2012
DOI: 10.1016/j.jhydrol.2011.08.056
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Results of the DMIP 2 Oklahoma experiments

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Cited by 104 publications
(76 citation statements)
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“…A nice example of this is provided by De Smedt et al (2000), who implement such reasoning in regards to the parameter values (based on an understanding of the physical structure of the model) and obtain quite good model simulation results without resorting to any "calibration". In support of this, note that Safari et al (2012) reported satisfactory results using an uncalibrated WetSpa, with only minor improvements obtained through calibration (see also Smith et al, 2012). De Smedt (2009, 2010) reported results of the snow modules of the WetSpa model using preset values with no calibration.…”
mentioning
confidence: 73%
“…A nice example of this is provided by De Smedt et al (2000), who implement such reasoning in regards to the parameter values (based on an understanding of the physical structure of the model) and obtain quite good model simulation results without resorting to any "calibration". In support of this, note that Safari et al (2012) reported satisfactory results using an uncalibrated WetSpa, with only minor improvements obtained through calibration (see also Smith et al, 2012). De Smedt (2009, 2010) reported results of the snow modules of the WetSpa model using preset values with no calibration.…”
mentioning
confidence: 73%
“…Reed et al, 2004;Breuer et al, 2009;Smith et al, 2012;Lobligeois et al, 2014;Maxwell et al, 2015;Vansteenkiste et al, 2014), there is surprisingly little fruitful exchange between the different modelling communities who start their model development from the two contrasting endpoints in the resolution-complexity continuum. Models at the lowresolution and low-complexity end of the continuum are criticized for lacking a robust physical or theoretical basis and for their inability to meaningfully represent spatial patterns (e.g.…”
Section: Introductionmentioning
confidence: 99%
“…Since the hydrological response of a basin is very sensitive to the spatio-temporal variability in various physical attributes of soil, land use, and topography, hydrological models that consider the spatial variability are better suited for accurate flood simulation and predictions [23][24][25]. Distributed hydrologic models can also provide a detailed description of the flood hazard areas, especially in urban catchments [26].…”
Section: Introductionmentioning
confidence: 99%
“…Physically based, distributed models employ a gridded nature, which allows parameters to be constrained within certain ranges that have clear physical meanings. Recent research demonstrated that physically-based, distributed hydrologic models can potentially perform as well as-or outperform-calibrated conceptual, lumped models [24][25][26][27]. The physically-based Gridded Surface Subsurface Hydrologic Analysis (GSSHA) model is an example of a grid-based fully-distributed hydrologic models [28].…”
Section: Introductionmentioning
confidence: 99%