Skip to main content

Table 2 Statistical indicators, equation, range, and best value used in the study

From: Spatiotemporal variability and trends of rainfall and its association with Pacific Ocean Sea surface temperature in West Harerge Zone, Eastern Ethiopia

Statistic

Equation

Range

Unit

Best value

Pearson Correlation Coefficient (r)

\({\text{r}}_{ = } \frac{{\mathop \sum \nolimits_{{{\text{i}} = 1}}^{\text{n}} ({\text{Gi}} - {\bar{\text{G}}})\left( {{\text{Si}} - {\bar{\text{S}}}} \right)}}{{ \sqrt {\mathop \sum \nolimits_{{{\text{i}} = 1}}^{\text{n}} ({\text{Gi}} - {\bar{\text{G}}})^{2} \mathop \sum \nolimits_{{{\text{i}} = 1}}^{\text{n}} ({\text{Si}} - {\bar{\text{S}}})^{2} } }}\)

− 1 to 1

None

1

Nash–Sutcliff efficacy Coefficient (NSE)

\({\text{NSE}} = 1 - \frac{{\mathop \sum \nolimits_{{{\text{i}} = 1}}^{\text{n}} ({\text{Gi}} - {\text{Si}})^{2} }}{{\mathop \sum \nolimits_{{{\text{i}} = 1}}^{\text{n}} ({\text{Gi}} - {\bar{\text{G}}})^{2} }}\)

− ∞ to 1

None

1

Root Mean Square Error (RMSE)

\({\text{RMSE}} = \frac{{\sqrt {\mathop \sum \nolimits_{i = 1}^{n} \left( {Si - Gi} \right)^{2} } }}{n}\)

0 to ∞

mm

0

Mean Absolute Error (MAE)

\({\text{MAE}} = \frac{1}{n}\mathop \sum \limits_{i = 1}^{n} |Si - Gi|\)

0 to ∞

mm

0

Mean Bias Error (MBE)

\({\text{MBE}} = \frac{1}{n}\mathop \sum \limits_{i = 1}^{n} \left( {Si - Gi} \right)\)

− ∞ to ∞

mm

0

  1. Where n is the length of the time series, and i is the number of years. Gi and Si are the meteorological gauge rainfall value and CHIRPS rainfall value in the year i, respectively, and \(\overline{\text{G}}\) and \(\overline{\text{S}}\) are the mean meteorological gauge rainfall and the mean of CHIRPS rainfall, respectively