Multi-objective assessment of hydrological model performances using Nash–Sutcliffe and Kling–Gupta efficiencies on a worldwide large sample of watersheds
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Hydrology and Atmospheric Sciences, University of ArizonaIssue Date
2024-02-23Keywords
DiagnosticsHydrological modeling
Kling–Gupta efficiency
Large-sample hydrology
Nash–Sutcliffe efficiency
Taylor diagram
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Academie des sciencesCitation
Thibault Mathevet; Nicolas Le Moine; Vazken Andréassian; Hoshin Gupta; Ludovic Oudin. Multi-objective assessment of hydrological model performances using Nash–Sutcliffe and Kling–Gupta efficiencies on a worldwide large sample of watersheds. Comptes Rendus. Géoscience, Volume 355 (2023) no. S1, pp. 117-141. doi : 10.5802/crgeos.189. https://comptes-rendus.academie-sciences.fr/geoscience/articles/10.5802/crgeos.189/Journal
Comptes Rendus - GeoscienceRights
This article is licensed under the Creative Commons Attribution 4.0 International License. https://creativecommons.org/licenses/by/4.0/.Collection Information
This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.Abstract
We introduce a new diagnosis tool that is well suited to analyzing simulation results over large samples of watersheds. It consists of a modification of the classical Taylor diagram to simultaneously visualize several error components (based on bias, standard deviation or squared errors) that are commonly used in efficiency criteria (such as the Nash–Sutcliffe efficiency (NSE) or the Kling–Gupta efficiency (KGE)) to evaluate hydrological model performance. We propose a methodological framework that explicitly links the graphical and numerical evaluation approaches, and show how they can be usefully combined to visually interpret numerical experiments conducted on large datasets. The approach is illustrated using results obtained by testing two rainfall-runoff models on a sample of 2050 watersheds from 8 countries and calibrated with two alternative objective functions (NSE and KGE). The assessment tool clearly highlights well-documented problems related to the use of the NSE for the calibration of rainfall-runoff models, which arise due to interactions between the ratio of simulated to observed standard deviations and the correlation coefficient. We also illustrate the negative impacts of classical mathematical transformations (square root) applied to streamflow when employing NSE and KGE as metrics for model calibration. © 2023 Elsevier Masson SAS. All rights reserved.Note
Open access articleISSN
1631-0713Version
Final Published Versionae974a485f413a2113503eed53cd6c53
10.5802/crgeos.189
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Except where otherwise noted, this item's license is described as This article is licensed under the Creative Commons Attribution 4.0 International License. https://creativecommons.org/licenses/by/4.0/.