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River basins located in the Central Sudetes (SW Poland) demonstrate a high vulnerability to flooding. Four mountainous basins and the corresponding outlets have been chosen for modeling the streamflow dynamics using TOPMODEL, a physically based semi-distributed topohydrological model. The model has been calibrated using the Monte Carlo approach—with discharge, rainfall, and evapotranspiration data used to estimate the parameters. The overall performance of the model was judged by interpreting the efficiency measures. TOPMODEL was able to reproduce the main pattern of the hydrograph with acceptable accuracy for two of the investigated catchments. However, it failed to simulate the hydrological response in the remaining two catchments. The best performing data set obtained Nash-Sutcliffe efficiency of 0.78. This data set was chosen to conduct a detailed analysis aiming to estimate the optimal timespan of input data for which TOPMODEL performs best. The best fit was attained for the half-year time span. The model was validated and found to reveal good skills.
Wydawca
Czasopismo
Rocznik
Tom
Strony
203--222
Opis fizyczny
Bibliogr. 78 poz.
Twórcy
autor
- Faculty of Earth Sciences and Environmental Management, Institute of Geography and Regional Development, University of Wrocław, Wrocław, Poland
- Center for Geospatial Analytics, North Carolina State University, Raleigh, USA
autor
- Faculty of Earth Sciences and Environmental Management, Institute of Geography and Regional Development, University of Wrocław, Wrocław, Poland
Bibliografia
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Uwagi
Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2018)
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-f1529697-d483-47d7-afff-6f7ca8314119