Analysis of Magma Activity during the Cerro Azul Volcanic Unrest in March 2017 Using Sentinel-1 DInSAR Observations

Cerro Azul volcano, one of the most active volcanoes in the Galpagos Archipelago, exhibited significant unrest in March 2017, marked by dramatic displacement around the caldera and on the southeastern plain.This study applied differential interferometric synthetic aperture radar (DInSAR) technique to SAR image pairs acquired from the Sentinel-1A satellite's ascending and descending nodes to measure the line-of-sight (LOS) and two-dimensional (up-down and east-west) displacements during the 2017 unrest of the volcano.Extensive concentric fringe patterns were observed around the caldera and on the southeastern plain of Cerro Azul volcano, indicating LOS displacements away from and toward the satellite, respectively.Two-dimensional displacements revealed that the volcanic body around the caldera contracted, while the southeastern plain uplifted and expanded.To further characterize magmatic activity during the unrest, we inverted LOS displacements from both ascending and descending observations using Mogi and Sill source models.The surface displacements simulated from the optimal magma source parameters obtained through inversion showed a normalized root mean square error of less than 5% compared to the DInSAR-observed displacements, confirming the reliability of the inversion results.The Mogi source was located approximately 4.7 km beneath the northeastern caldera rim of Cerro Azul and exhibited a volume change of -31 10 6 m 3 .The Sill source, characterized by a long rectangular shape approximately 10 km in length and 1 km in width, was situated about 7 km beneath the southeastern plain and showed a volume change of 68 10 6 m 3 .The volume increase of the Sill source was approximately twice that of the volume decrease of the Mogi source.Results of this study suggest that magma intrusion into the southeastern plain, originating from the Mogi source and deeper magma reservoirs, likely drove https://www.kjrs.org

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Journal
Korean Journal of Remote Sensing
Published
2024-12-31
DOI
https://doi.org/10.7780/kjrs.2024.40.6.1.4
Citations
1
Primary Topic
Earthquake Detection and Analysis
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article
Field-Weighted Citation Impact
0.53

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article

Analysis of Magma Activity during the Cerro Azul Volcanic Unrest in March 2017 Using Sentinel-1 DInSAR Observations

Hyangsun Han, Jinwoo Kim, Young‐Beom Jeon, Seohyeon Kim et al.
1 citations
Korean Journal of Remote Sensing
Earthquake Detection and Analysis
0.53
article

Analysis of Magma Activity during the Cerro Azul Volcanic Unrest in March 2017 Using Sentinel-1 DInSAR Observations

Hyangsun Han, Jinwoo Kim, Young‐Beom Jeon, Seohyeon Kim, S. Lee
article en
1 citations

Abstract

Cerro Azul volcano, one of the most active volcanoes in the Galpagos Archipelago, exhibited significant unrest in March 2017, marked by dramatic displacement around the caldera and on the southeastern plain.This study applied differential interferometric synthetic aperture radar (DInSAR) technique to SAR image pairs acquired from the Sentinel-1A satellite's ascending and descending nodes to measure the line-of-sight (LOS) and two-dimensional (up-down and east-west) displacements during the 2017 unrest of the volcano.Extensive concentric fringe patterns were observed around the caldera and on the southeastern plain of Cerro Azul volcano, indicating LOS displacements away from and toward the satellite, respectively.Two-dimensional displacements revealed that the volcanic body around the caldera contracted, while the southeastern plain uplifted and expanded.To further characterize magmatic activity during the unrest, we inverted LOS displacements from both ascending and descending observations using Mogi and Sill source models.The surface displacements simulated from the optimal magma source parameters obtained through inversion showed a normalized root mean square error of less than 5% compared to the DInSAR-observed displacements, confirming the reliability of the inversion results.The Mogi source was located approximately 4.7 km beneath the northeastern caldera rim of Cerro Azul and exhibited a volume change of -31 10 6 m 3 .The Sill source, characterized by a long rectangular shape approximately 10 km in length and 1 km in width, was situated about 7 km beneath the southeastern plain and showed a volume change of 68 10 6 m 3 .The volume increase of the Sill source was approximately twice that of the volume decrease of the Mogi source.Results of this study suggest that magma intrusion into the southeastern plain, originating from the Mogi source and deeper magma reservoirs, likely drove https://www.kjrs.org

Korean Journal of Remote SensingVol. 40(6)
Kangwon National University (KR)
National Research Foundation of Korea, Ministry of the Interior and Safety, Ministry of SMEs and Startups
Climate action
Openalex Percentile: Top 31%
Earthquake Detection and Analysis
0.53
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