Abstract

This study aims to simulate tsunami wave heights and their travel time toward the WestKalimantan coastal area. A Nuclear Power Plant (NPP) will be developed in a coastal area in the WestKalimantan Province, Indonesia. The two scenarios of events that may trigger the tsunami waves are volcanicevents caused by Mount Krakatau located in the Sunda Strait and tectonic subduction located at the IndianOcean on the west side of the Sunda Strait. Modeling the tsunami propagation using a finite-element-basedhydrodynamic model developed by the US Army Corps of Engineer, namely the Surface-water ModelingSystem (SMS), is carried out. The model simulates tsunami wave propagation for six alternative locations atthe proposed site of NPP. The model domains consist of Sunda Strait and Karimata Strait domains. The SundaStrait domain model is validated by the observed historical tsunami heights reaching the 12 locations inLampung, Banten, West Java, and Jakarta of Indonesia. The model validations show a good agreement. Thevalidated hydrodynamic model results of the Sunda Strait model are used as the boundary conditions for theKarimata Strait domain model. The Karimata Strait model results show that the peaks of tsunami wave heightsthat reach the western Kalimantan coast are between 12 cm and 116 cm. The minimum wave height peak thatreaches the six prospective locations is 12 cm, which is located in Sambas Regency.

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