Multi-Temporal InSAR Analysis for Monitoring Ground Deformation in Amorgos Island, Greece

Radar Interferometry is a widely used method for estimating ground deformation, as it provides precision to a few millimeters to centimeters, and at the same time, a wide spatial coverage of the study area. On 9 July 1956, one of the strongest earthquakes of the 20th century in the area of the South...

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Main Authors: Stavroula Alatza, Ioannis Papoutsis, Demitris Paradissis, Charalampos Kontoes, Gerassimos A. Papadopoulos
Format: Article
Language:English
Published: MDPI AG 2020-01-01
Series:Sensors
Subjects:
Online Access:https://www.mdpi.com/1424-8220/20/2/338
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spelling doaj-a5c38ecfc2754118be19bb140975c0ac2020-11-25T03:00:54ZengMDPI AGSensors1424-82202020-01-0120233810.3390/s20020338s20020338Multi-Temporal InSAR Analysis for Monitoring Ground Deformation in Amorgos Island, GreeceStavroula Alatza0Ioannis Papoutsis1Demitris Paradissis2Charalampos Kontoes3Gerassimos A. Papadopoulos4Higher Geodesy Laboratory and Dionysos Satellite Observatory, School of Rural and Surveying Engineering, National Technical University of Athens, 9 Iroon Polytechniou str, 15780 Zographos, GreeceInstitute for Astronomy, Astrophysics, Space Applications & Remote Sensing, National Observatory of Athens, Vas. Pavlou & I. Metaxa str, 15236 Penteli, GreeceHigher Geodesy Laboratory and Dionysos Satellite Observatory, School of Rural and Surveying Engineering, National Technical University of Athens, 9 Iroon Polytechniou str, 15780 Zographos, GreeceInstitute for Astronomy, Astrophysics, Space Applications & Remote Sensing, National Observatory of Athens, Vas. Pavlou & I. Metaxa str, 15236 Penteli, GreeceInternational Society for the Prevention & Mitigation of Natural Hazards, 10681 Athens, GreeceRadar Interferometry is a widely used method for estimating ground deformation, as it provides precision to a few millimeters to centimeters, and at the same time, a wide spatial coverage of the study area. On 9 July 1956, one of the strongest earthquakes of the 20th century in the area of the South Aegean, occurred in Amorgos, with a magnitude of Mw = 7.7. The objective of this research is to map ground deformation in Amorgos island, using InSAR techniques. We conducted a multi-temporal analysis of all available data from 2003 to 2019 by exploiting historical ENVISAT SAR imagery, as well as the dense archive of Sentinel-1 SLC imagery. Persistent Scatterer Interferometry (PS) and Small Baseline Subset (SBAS) methods were implemented. Results of both data-sets indicate a small-scale deformation on the island. A multi-track analysis was implemented on Sentinel-1 data to decompose the line of sight velocities to vertical and horizontal. The central south coast is experiencing horizontal movement, while uplift of a maximum value of 5 mm/y is observed in the southeastern coast. The combination of the good spatial coverage achievable via InSAR, with GPS measurements, is suggested an important tool for the seamless monitoring of Amorgos island towards tectonic hazard estimation.https://www.mdpi.com/1424-8220/20/2/338sar interferometryamorgos 1956 earthquakesentinel-1timeseries analysislos decompositionground deformation
collection DOAJ
language English
format Article
sources DOAJ
author Stavroula Alatza
Ioannis Papoutsis
Demitris Paradissis
Charalampos Kontoes
Gerassimos A. Papadopoulos
spellingShingle Stavroula Alatza
Ioannis Papoutsis
Demitris Paradissis
Charalampos Kontoes
Gerassimos A. Papadopoulos
Multi-Temporal InSAR Analysis for Monitoring Ground Deformation in Amorgos Island, Greece
Sensors
sar interferometry
amorgos 1956 earthquake
sentinel-1
timeseries analysis
los decomposition
ground deformation
author_facet Stavroula Alatza
Ioannis Papoutsis
Demitris Paradissis
Charalampos Kontoes
Gerassimos A. Papadopoulos
author_sort Stavroula Alatza
title Multi-Temporal InSAR Analysis for Monitoring Ground Deformation in Amorgos Island, Greece
title_short Multi-Temporal InSAR Analysis for Monitoring Ground Deformation in Amorgos Island, Greece
title_full Multi-Temporal InSAR Analysis for Monitoring Ground Deformation in Amorgos Island, Greece
title_fullStr Multi-Temporal InSAR Analysis for Monitoring Ground Deformation in Amorgos Island, Greece
title_full_unstemmed Multi-Temporal InSAR Analysis for Monitoring Ground Deformation in Amorgos Island, Greece
title_sort multi-temporal insar analysis for monitoring ground deformation in amorgos island, greece
publisher MDPI AG
series Sensors
issn 1424-8220
publishDate 2020-01-01
description Radar Interferometry is a widely used method for estimating ground deformation, as it provides precision to a few millimeters to centimeters, and at the same time, a wide spatial coverage of the study area. On 9 July 1956, one of the strongest earthquakes of the 20th century in the area of the South Aegean, occurred in Amorgos, with a magnitude of Mw = 7.7. The objective of this research is to map ground deformation in Amorgos island, using InSAR techniques. We conducted a multi-temporal analysis of all available data from 2003 to 2019 by exploiting historical ENVISAT SAR imagery, as well as the dense archive of Sentinel-1 SLC imagery. Persistent Scatterer Interferometry (PS) and Small Baseline Subset (SBAS) methods were implemented. Results of both data-sets indicate a small-scale deformation on the island. A multi-track analysis was implemented on Sentinel-1 data to decompose the line of sight velocities to vertical and horizontal. The central south coast is experiencing horizontal movement, while uplift of a maximum value of 5 mm/y is observed in the southeastern coast. The combination of the good spatial coverage achievable via InSAR, with GPS measurements, is suggested an important tool for the seamless monitoring of Amorgos island towards tectonic hazard estimation.
topic sar interferometry
amorgos 1956 earthquake
sentinel-1
timeseries analysis
los decomposition
ground deformation
url https://www.mdpi.com/1424-8220/20/2/338
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