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Prange, S., Vohland, K., Conradt, T., & Hattermann, F. F. (2013). Klimabedingte Veränderungen der Abflussdynamik von ausgewählten deutschen Fließgewässern und ihre naturschutzfachliche Bedeutung. In: Schutzgebiete Deutschlands im Klimawandel – Risiken und Handlungsoptionen. In F. Badeck, K. Böhning-Gaese, G. Ellwanger, J. Hanspach, P. L. Ibisch, S. Klotz, et al. (Eds.), (pp. 55–69). Naturschutz und Biologische Vielfalt, 129. Bonn-Bad Godesberg: Bundesamt für Naturschutz.
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Conradt, T. (2013). Introduction to the eco-hydrological model SWIM, recent applications and new developments..
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Conradt, T., Hattermann, F. F., Koch, H., & Wechsung, F. (2013). Klima- und Landnutzungsszenarien in ihren Wirkungen auf den Wasserabfluss. In F. Wechsung, V. Hartje, S. Kaden, M. Venohr, B. Hansjürgens, & P. Gräfe (Eds.), (pp. 177–209). Die Elbe im globalen Wandel. Berlin: Weißensee Verl.
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Conradt, T., Koch, H., Hattermann, F. F., Wechsung, F., Hartje, V., Kaden, S., et al. (2013). Validierung von Lokalkorrekturen der Verdunstung bei den Simulationen des Wasserabflusses. In F. Wechsung, V. Hartje, S. Kaden, M. Venohr, B. Hansjürgens, & P. Gräfe (Eds.), (pp. 211–231). Die Elbe im globalen Wandel. Berlin: Weißensee Verl.
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Conradt, T., Wechsung, F., & Bronstert, A. (2013). Three perceptions of the evapotranspiration landscape: comparing spatial patterns from a distributed hydrological model, remotely sensed surface temperatures, and sub-basin water balances. Hydrol. Earth System Sci., 17(7), 2947–2966.
Abstract: A problem encountered by many distributed hydrological modelling studies is high simulation errors at interior gauges when the model is only globally calibrated at the outlet. We simulated river runoff in the Elbe River basin in central Europe (148 268 km(2)) with the semi-distributed eco-hydrological model SWIM (Soil and Water Integrated Model). While global parameter optimisation led to Nash-Sutcliffe efficiencies of 0.9 at the main outlet gauge, comparisons with measured runoff series at interior points revealed large deviations. Therefore, we compared three different strategies for deriving sub-basin evapotranspiration: (1) modelled by SWIM without any spatial calibration, (2) derived from remotely sensed surface temperatures, and (3) calculated from long-term precipitation and discharge data. The results show certain consistencies between the modelled and the remote sensing based evapotranspiration rates, but there seems to be no correlation between remote sensing and water balance based estimations. Subsequent analyses for single sub-basins identify amongst others input weather data and systematic error amplification in inter-gauge discharge calculations as sources of uncertainty. The results encourage careful utilisation of different data sources for enhancements in distributed hydrological modelling.
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