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Trends in Science and Technology   535
                                                   for Sustainable Living


                     A study has shown an interaction between El Niño Southern
                Oscillation  (ENSO)  and  the  Indian  Ocean  Dipole  (IOD)  to  the  dry
                season’s length, affecting salt production. Strong or extreme El
                Niño and positive IOD phases simultaneously result in longer
                drought conditions, thereby increasing salt harvest, as happened
                in 1982, 1997, and 2015. On the other hand, La Niña and negative
                IOD phases that occur simultaneously can increase rainfall. Rain
                throughout the dry season can cause salt harvest failure in all salt
                centers, as happened in 1998, 2010, and 2016 (Bramawanto & Abida,
                2017). Suppose at one time there is El Niño & positive IOD occurs
                simultaneously. In that case, vigilance is needed when it becomes
                La Niña and the negative IOD phase drastically the following year,
                impacting salt harvest failures like 2009-2010 and 2015-2016. Thus,
                it is increasingly evident that climate-weather factors significantly
                affect  salt  production.  Historical data  on  climate  variability,
                especially rainfall (precipitation) and salt production on a national
                scale, have the potential to be used to predict salt production in the
                future.
                     Studying rainfall in Indonesian regions that are generated by
                climate variability, such as ENSO and IOD, has its challenges. Various
                non-linear processes such as non-linear ocean advection, non-
                linear atmosphere-ocean interactions, state-dependent stochastic
                noise, tropical wave instability, and biophysical processes lead to
                El Niño and La Niña spatial  and temporal asymmetries  (An et al.,
                2020). Approaches using the Global Climate Model (GCM) and
                the Regional Climate Model (RCM) can be applied to developing
                climate change scenarios and anticipating ENSO irregularities due
                to complex ocean-atmosphere interactions (Endris et al., 2018).
                     Cirebon Regency was recorded as the largest producer
                of people’s salt in 2015, reaching 435,439 tons, outperforming
                Sampang Regency in East Java Province, Pati Regency in Central
                Java Province, and Indramayu Regency in West Java (Katadata,
                2016). However, this achievement did not continue in the following
                years, as seen from the decreasing salt production in Cirebon
                Regency.
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