CDT computes several statistics to evaluate the performance of merged data performed with CDT, satellite rainfall estimates products and the output of climate models, and to evaluate the skill of a specific methods or parameters used for the bias adjustment or the merging. These statistics can be classified into 3 groups: continuous, categorical and volumetric. The following table shows the list of all computed statistics.


Abbreviation Name Long Name Perfect Score Statistics Group Documentation
CORR Correlation 1 Continuous Forecast verification
BR2 Coefficient of determination (R2) multiplied by the regression slope 1 Continuous Package hydroGOF
BIAS Bias 1 Continuous Forecast verification
PBIAS Percent Bias 0 Continuous Forecast verification
ME Mean Error 0 Continuous Forecast verification
MAE Mean Absolute Error 0 Continuous Forecast verification
RMSE Root Mean Square Error 0 Continuous Forecast verification
NSE Nash-Sutcliffe Efficiency 1 Continuous Forecast verification
MNSE Modified Nash-Sutcliffe efficiency 1 Continuous Package hydroGOF
RNSE Relative Nash-Sutcliffe efficiency 1 Continuous Package hydroGOF
IOA Index of Agreement 1 Continuous Package hydroGOF
MIOA Modified index of agreement 1 Continuous Package hydroGOF
RIOA Relative Index of Agreement 1 Continuous Package hydroGOF
POD Probability Of Detection 1 Categorical Forecast verification
POFD Probability Of False Detection 0 Categorical Forecast verification
FAR False Alarm Ratio 0 Categorical Forecast verification
FBS Frequency Bias (Bias score) 1 Categorical Forecast verification
CSI Critical Success Index 1 Categorical Forecast verification
HSS Heidke Skill Score 1 Categorical Forecast verification
MQB Mean Quantile Bias 1 Volumetric (Aghakouchak et al., 2011) and (Aghakouchak & Mehran, 2013)
MQE Mean Quantile Error 0 Volumetric (Aghakouchak et al., 2011) and (Aghakouchak & Mehran, 2013)
VHI Volumetric Hit Index 1 Volumetric (Aghakouchak et al., 2011) and (Aghakouchak & Mehran, 2013)
QPOD Quantile Probability of Detection 1 Volumetric (Aghakouchak et al., 2011) and (Aghakouchak & Mehran, 2013)
VFAR Volumetric False Alarm Ratio 0 Volumetric (Aghakouchak et al., 2011) and (Aghakouchak & Mehran, 2013)
QFAR Quantile False Alarm Ratio 0 Volumetric (Aghakouchak et al., 2011) and (Aghakouchak & Mehran, 2013)
VMI Volumetric Miss Index 0 Volumetric (Aghakouchak et al., 2011) and (Aghakouchak & Mehran, 2013)
QMISS Quantile Miss Index 0 Volumetric (Aghakouchak et al., 2011) and (Aghakouchak & Mehran, 2013)
VCSI Volumetric Critical Success Index 1 Volumetric (Aghakouchak et al., 2011) and (Aghakouchak & Mehran, 2013)
QCSI Quantile Critical Success Index 1 Volumetric (Aghakouchak et al., 2011) and (Aghakouchak & Mehran, 2013)

References:

AghaKouchak, A., Behrangi , A., Sorooshian , S., Hsu , K., and Amitai , E. (2011): Evaluation of satellite-retrieved extreme precipitation rates across the Central United States. Journal of Geophysical Research, 116, D02115, doi:10.1029/2010JD014741.

AghaKouchak, A., and Mehran , A. (2013): Extended Contingency Table: Performance Metrics for Satellite Observations and Model Simulations. Water Resources Research, doi:10.1002/wrcr.20498.