Kling–Gupta efficiency
{{Short description|Performance indicator for hydrologic models}}
The Kling–Gupta efficiency (KGE) is a goodness-of-fit indicator widely used in the hydrologic sciences for comparing simulations to observations. It was created by hydrologic scientists Harald Kling and Hoshin Vijai Gupta.{{Cite journal| doi = 10.1029/2011WR010962| issn = 1944-7973| volume = 47| issue = 10| last1 = Gupta| first1 = Hoshin Vijai| last2 = Kling| first2 = Harald| title = On typical range, sensitivity, and normalization of Mean Squared Error and Nash–Sutcliffe Efficiency type metrics| journal = Water Resources Research| accessdate = 2023-08-24| date = 2011| bibcode = 2011WRR....4710601G| s2cid = 119636876| url = https://onlinelibrary.wiley.com/doi/abs/10.1029/2011WR010962| url-access = subscription}} Its creators intended for it to improve upon widely used metrics such as the coefficient of determination and the Nash–Sutcliffe model efficiency coefficient.
:
\text{KGE} =1-\sqrt{(r-1)^2+(\alpha-1)^2+(\beta-1)^2}
where:
- is the Pearson correlation coefficient,
- is a term representing the variability of prediction errors,
- is a bias term.
The terms and are defined as follows:
:
\beta=\frac{\mu_s}{\mu_o}
where:
- is the mean of the simulated time series (e.g.: flows predicted by the model)
- is the mean of the observed time series
and
:
\alpha = \frac{\sigma_s}{\sigma_o}
where:
- is the variance of the simulated time series, so is estimated by the standard deviation of simulated data.
- is the variance of the observed time series
A modified version, KGE', was proposed by Kling et al. in 2012.{{Cite journal| doi = 10.1016/j.jhydrol.2012.01.011| volume = 424| pages = 264–277| last1 = Kling| first1 = Harald| last2 = Fuchs| first2 = Martin| last3 = Paulin| first3 = Maria| title = Runoff conditions in the upper Danube basin under an ensemble of climate change scenarios| journal = Journal of Hydrology| date = 2012| bibcode = 2012JHyd..424..264K}}