Assesses the model's calibration quality with the help of the pairwise complete modelled as well as observed loads and the following metrics:
NSE: Nash-Sutcliffe Efficiency
mNSE: Modified Nash-Sutcliffe Efficiency (j = 1)
KGE: Modified Kling-Gupta Efficiency
RMSE: Root Mean Square Error
PBIAS: Percent Bias
RSR: Ratio of the RMSE to the standard deviation of the observations
RCV: Ratio of the coefficients of variation
GMRAE: Geometric Mean Relative Absolute Error
MdRAE: Median Relative Absolute Error
In addition, a scatter plot with the observed river loads on the x- and the modelled river loads on the y-axis is displayed and provides a visual impression of the model performance. Other elements of this plot are an identity line (solid) and plus/minus 30% deviation lines (dashed).
## S4 method for signature 'RPhosFate'calibrationQuality(x, substance, col)
Arguments
x: An S4 RPhosFate river catchment object.
substance: A character string specifying the substance to calculate.
col: A character string specifying the calibration data column with the respective substance river loads.
Returns
A named numeric vector containing the assessed metrics along with the in-channel retention ratio (one minus sum of xxt at catchment outlet(s) divided by sum of xxt_inp).
Nash, J.E., Sutcliffe, J.V., 1970. River flow forecasting throughconceptual models part I – a discussion of principles. Journal ofHydrology 10, 282–290. https://doi.org/10.1016/0022-1694(70)90255-6
Legates, D.R., McCabe Jr., G.J., 1999. Evaluating the use of“goodness-of-fit” measures in hydrologic and hydroclimatic modelvalidation. Water Resources Research 35, 233–241.https://doi.org/10.1029/1998WR900018
Kling, H., Fuchs, M., Paulin, M., 2012. Runoff conditions in the upperDanube basin under an ensemble of climate change scenarios. Journal ofHydrology 424–425, 264–277.https://doi.org/10.1016/j.jhydrol.2012.01.011
Moriasi, D.N., Arnold, J.G., Van Liew, M.W., Bingner, R.L., Harmel,R.D., Veith, T.L., 2007. Model evaluation guidelines for systematicquantification of accuracy in watershed simulations. Transactions ofthe ASABE 50, 885–900.