3D SAR Speckle Offset Tracking Potential for Monitoring Landfast Ice Growth and Displacement

This study investigates the growth and displacement of landfast ice along the shoreline of the Mackenzie Delta in Northwest Territories, Canada, by synthetic aperture radar (SAR) speckle offset tracking (SPO). Three-dimensional (3D) offsets were reconstructed from Sentinel-1 ascending and descending...

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Published in:Remote Sensing
Main Authors: Byung-Hun Choe, Sergey Samsonov, Jungkyo Jung
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2021
Subjects:
Online Access:https://doi.org/10.3390/rs13112168
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spelling ftmdpi:oai:mdpi.com:/2072-4292/13/11/2168/ 2023-08-20T04:07:54+02:00 3D SAR Speckle Offset Tracking Potential for Monitoring Landfast Ice Growth and Displacement Byung-Hun Choe Sergey Samsonov Jungkyo Jung agris 2021-06-01 application/pdf https://doi.org/10.3390/rs13112168 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/rs13112168 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 13; Issue 11; Pages: 2168 SAR speckle offset tracking 3D time-series analysis landfast ice growth Mackenzie Delta Sentinel-1 Text 2021 ftmdpi https://doi.org/10.3390/rs13112168 2023-08-01T01:51:37Z This study investigates the growth and displacement of landfast ice along the shoreline of the Mackenzie Delta in Northwest Territories, Canada, by synthetic aperture radar (SAR) speckle offset tracking (SPO). Three-dimensional (3D) offsets were reconstructed from Sentinel-1 ascending and descending SAR images acquired on the same dates during the November 2017–April 2018 and October 2018–May 2019 annual cycles. The analysis revealed both horizontal and vertical offsets. The annual horizontal offsets of up to ~8 m are interpreted as landfast ice displacements caused by wind and ocean currents. The annual vertical offsets of approximately −1 to −2 m were observed from landfast ice, which are likely due to longer radar penetration up to the ice–water interface with increasing landfast ice thickness. Numerical ice thickness model estimates supported the conclusion that the cumulative vertical negative offsets correspond to the growth of freshwater ice. Time-series analysis showed that the significant growth and displacement of landfast ice in the Mackenzie Delta occurred between November and January during the 2017–2018 and 2018–2019 cycles. Text Mackenzie Delta Northwest Territories MDPI Open Access Publishing Northwest Territories Canada Mackenzie Delta ENVELOPE(-136.672,-136.672,68.833,68.833) Remote Sensing 13 11 2168
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic SAR speckle offset tracking
3D time-series analysis
landfast ice growth
Mackenzie Delta
Sentinel-1
spellingShingle SAR speckle offset tracking
3D time-series analysis
landfast ice growth
Mackenzie Delta
Sentinel-1
Byung-Hun Choe
Sergey Samsonov
Jungkyo Jung
3D SAR Speckle Offset Tracking Potential for Monitoring Landfast Ice Growth and Displacement
topic_facet SAR speckle offset tracking
3D time-series analysis
landfast ice growth
Mackenzie Delta
Sentinel-1
description This study investigates the growth and displacement of landfast ice along the shoreline of the Mackenzie Delta in Northwest Territories, Canada, by synthetic aperture radar (SAR) speckle offset tracking (SPO). Three-dimensional (3D) offsets were reconstructed from Sentinel-1 ascending and descending SAR images acquired on the same dates during the November 2017–April 2018 and October 2018–May 2019 annual cycles. The analysis revealed both horizontal and vertical offsets. The annual horizontal offsets of up to ~8 m are interpreted as landfast ice displacements caused by wind and ocean currents. The annual vertical offsets of approximately −1 to −2 m were observed from landfast ice, which are likely due to longer radar penetration up to the ice–water interface with increasing landfast ice thickness. Numerical ice thickness model estimates supported the conclusion that the cumulative vertical negative offsets correspond to the growth of freshwater ice. Time-series analysis showed that the significant growth and displacement of landfast ice in the Mackenzie Delta occurred between November and January during the 2017–2018 and 2018–2019 cycles.
format Text
author Byung-Hun Choe
Sergey Samsonov
Jungkyo Jung
author_facet Byung-Hun Choe
Sergey Samsonov
Jungkyo Jung
author_sort Byung-Hun Choe
title 3D SAR Speckle Offset Tracking Potential for Monitoring Landfast Ice Growth and Displacement
title_short 3D SAR Speckle Offset Tracking Potential for Monitoring Landfast Ice Growth and Displacement
title_full 3D SAR Speckle Offset Tracking Potential for Monitoring Landfast Ice Growth and Displacement
title_fullStr 3D SAR Speckle Offset Tracking Potential for Monitoring Landfast Ice Growth and Displacement
title_full_unstemmed 3D SAR Speckle Offset Tracking Potential for Monitoring Landfast Ice Growth and Displacement
title_sort 3d sar speckle offset tracking potential for monitoring landfast ice growth and displacement
publisher Multidisciplinary Digital Publishing Institute
publishDate 2021
url https://doi.org/10.3390/rs13112168
op_coverage agris
long_lat ENVELOPE(-136.672,-136.672,68.833,68.833)
geographic Northwest Territories
Canada
Mackenzie Delta
geographic_facet Northwest Territories
Canada
Mackenzie Delta
genre Mackenzie Delta
Northwest Territories
genre_facet Mackenzie Delta
Northwest Territories
op_source Remote Sensing; Volume 13; Issue 11; Pages: 2168
op_relation https://dx.doi.org/10.3390/rs13112168
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs13112168
container_title Remote Sensing
container_volume 13
container_issue 11
container_start_page 2168
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