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Journal ArticleDOI

The future of distributed models: model calibration and uncertainty prediction.

Keith Beven, +1 more
- 01 Jul 1992 - 
- Vol. 6, Iss: 3, pp 279-298
TLDR
The GLUE procedure works with multiple sets of parameter values and allows that, within the limitations of a given model structure and errors in boundary conditions and field observations, different sets of values may be equally likely as simulators of a catchment.
Abstract
This paper describes a methodology for calibration and uncertainty estimation of distributed models based on generalized likelihood measures. The GLUE procedure works with multiple sets of parameter values and allows that, within the limitations of a given model structure and errors in boundary conditions and field observations, different sets of values may be equally likely as simulators of a catchment. Procedures for incorporating different types of observations into the calibration; Bayesian updating of likelihood values and evaluating the value of additional observations to the calibration process are described. The procedure is computationally intensive but has been implemented on a local parallel processing computer.

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Citations
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Journal ArticleDOI

Decomposition of the mean squared error and NSE performance criteria: Implications for improving hydrological modelling

TL;DR: A diagnostically interesting decomposition of NSE is presented, which facilitates analysis of the relative importance of its different components in the context of hydrological modelling, and it is shown how model calibration problems can arise due to interactions among these components.
Book

Sensitivity Analysis in Practice: A Guide to Assessing Scientific Models

TL;DR: In this paper, the authors present a method for sensitivity analysis of a fish population model using Monte Carlo filtering and variance-based methods, which is based on the Bayesian uncertainty estimation.
Journal ArticleDOI

A manifesto for the equifinality thesis

TL;DR: The argument is made that the potential for multiple acceptable models as representations of hydrological and other environmental systems (the equifinality thesis) should be given more serious consideration than hitherto.
Journal ArticleDOI

Equifinality, data assimilation, and uncertainty estimation in mechanistic modelling of complex environmental systems using the GLUE methodology

TL;DR: The generalised likelihood uncertainty estimation (GLUE) methodology for model identification allowing for equifinality is described, and an example application to rainfall-runoff modelling is used to illustrate the methodology, including the updating of likelihood measures.
Journal ArticleDOI

Status of Automatic Calibration for Hydrologic Models: Comparison with Multilevel Expert Calibration

TL;DR: The capability of the shuffled complex evolution automatic procedure is compared with the interactive multilevel calibration multistage semiautomated method developed for calibration of the Sacramento soil moisture accounting streamflow forecasting model of the U.S. National Weather Service and suggests that the state of the art in automatic calibration now can be expounded.
References
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Book

Bayesian inference in statistical analysis

TL;DR: In this article, the effect of non-normality on inference about a population mean with generalizations was investigated. But the authors focused on the effect on the mean with information from more than one source.
Journal ArticleDOI

On the Mathematical Foundations of Theoretical Statistics

TL;DR: In this paper, the authors define the center of location as the abscissa of a frequency curve for which the sampling errors of optimum location are uncorrelated with those of optimum scaling.
Book

Fuzzy Sets, Uncertainty and Information

TL;DR: The fuzzy sets uncertainty and information is one book that the authors really recommend you to read, to get more solutions in solving this problem.
Journal ArticleDOI

Empirical equations for some soil hydraulic properties

TL;DR: In this paper, a power function relating soil moisture and hydraulic conductivity is used to derive a formula for the wetting front suction required by the Green-Ampt equation.
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