2014
DOI: 10.1061/(asce)he.1943-5584.0000909
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Parameter Uncertainty Analysis of Surface Flow and Sediment Yield in the Huolin Basin, China

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Cited by 44 publications
(33 citation statements)
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“…Since environmental data are usually not well behaved, input data and parameters are the major sources of uncertainties in risk assessment [15,16]. For example, concentrations of contaminants in the water sample are sometimes below the analytical reporting limit of the laboratory (also called the detection limit).…”
Section: Introductionmentioning
confidence: 99%
“…Since environmental data are usually not well behaved, input data and parameters are the major sources of uncertainties in risk assessment [15,16]. For example, concentrations of contaminants in the water sample are sometimes below the analytical reporting limit of the laboratory (also called the detection limit).…”
Section: Introductionmentioning
confidence: 99%
“…Furthermore, in the studies conducted in other parts of the world (e.g. Lenhart et al ., ; Muleta and Nicklow, ; Migliaccio and Chaubey, ; Yang et al ., ; Cibin et al ., ; Xue et al ., ), out of the sensitive parameters considered for streamflow simulation, generally, parameters like CN2, ESCO, SOL_AWC and GW_DELAY are common in most studies.…”
Section: Resultsmentioning
confidence: 99%
“…A close perusal of Figures and reveal that in case of SUFI‐2, the posterior distribution of optimal parameters spreads uniformly throughout the entire posterior range, whereas some of the parameters are not uniformly distributed in the posterior distribution in the case of GLUE. This indicates that GLUE provides a more objective distribution for posterior distribution (Xue et al ., ). It is also apparent from Figures and that sometimes SUFI‐2 yields poor results (NSE = zero or negative), but this is not the case with GLUE.…”
Section: Comparison Of Sufi‐2 and Glue Optimization Techniquesmentioning
confidence: 97%
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“…These values are often defined as optional input attributes and are generated through model calibration process, which is an important step in the application of a watershed model (Guinot et al 2011, Ye et al 2011). Nevertheless, the identification of these soil properties is a complex non-linear problem because numerous subprocesses are considered or because the interactions between parameters are complex (Shen et al 2010, Xue et al 2014. In this sense, soil properties cannot be identified easily because the calibrated soil properties might be a balanced different parameters, which cannot reflect the hydrological or environmental characteristics of the watershed (Schwen et al 2014).…”
Section: Introductionmentioning
confidence: 99%