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Trends in Science and Technology   545
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                and sub-tropic precipitation. However, in this study, the rainfall
                from TRMM in the Cirebon district is still being compared with other
                rainfall data and will be discussed in another article.
                     The  findings  of  the  correlation  study  reveal  that  the  BMKG
                and TRMM rainfall patterns in Kalimantan are more similar as the
                cumulative number increases, with the yearly cumulative showing
                the highest correlation value (0,661–0,909). In particular, as a
                replacement  for  difficult-to-measure  specific  region  data,  TRMM
                rainfall  data  is  considered  capable  and  viable  as  a  fill-in  for  the
                missing BMKG rainfall data (Setiyawan et al., 2022).

                DISCUSSION

                1.   Correlation Analysis
                     The results of the correlation analysis showed that rainfall
                and rainy days each influenced Cirebon sea salt production with a
                negative correlation (Figure 4). It means that the increase in rainfall
                and the number of rainy days separately affect the decrease in
                sea salt yields. And conversely, low precipitation and a few rainy
                days can increase salt yields in Cirebon. The negative correlation
                between the number of rainy days and salt yield was stronger,
                with a value of -0,81755, than the correlation between rainfall and
                salt yield, with a value of -0,63075. Based on the de Vaus version
                correlation coefficient interpretation, interpretation of the strength of
                the relationship between variables shows that rainfall has a strong
                relationship with harvest yields, and rainy days have a powerful
                connection with sea salt yields.
                     The decline in salt production in 2016, 2020, and 2021 is
                closely related to the effects of wet drought due to La Niña events in
                those years. Simultaneous La Niña and negative IOD triggered the
                2016 wet-dry season. In 2020 and 2021, the wet-dry season will be
                caused by a series of multi-year La Niña (also called triple dip La
                Niña) in 2020-2022, accompanied by a negative IOD. Historical data
                shows that multi-year La Niña, as happened in the periods 1973–
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