Analysis of Coastline Changes in Palu Bay, Central Sulawesi after the 2018 Tsunami Based on Sentinel 1 Satellite Imagery Using the Digital Shoreline Analysis System (DSAS) Method

M. A. Z. Fuad, Fikri Hardiansyah, B. Semedi
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Abstract

The Palu-Donggala earthquake that occurred on September 28, 2018 caused additional disasters in the form of liquefaction and tsunami. The tsunami that hit the coastal area of Palu Bay caused considerable damage, indicating a change in the coastline. The purpose of this study was to determine the changes in the coastline that occurred in Palu Bay, Palu City, Central Sulawesi as a result of the Tsunami. The data used in this study are Sentinel 1 satellite imagery before and after the Tsunami occurred. The coastline at each time is obtained from the extraction of Sentinel 1 satellite imagery. Analysis of shoreline change uses quantitative descriptive techniques with the help of the DSAS tool with change analysis based on the Net Shoreline Movement (NSM) method which is integrated with ArcGIS software. The results show that there has been a significant change in the coastline in Palu Bay, Palu City, Central Sulawesi. Coastline changes that occur are in the form of abrasion and accretion conditions, but are more dominated by abrasion. The highest abrasion of -167.53m is found on transect 309 which is located in the District of Mantikulore, and the lowest abrasion value of -0.43m is found on transect 242 which is located in the Ulujadi District. Meanwhile, the highest accretion value of 47.27m is found on transect 105 which is located in the West Palu District, and the lowest abrasion value of 0.56m is found on transect 68 which is also located in the West Palu District. The magnitude of the change in coastline that occurred in Palu Bay, Palu City, Central Sulawesi after the Tsunami was influenced by the openness of the coastal area to wave blows, the oval and narrow morphology of Palu Bay and the occurrence of ground deformation in the Palu-Koro Fault
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基于Sentinel 1卫星图像的2018年苏拉威西岛中部帕卢湾海啸后海岸线变化分析
2018年9月28日发生的帕鲁-东加拉地震以液化和海啸的形式造成了额外的灾害。袭击帕卢湾沿海地区的海啸造成了相当大的破坏,表明海岸线发生了变化。本研究的目的是确定海啸对苏拉威西岛中部帕卢市帕卢湾海岸线的影响。本研究中使用的数据是海啸发生前后的哨兵1号卫星图像。每次的海岸线是由哨兵1号卫星图像提取得到的。岸线变化分析采用定量描述技术,借助DSAS工具,结合ArcGIS软件进行基于净岸线运动(NSM)方法的变化分析。结果表明,苏拉威西岛中部帕卢市帕卢湾的海岸线发生了明显的变化。海岸线的变化以磨损和增生条件的形式发生,但更多地以磨损为主。位于Mantikulore区的样带309的磨损值最高,为-167.53m,位于Ulujadi区的样带242的磨损值最低,为-0.43m。同时,位于West Palu区的样带105的吸积值最高,为47.27m,而位于West Palu区的样带68的磨损值最低,为0.56m。海啸发生后,苏拉威西岛中部帕卢市帕卢湾海岸线的变化幅度受沿海地区对海浪的开放程度、帕卢湾椭圆形狭窄的地貌以及帕卢-科罗断层地面变形的发生等因素的影响
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