Optimization of Loop Closure Phase on LiCSBAS for Ground Deformation Monitoring in Southern Sumatra

Muhammad Razzaaq Al Ghiffari, D. Nugroho, Afifuddin, A. Agustan, C. Endyana, Hendarmawan
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Abstract

Indonesian territory has an active tectonic, one of which is Southern Sumatra. This is due to the presence of a subduction zone in the west and the Sumatra fault which is parallel to each other. Such geological condition can lead to disasters (e.g earthquakes and tsunamis) whenever it occurs. Accordingly, monitoring ground deformation is an important analysis to do in this area. LiCSBAS becomes an effective open-source tool for observing time-series of ground deformation using InSAR. One of the stages, the loop closure phase is a critical step in generating the number of interferograms and pixels that will be used. The objective of this study is to observe ground deformation in Southern Sumatra by taking the optimal value of the loop closure threshold. The data processing results that the threshold value used is 1.6 rad. Meanwhile, the deformation pattern is generally divided into two areas, the western and eastern parts of Southern Sumatra. The western part close to the Sumatra Fault Zone shows a subsidence at a rate ∼115 mm/year and the eastern indicates an uplift ∼68 mm/year.
南苏门答腊岛地表变形监测LiCSBAS闭环相位优化
印度尼西亚境内有一个活跃的构造,其中之一是南苏门答腊。这是由于在西部存在一个俯冲带和相互平行的苏门答腊断层。这样的地质条件无论何时发生都可能导致灾难(如地震和海啸)。因此,监测地面变形是该地区的重要分析工作。LiCSBAS是利用InSAR观测地表时间序列变形的有效开源工具。其中一个阶段,环路闭合阶段是产生将要使用的干涉图和像素数量的关键步骤。本研究的目的是通过选取环闭合阈值的最优值来观测苏门答腊岛南部的地面变形。数据处理结果表明,使用的阈值为1.6 rad。同时,变形格局大致分为南苏门答腊西部和东部两个区域。靠近苏门答腊断裂带的西部以~ 115 mm/年的速度下沉,东部以~ 68 mm/年的速度隆起。
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