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5. Forecast Accuracy Evaluation    91




                  b y being the forecasted outputs (or predicted time series), y the observed data (or
                  observed or measured time series), and N the number of observations. MBE is not
                  a good indicator of the model reliability because the errors often compensate each
                  other, but it allows to see how much it overestimates or underestimates.

                  •  MAE is appropriate for applications with linear cost functions, that is, situations
                    where the costs resulting from a poor forecast are proportional to the forecast
                    error:
                                                   N
                                               1  X
                                       MAE ¼         jb yðiÞ  yðiÞj              (3.2)
                                               N
                                                   i¼1
                  •  The mean square error (MSE) uses the square of the difference between observed
                    and predicted values. This index penalizes the highest gaps:

                                                  N
                                              1  X             2
                                       MSE ¼         ðb yðiÞ  yðiÞÞ              (3.3)
                                              N
                                                  i¼1
                     MSE is usually the index minimized by training algorithms [found in Artificial
                  Neural Network (ANN) methods for instance].
                  •  The root mean square error (RMSE) is more sensitive to important forecast errors
                    and hence is suitable for applications where small errors are more tolerable and
                    larger errors lead to costs that are disproportionate, as in the case of utility
                    applications, for example. It is probably the reliability factor that is the most
                    widely used:
                                                 v ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
                                                 u      N
                                         p ffiffiffiffiffiffiffiffiffiffi  u 1  X        2
                                 RMSE ¼    MSE ¼  t        ðb yðiÞ  yðiÞÞ        (3.4)
                                                   N
                                                        i¼1

                  •  The mean absolute percentage error is close to the MAE but each gap between
                    observed and predicted data is divided by the observed data to get the relativegap.
                                                    N
                                               1   X  b yðiÞ  yðiÞ
                                       MAPE ¼                                    (3.5)
                                               N         yðiÞ
                                                   i¼1
                     This index has the disadvantage of being unstable when y(i) is near zero and it
                  cannot be defined for y(i) ¼ 0.
                     Often, these errors are normalized, which is particularly true for the RMSE; the
                  mean value of irradiation is generally used as reference:
                                              v ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
                                              u      N
                                                1
                                              u     X            2
                                                       ðb yðiÞ  yðiÞÞ
                                              t
                                                N
                                                    i¼1
                                     nRMSE ¼                                     (3.6)
                                                       y
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