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548     Fakultas Sains dan Teknologi
                   Universitas Terbuka (2023)



                    Coefficients  Standard Error  t Stat  P-value  Lower 95%  Upper 95%
           Intercept   393909,6    64275,18  6,128488  0,000281  245690,7886  542128,4284
           Rainfall    -94,5048     160,559  -0,5886  0,57237  -464,754438  275,7448966
           Rainy days  -6777,47     2533,61  -2,67503  0,028142  -12619,98983  -934,9583271

                       Partially, the effect of the number of rainy days on salt yields
                 looks  more  significant  than  the  effect  of  rainfall  on  salt  harvests,
                 indicated by the p-value of the number of rainy days (0,028), which
                 is lower than alpha (0,05). This analysis produced a formula that
                 can be used to estimate the salt harvest (Y’) as follows.

                          Y' = 393.909,6 - (94,5 × X ) - (6.777,5 × X ) + e   (4)
                                             1           2
                       The results of the predictions can only predict the ups and
                 downs  (fluctuations)  of  sea  salt  yields  in  Cirebon  and  illustrate
                 that if rainfall (X ) and the number of rainy days (X ) increase, the
                               1                           2
                 sea salt harvest (Y') will decrease and vice versa, indicated by the
                 negative value of the coefficient for rainfall and the number of rainy
                 days. In comparison between the actual value (blue line) and the
                 predicted results (red line) using the formula from multiple linear
                 regression (4), the error value of the model is relatively high (Table
                 6 and Figure 6), so the prediction accuracy is still low. Using rainfall
                 reanalysis  data  as  a  predictor  can  also  result  in  low  prediction
                 accuracy. The anomaly of Cirebon sea salt production in the last
                 five years, which has continued to experience a significant decline
                 compared to the harvest of Indramayu sea salt in a coastal area, is
                 also thought to have affected the low accuracy. However, in general,
                 the resulting fluctuation pattern is similar, so it is still feasible to be
                 used to predict sea salt yields. The accuracy of the method can
                 be improved by increasing the number of input data variables
                 or by adding other variables that have the potential to affect salt
                 yields. Other climatological variables that can be added include
                 air temperature, relative humidity, wind speed, and evaporation
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