Kling–Gupta efficiency

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Template:Short description 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.[1] Its creators intended for it to improve upon widely used metrics such as the coefficient of determination and the Nash–Sutcliffe model efficiency coefficient.

KGE=1(r1)2+(α1)2+(β1)2

where:

The terms α and β are defined as follows:

β=μsμo

where:

  • μs is the mean of the simulated time series (e.g.: flows predicted by the model)
  • μo is the mean of the observed time series

and

α=σsσo

where:

  • σs2 is the variance of the simulated time series, so σs is estimated by the standard deviation of simulated data.
  • σo2 is the variance of the observed time series

A modified version, KGE', was proposed by Kling et al. in 2012.[2]

References

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