest, Snow and Landscape Research (WSL) Birmensdorf, Zürcherstr. 111, CH-8903 Birmensdorf, Switzerland
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  • Tomas Vitvar

    1. Institute for Atmosphere and Climate Science, Swiss Federal Institute of Technology (ETH) Zurich, Winterthurerstr. 190, CH-8057 Zurich, Switzerland
    2. State University of New York, College of Environmental Science and Forestry, 1 Forestry Drive, Syracuse NY 13210, USA
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Abstract

In mountainous catchments the quality of runoff modelling depends strongly on the assessment of the spatial differences in the generation of the various runoff components and of the flow paths as coupled with the amount and intensity of precipitation and/or the snow melting. These catchments are also suitable for the intercomparison of different kinds of hydrological models, particularly of different approaches for the simulation of runoff generation. Two differently structured catchment models were applied on the pre-alpine Rietholzbach research catchment (3·2 km2) within the period 1981–98 and on the high-alpine Dischmabach catchment (43 km2) within the period 1981–96 for the simulation of hydrological processes and of the runoff hydrographs. The models adopted are the more physically based WaSiM-ETH model, with grid-oriented computation of the water balance elements, and the rather conceptual PREVAH model, based on hydrological response units. The simulation results and the differences resulting from the application of the two models are discussed and compared with the observed catchment discharges, with measurements of evapotranspiration, soil moisture, outflow of a lysimeter, and of groundwater levels in three access tubes. The model intercomparison indicates that the two approaches for determining runoff generation with different degrees of complexity performed with similar statistical efficiency over a period longer than 15 years. The analysis of the simulated runoff components shows that the interflow is the main runoff component and that the portion of the runoff components depends strongly on the approach used. The snowmelt model component is of decisive importance in the snowmelt season and needs to take into account the role of air temperature and radiation for simulating runoff generation in a spatially distributed manner. Copyright © 2003 John Wiley & Sons, Ltd.

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