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Technical note: Inherent benchmark or not? Comparing Nash–Sutcliffe and Kling–Gupta efficiency scores
Open accessAbstract
Abstract. A traditional metric used in hydrology to summarize model performance is the Nash–Sutcliffe efficiency (NSE). Increasingly an alternative metric, the Kling–Gupta efficiency (KGE), is used instead. When NSE is used, NSE = 0 corresponds to using the mean flow as a benchmark predictor. The same reasoning is applied in various studies that use KGE as a metric: negative KGE values are viewed as bad model performance, and only positive values are seen as good model performance. Here we show that using the mean flow as a predictor does not result in KGE = 0, but instead KGE =1-√2≈-0.41. Thus, KGE values greater than −0.41 indicate that a model improves upon the mean flow benchmark – even if the model's KGE value is negative. NSE and KGE values cannot be directly compared, because their relationship is non-unique and depends in part on the coefficient of variation of the observed time series. Therefore, modellers who use the KGE metric should not let their understanding of NSE values guide them in interpreting KGE values and instead develop new understanding based on the constitutive parts of the KGE metric and the explicit use of benchmark values to compare KGE scores against. More generally, a strong case can be made for moving away from ad hoc use of aggregated efficiency metrics and towards a framework based on purpose-dependent evaluation metrics and benchmarks that allows for more robust model adequacy assessment.
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“Notably, because KGE values below − 0.41 indicate a lack of hydrologic skill relative to the mean flow baseline56, our median KGE of 0.41 (top quartile of 0.65) confirms that at least half (resp. one fourth) of the generated ARCs offer meaningful (resp. good) predictive capacity and significantly outperform this standard threshold.”
From Global scale river discharge and mean depth from radar altimetry and model (2026) · cites this paper as [56]
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Model Evaluation Guidelines for Systematic Quantification of Accuracy in Watershed Simulations
Moriasi, D. N., Arnold, J. G., Liew, M. W. V., Bingner, R. L., Harmel, R. D., & Veith, T. L. (2007) · Transactions of the ASABE · doi:10.13031/2013.23153 · Cited by 13,446
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The role of aerodynamic resistance in thermal remote sensing-based evapotranspiration models
Trebs, I., Mallick, K., Bhattarai, N., Sulis, M., Cleverly, J., Woodgate, W., Silberstein, R., Hinko-Najera, N., Beringer, J., Meyer, W. S., et al. (2021) · Remote Sensing of Environment · doi:10.1016/j.rse.2021.112602 · Cited by 68
Global scale river discharge and mean depth from radar altimetry and model
Paris, A., Garambois, P.-A., Gal, L., Cerbelaud, A., Larnier, K., David, C. H., Jucá Oliveira, R. A., Correa, S. W., Tourian, M. J., & Calmant, S. (2026) · Nature Communications · doi:10.1038/s41467-026-78275-5
Metadata
- Authors
- Knoben, W. J. M., Freer, J. E., & Woods, R. A.
- Venue
- Hydrology and Earth System Sciences
- Publisher
- Copernicus GmbH
- Published
- 2019-10-25
- Volume
- 23
- Issue
- 10
- Pages
- 4323-4331
- ISSN
- 1027-5606 (ISSN-L)
- 1607-7938
- OpenAlex
- W2954648193
- Cited by
- 1,432
- References
- 1
- FWCI
- 45.52
- Type
- journal article
- Language
- en
- Open access
- gold
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- Knoben, W. J. M., Freer, J. E., & Woods, R. A. (2019). Technical note: Inherent benchmark or not? Comparing Nash–Sutcliffe and Kling–Gupta efficiency scores. Hydrology and Earth System Sciences. https://doi.org/10.5194/hess-23-4323-2019
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