Mapping Surface Deformation Over Tatun Volcano Group, Northern Taiwan Using Multitemporal InSAR

The Tatun Volcano Group (TVG) is located at the northern coast of Taiwan Island with only 15 km to the Taipei metropolis. Recent geothermal and geochemical studies suggest that the TVG is dormant-active rather than extinct, implying the eruption potential to devastate the nearby area of 7 million in...

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Main Authors: Hongyu Liang, Xin Li, Rou-Fei Chen
Format: Article
Language:English
Published: IEEE 2021-01-01
Series:IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing
Subjects:
Online Access:https://ieeexplore.ieee.org/document/9321539/
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author Hongyu Liang
Xin Li
Rou-Fei Chen
author_facet Hongyu Liang
Xin Li
Rou-Fei Chen
author_sort Hongyu Liang
collection DOAJ
description The Tatun Volcano Group (TVG) is located at the northern coast of Taiwan Island with only 15 km to the Taipei metropolis. Recent geothermal and geochemical studies suggest that the TVG is dormant-active rather than extinct, implying the eruption potential to devastate the nearby area of 7 million inhabitants. Although some geodetic tools (e.g., global positioning system and precise leveling) have been utilized to analyze the activity associated with volcanism, it is still challenging for conventional interferometric synthetic aperture radar (InSAR) technique to obtain clear ground surface movement at the TVG due to decorrelation and complex atmospheric delay. In this study, we present an improved multi-temporal InSAR (MTInSAR) approach to explore the temporal evolution and spatial extent of displacement at the TVG from 19 L-band ALOS/PALSAR images acquired between 2007 and 2011. Stratified atmospheric delays and orbit error are corrected with a patch-based joint model as different phase components can be separated according to their distinct spatiotemporal characteristics. The spatial deformation patterns indicate an uplift of 10 mm/year at the SW-NE ridge and subsidence with a rate of 10 mm/year at the E-W ridge. The temporal deformation variations at Mt. Chihshin and Huangzuei have high similarity with correlation coefficients of 0.9 above. This indicates that the subsidence at Mts. Chihshin and Huangzuei might be caused by released hydrothermal fluids related to tectono-magmatic activity within the hydrothermal system beneath the TVG.
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spelling doaj.art-c9057326a59a45ab9c6bfe500197ede22022-12-21T22:52:56ZengIEEEIEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing2151-15352021-01-01142087209510.1109/JSTARS.2021.30506449321539Mapping Surface Deformation Over Tatun Volcano Group, Northern Taiwan Using Multitemporal InSARHongyu Liang0https://orcid.org/0000-0002-6410-1631Xin Li1https://orcid.org/0000-0001-8953-4516Rou-Fei Chen2College of Surveying and Geo-Informatics, Tongji University, Shanghai, ChinaState Key Laboratory of Resources and Environmental Information System, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, ChinaDepartment of Materials and Mineral Resources Engineering, National Taipei University of Technology, Taipei, TaiwanThe Tatun Volcano Group (TVG) is located at the northern coast of Taiwan Island with only 15 km to the Taipei metropolis. Recent geothermal and geochemical studies suggest that the TVG is dormant-active rather than extinct, implying the eruption potential to devastate the nearby area of 7 million inhabitants. Although some geodetic tools (e.g., global positioning system and precise leveling) have been utilized to analyze the activity associated with volcanism, it is still challenging for conventional interferometric synthetic aperture radar (InSAR) technique to obtain clear ground surface movement at the TVG due to decorrelation and complex atmospheric delay. In this study, we present an improved multi-temporal InSAR (MTInSAR) approach to explore the temporal evolution and spatial extent of displacement at the TVG from 19 L-band ALOS/PALSAR images acquired between 2007 and 2011. Stratified atmospheric delays and orbit error are corrected with a patch-based joint model as different phase components can be separated according to their distinct spatiotemporal characteristics. The spatial deformation patterns indicate an uplift of 10 mm/year at the SW-NE ridge and subsidence with a rate of 10 mm/year at the E-W ridge. The temporal deformation variations at Mt. Chihshin and Huangzuei have high similarity with correlation coefficients of 0.9 above. This indicates that the subsidence at Mts. Chihshin and Huangzuei might be caused by released hydrothermal fluids related to tectono-magmatic activity within the hydrothermal system beneath the TVG.https://ieeexplore.ieee.org/document/9321539/Interferometric synthetic aperture radar (InSAR)orbital errorTatun Volcano Group (TVG)tropospheric delay
spellingShingle Hongyu Liang
Xin Li
Rou-Fei Chen
Mapping Surface Deformation Over Tatun Volcano Group, Northern Taiwan Using Multitemporal InSAR
IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing
Interferometric synthetic aperture radar (InSAR)
orbital error
Tatun Volcano Group (TVG)
tropospheric delay
title Mapping Surface Deformation Over Tatun Volcano Group, Northern Taiwan Using Multitemporal InSAR
title_full Mapping Surface Deformation Over Tatun Volcano Group, Northern Taiwan Using Multitemporal InSAR
title_fullStr Mapping Surface Deformation Over Tatun Volcano Group, Northern Taiwan Using Multitemporal InSAR
title_full_unstemmed Mapping Surface Deformation Over Tatun Volcano Group, Northern Taiwan Using Multitemporal InSAR
title_short Mapping Surface Deformation Over Tatun Volcano Group, Northern Taiwan Using Multitemporal InSAR
title_sort mapping surface deformation over tatun volcano group northern taiwan using multitemporal insar
topic Interferometric synthetic aperture radar (InSAR)
orbital error
Tatun Volcano Group (TVG)
tropospheric delay
url https://ieeexplore.ieee.org/document/9321539/
work_keys_str_mv AT hongyuliang mappingsurfacedeformationovertatunvolcanogroupnortherntaiwanusingmultitemporalinsar
AT xinli mappingsurfacedeformationovertatunvolcanogroupnortherntaiwanusingmultitemporalinsar
AT roufeichen mappingsurfacedeformationovertatunvolcanogroupnortherntaiwanusingmultitemporalinsar