Elevation Change of CookE2 Subglacial Lake in East Antarctica Observed by DInSAR and Time-Segmented PSInSAR

In this study, elevation change and surface morphology of CookE2, one of the most active subglacial lakes in East Antarctica, were analyzed by using Differential Interferometric Synthetic Aperture Radar (DInSAR) and a newly adapted Time-Segmented Persistent Scatterer Interferometric Synthetic Apertu...

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Published in:Remote Sensing
Main Authors: Jihyun Moon, Hoseung Lee, Hoonyol Lee
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2022
Subjects:
Online Access:https://doi.org/10.3390/rs14184616
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spelling ftmdpi:oai:mdpi.com:/2072-4292/14/18/4616/ 2023-08-20T04:01:14+02:00 Elevation Change of CookE2 Subglacial Lake in East Antarctica Observed by DInSAR and Time-Segmented PSInSAR Jihyun Moon Hoseung Lee Hoonyol Lee agris 2022-09-15 application/pdf https://doi.org/10.3390/rs14184616 EN eng Multidisciplinary Digital Publishing Institute Environmental Remote Sensing https://dx.doi.org/10.3390/rs14184616 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 14; Issue 18; Pages: 4616 active subglacial lake CookE2 DInSAR PSInSAR TS-PSInSAR Text 2022 ftmdpi https://doi.org/10.3390/rs14184616 2023-08-01T06:29:26Z In this study, elevation change and surface morphology of CookE2, one of the most active subglacial lakes in East Antarctica, were analyzed by using Differential Interferometric Synthetic Aperture Radar (DInSAR) and a newly adapted Time-Segmented Persistent Scatterer Interferometric Synthetic Aperture Radar (TS-PSInSAR) techniques. Firstly, several DInSAR pairs were used to study the surface morphology of the subglacial lake during the rapid discharge event in 2007 and the subsequent recharge in 2010 by using ALOS PALSAR data and the continuous recharge from 2018 to 2020 by using Sentinel-1 SAR data. For time-series observation from 2018 to 2020, however, simple integration of DInSAR deviates largely from the satellite altimeter data because errors from the horizontal flow of the surrounding ice field or atmospheric phase accumulate. Conventional PSInSAR deviates from the altimeter data if the LOS displacement exceeds 300 mm, i.e., approximately 1/4 of the slant range resolution of the Sentinel-1 SAR in Interferometric Wide-swath (IW) mode, during the time window. Therefore, a series of Time-Segmented PSInSAR with a 4-month time window could accurately distinguish 1.10 ± 0.01 m/year of highly linear (R2 = 0.99) surface rise rate of CookE2 and 0.63 m/year of horizontal deformation rate of the surrounding ice field from 2018 to 2020. Text Antarc* Antarctica East Antarctica MDPI Open Access Publishing East Antarctica The Sentinel ENVELOPE(73.317,73.317,-52.983,-52.983) Remote Sensing 14 18 4616
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic active subglacial lake
CookE2
DInSAR
PSInSAR
TS-PSInSAR
spellingShingle active subglacial lake
CookE2
DInSAR
PSInSAR
TS-PSInSAR
Jihyun Moon
Hoseung Lee
Hoonyol Lee
Elevation Change of CookE2 Subglacial Lake in East Antarctica Observed by DInSAR and Time-Segmented PSInSAR
topic_facet active subglacial lake
CookE2
DInSAR
PSInSAR
TS-PSInSAR
description In this study, elevation change and surface morphology of CookE2, one of the most active subglacial lakes in East Antarctica, were analyzed by using Differential Interferometric Synthetic Aperture Radar (DInSAR) and a newly adapted Time-Segmented Persistent Scatterer Interferometric Synthetic Aperture Radar (TS-PSInSAR) techniques. Firstly, several DInSAR pairs were used to study the surface morphology of the subglacial lake during the rapid discharge event in 2007 and the subsequent recharge in 2010 by using ALOS PALSAR data and the continuous recharge from 2018 to 2020 by using Sentinel-1 SAR data. For time-series observation from 2018 to 2020, however, simple integration of DInSAR deviates largely from the satellite altimeter data because errors from the horizontal flow of the surrounding ice field or atmospheric phase accumulate. Conventional PSInSAR deviates from the altimeter data if the LOS displacement exceeds 300 mm, i.e., approximately 1/4 of the slant range resolution of the Sentinel-1 SAR in Interferometric Wide-swath (IW) mode, during the time window. Therefore, a series of Time-Segmented PSInSAR with a 4-month time window could accurately distinguish 1.10 ± 0.01 m/year of highly linear (R2 = 0.99) surface rise rate of CookE2 and 0.63 m/year of horizontal deformation rate of the surrounding ice field from 2018 to 2020.
format Text
author Jihyun Moon
Hoseung Lee
Hoonyol Lee
author_facet Jihyun Moon
Hoseung Lee
Hoonyol Lee
author_sort Jihyun Moon
title Elevation Change of CookE2 Subglacial Lake in East Antarctica Observed by DInSAR and Time-Segmented PSInSAR
title_short Elevation Change of CookE2 Subglacial Lake in East Antarctica Observed by DInSAR and Time-Segmented PSInSAR
title_full Elevation Change of CookE2 Subglacial Lake in East Antarctica Observed by DInSAR and Time-Segmented PSInSAR
title_fullStr Elevation Change of CookE2 Subglacial Lake in East Antarctica Observed by DInSAR and Time-Segmented PSInSAR
title_full_unstemmed Elevation Change of CookE2 Subglacial Lake in East Antarctica Observed by DInSAR and Time-Segmented PSInSAR
title_sort elevation change of cooke2 subglacial lake in east antarctica observed by dinsar and time-segmented psinsar
publisher Multidisciplinary Digital Publishing Institute
publishDate 2022
url https://doi.org/10.3390/rs14184616
op_coverage agris
long_lat ENVELOPE(73.317,73.317,-52.983,-52.983)
geographic East Antarctica
The Sentinel
geographic_facet East Antarctica
The Sentinel
genre Antarc*
Antarctica
East Antarctica
genre_facet Antarc*
Antarctica
East Antarctica
op_source Remote Sensing; Volume 14; Issue 18; Pages: 4616
op_relation Environmental Remote Sensing
https://dx.doi.org/10.3390/rs14184616
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs14184616
container_title Remote Sensing
container_volume 14
container_issue 18
container_start_page 4616
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