Measuring Deformation in Jakarta through Long Term Synthetic Aperture Radar (SAR) Data Analysis

2nd International Conference of Indonesian Society for Remote Sensing 2016

地球科学;计算机科学

Agustan^1 ; Sulaiman, Albertus^1 ; Ito, Takeo^2

Center of Technology for Regional Resources Development (PTPSW), BPPT, Jakarta, Indonesia^1

Research Center for Seismology, Volcanology and Disaster Mitigation, Nagoya University, Japan^2

关键词: Application platforms;    Complex environmental problems;    Environmental carrying capacities;    Geothermal fluids;    Physical deformation;    Physical development;    Single-look complexes;    Tectonic movements;   

Others  :  https://iopscience.iop.org/article/10.1088/1755-1315/47/1/012022/pdf
DOI  :  10.1088/1755-1315/47/1/012022

学科分类：计算机科学（综合）

来源: IOP

【 摘 要 】

Jakarta as a home for more than 10 millions habitant facing complex environmental problems due to physical development that cause physical deformation. Physical deformation issues such as decreasing environmental carrying capacity, land cover changes and land subsidence have occurred. Recent studies shows that the long of shoreline changes in a span of 13 years from 2002 to 2015 around 14 km due to land reclamation in Jakarta bay. Previous studies also concluded that Jakarta suffer a sinking phenomena due to its rapid subsidence rate, approximately 260 mm/year in northern part of Jakarta. During the 2007 to 2011, the land subsidence phenomena in Jakarta was observed by InSAR based on ALOS-PALSAR data and found that the subsided areas only occurred in certain areas, mainly in Pluit and Cengkareng regions, with a subsidence of approximately 70 cm for 4 years. Land subsidence is generally related to geological subsidence i.e. sediment consolidation due to its own weight and tectonic movements; or related to human activities such as withdrawal of ground water and geothermal fluid, oil and gas extraction from underground reservoirs, and collapse of underground mines. The amount of subsidence or uplift can be estimated from the number of concentric fringes that appear in the interferogram. This research utilizes Synthetic Aperture Radar (SAR) data observed from ALOS-2 (L-band) and Sentinel-1 (C-band) satellites. By interfering two single look complex (SLC) images from different observation epoch, it is found that the subsided area that has been identified before continues to subside. This occurs especially in Pluit region and has been revealed by interfering ALOS-2 data up to year 2016. The deformation in this area is approximately 12 cm from November 2015 to September 2016. The process of land reclamation also clearly identified by Sentinel-1 image by series data processing in Sentinels Application Platform (SNAP) software.