Abstract
We show that given certain constraints, such as the spatial pattern of parameters, unique solutions do exist, thus making it possible to calibrate a distributed model. As we have shown in previous chapters, the drainage length, slope, and other parameters extracted from DEMs and geospatial data are resolution dependent. Thus, it is more likely than not, such parameters would require some adjustment. This chapter presents a method for calibrating a distributed model consistent with the conservation equations that underlie PBD models.
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Vieux, B.E. (2016). Distributed Model Calibration. In: Distributed Hydrologic Modeling Using GIS. Water Science and Technology Library, vol 74. Springer, Dordrecht. https://doi.org/10.1007/978-94-024-0930-7_10
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DOI: https://doi.org/10.1007/978-94-024-0930-7_10
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