Unterschiede
Hier werden die Unterschiede zwischen zwei Versionen angezeigt.
Beide Seiten der vorigen Revision Vorhergehende Überarbeitung Nächste Überarbeitung | Vorhergehende Überarbeitung | ||
thesis:diagnosticcalibration [2013/12/15 11:50] – mweiler | thesis:diagnosticcalibration [2019/10/17 15:13] (aktuell) – mweiler | ||
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- | ===== Diagnostic calibration of a hydrological model in snow and glacier melt dominated | + | ===== Diagnostic calibration of a hydrological model in mountainous |
== Problemstellung == | == Problemstellung == | ||
Zeile 5: | Zeile 5: | ||
== Ziel der Arbeit == | == Ziel der Arbeit == | ||
- | Usually, climate and runoff are the sole sources for model calibration. However, partitioning the hydrograph into periods when certain processes are dominating the runoff generation could be used to find model parameters only relevant for these processes in the model. In addition, high temporal data not being used directly in the model application (daily fluctuation of the stream hydrograph in hourly data) could be used for diagnostic calibration. At the end, the improved parameter calibration will be compared to multi-objective calibration approaches using addition data (snow depth, snow distribution, | + | Usually, climate and runoff are the sole sources for model calibration. However, partitioning the hydrograph into periods when certain processes are dominating the runoff generation could be used to find model parameters only relevant for these processes in the model. In addition, high temporal |
== Methode == | == Methode == | ||
Zeile 34: | Zeile 34: | ||
Yilmaz, K. K., Gupta, H. V. and Wagener, T.: A process-based diagnostic approach to model evaluation: Application to the NWS distributed hydrologic model, Water Resour. Res., 44, W09417, doi: | Yilmaz, K. K., Gupta, H. V. and Wagener, T.: A process-based diagnostic approach to model evaluation: Application to the NWS distributed hydrologic model, Water Resour. Res., 44, W09417, doi: | ||
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