Surface deformation monitoring of Sinabung volcano using multi temporal InSAR method and GIS analysis for affected area assessment

3rd International Conference on Science, Technology, and Interdisciplinary Research

自然科学;工业技术

Aditiya, A.^1,4 ; Aoki, Y.^2 ; Anugrah, R.D.^3

Civil Engineering Department, University of Tokyo, Tokyo

151-0063, Japan^1

Earthquake Research Institute, University of Tokyo, Tokyo

151-0063, Japan^2

Urban Engineering Department, University of Tokyo, Tokyo

151-0063, Japan^3

Geospatial Information Agency of Indonesia, Jl. Raya Jakarta-Bogor Km. 46, Cibinong, Indonesia^4

关键词: Disaster reduction;    High spatial resolution;    Interferometric synthetic aperture radars;    Observation Period;    Phase unwrapping;    Surface deformation;    Time series method;    Volcanic activities;   

Others  :  https://iopscience.iop.org/article/10.1088/1757-899X/344/1/012003/pdf
DOI  :  10.1088/1757-899X/344/1/012003

来源: IOP

【 摘 要 】

Sinabung Volcano which located in northern part of Sumatera island is part of a hundred active volcano in Indonesia. Surface deformation is detected over Sinabung Volcano and surrounded area since the first eruption in 2010 after 400 years long rest. We present multi temporal Interferometric Synthetic Aperture Radar (InSAR) time-series method of ALOS-2 L-band SAR data acquired from December 2014 to July 2017 to reveal surface deformation with high spatial resolution. The method includes focusing the SAR data, generating interferogram and phase unwrapping using SNAPHU tools. The result reveal significant deformation over Sinabung Volcano areas at rates up to 10 cm during observation period and the highest deformation occurs in western part which is trajectory of lava. We concluded the observed deformation primarily caused by volcanic activity respectively after long period of rest. In addition, Geographic Information System (GIS) analysis produces disaster affected areas of Sinabung eruption. GIS is reliable technique to estimate the impact of the hazard scenario to the exposure data and develop scenarios of disaster impacts to inform their contingency and emergency plan. The GIS results include the estimated affected area divided into 3 zones based on pyroclastic lava flow and pyroclastic fall (incandescent rock and ash). The highest impact is occurred in zone II due to many settlements are scattered in this zone. This information will be support stakeholders to take emergency preparation for disaster reduction. The continuation of this high rate of decline tends to endanger the population in next periods.