2013
DOI: 10.1002/wrcr.20444
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Separately accounting for uncertainties in rainfall and runoff: Calibration of event-based conceptual hydrological models in small urban catchments using Bayesian method

Abstract: [1] Uncertainty analysis of hydrological models is usually based on model calibration, and the Bayesian method is a popular way to evaluate the uncertainty. The traditional Bayesian method usually uses lumped model residuals to form the likelihood function, where uncertainty in inputs (rainfall) is not explicitly addressed. This paper compares three approaches based on Bayesian inferences, considering rainfall uncertainty either implicitly or explicitly in calibration. Consistent parameter estimation and relia… Show more

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Cited by 29 publications
(20 citation statements)
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References 42 publications
(92 reference statements)
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“…For instance, errors in areal rainfall (represented by point measurements) and runoff measurements lead to biased calibration results, as in calibration, the model parameters are adjusted to make the lumped model outputs match the measurements. Additionally, the model parameters are correlated (e.g., Sun & Bertrand‐Krajewski, ). The initial loss and proportional loss are negatively correlated; the reservoir constant and the time shift are also negatively correlated.…”
Section: Resultsmentioning
confidence: 99%
“…For instance, errors in areal rainfall (represented by point measurements) and runoff measurements lead to biased calibration results, as in calibration, the model parameters are adjusted to make the lumped model outputs match the measurements. Additionally, the model parameters are correlated (e.g., Sun & Bertrand‐Krajewski, ). The initial loss and proportional loss are negatively correlated; the reservoir constant and the time shift are also negatively correlated.…”
Section: Resultsmentioning
confidence: 99%
“…Inferring σ β leads to a hierarchical parameter estimation problem. While some applications of RM kept σ β fixed [ Sun and Bertrand‐Krajewski , ], making the error model nonhierarchical, we prefer to infer this hyperparameter to learn about the overall input variance detected during calibration [ Li et al ., ; Sikorska et al ., ]. Despite using the same likelihood function as for the LS method, the replacement of the input description (2) by (6) leads to the consideration of input uncertainty at the level of whole storm events and augments the parameter vector with the parameters boldΨx={β,σβ} of the rainfall error model.…”
Section: Methodsmentioning
confidence: 99%
“…A more satisfying approach for considering input errors is to make the input uncertain and to propagate it through the model [ Honti et al ., ; McMillan et al ., ]. A simple way of doing so, which has become popular in hydrology, is the use of so‐called rainfall multipliers [ Kavetski et al ., ; Sun and Bertrand‐Krajewski , ]. These are event‐specific random variables multiplied with the observed rain to provide the input to the model.…”
Section: Introductionmentioning
confidence: 99%
“…In both methods, structural and input uncertainties are aggregated into one term. Approaches that, instead of just describing the output errors, focus on identifying the causes of model inadequacies. To quantify input uncertainty, rainfall multipliers have been proposed [ Kuczera et al ., ; Sun and Bertrand‐Krajewski , ]. Structural uncertainty, instead, has been dealt with by inferring the model equations [ Bulygina and Gupta , ], the behavior of dynamic parameters [ Reichert and Mieleitner , ], or the value of model parameters and states [ Vrugt et al ., ].…”
Section: Brief Review Of Methods Applied For Uncertainty Quantificatimentioning
confidence: 99%