Alamsyah Kurniawan
Previous studies showed that the tide mixing zone in the Malacca Strait could influence the spread of sea level anomalies from the South China Sea to the Andaman Sea. Strong tidal dynamics in the Malacca Strait are mainly due to the fact that here the main interaction occurs from tidal signals that enter the region from the two oceans namely the Indies, especially semi-diurnal and Pacific, especially diurnal. In addition, a complex setting mechanism, multi-scale, multi-dimensional, time The dynamics of the marine system that varies and is very non-linear make oceanographic modeling efforts much more challenging. Conventional numerical models provide major solutions for challenging tasks in characterizing and predicting marine weather (especially water levels and flow) by representing underlying physics in the equation that can be solved. However, capturing the ocean dynamics in total, taking into account non-tidal anomalies requires careful model adjustment for further improvement. The results of this study in this paper illustrate that the location of the tide mixing zone In local areas such as the Malacca Strait can be analyzed effectively by using a combination of numerical modeling and data-based models. These results support the indication that the phenomenon of mixed tidal zones observed in narrow grooves between the Malacca Strait and the Singapore Strait which can cause a blockage effect for the spread of sea level anomalies that occur in the South China Sea or the Java Sea. This work shows AMI efficiency as a potential hydroinformatics tool. Future work is recommended to calculate AMI for all domains in spatial maps to have a spatial distribution of ami in the desired area
Application of appropriate technology
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