Ground-Based Radar Interferometry of Sea Ice

In light of recent Arctic change, there is a need to better understand sea ice dynamic processes at the floe scale to evaluate sea ice stability, deformation, and fracturing. This work investigates the use of the Gamma portable radar interferometer (GPRI) to characterize sea ice displacement and sur...

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Published in:Remote Sensing
Main Authors: Dyre Oliver Dammann, Mark A. Johnson, Emily R. Fedders, Andrew R. Mahoney, Charles L. Werner, Christopher M. Polashenski, Franz J. Meyer, Jennifer K. Hutchings
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2020
Subjects:
Online Access:https://doi.org/10.3390/rs13010043
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spelling ftmdpi:oai:mdpi.com:/2072-4292/13/1/43/ 2023-08-20T04:04:38+02:00 Ground-Based Radar Interferometry of Sea Ice Dyre Oliver Dammann Mark A. Johnson Emily R. Fedders Andrew R. Mahoney Charles L. Werner Christopher M. Polashenski Franz J. Meyer Jennifer K. Hutchings agris 2020-12-24 application/pdf https://doi.org/10.3390/rs13010043 EN eng Multidisciplinary Digital Publishing Institute Environmental Remote Sensing https://dx.doi.org/10.3390/rs13010043 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 13; Issue 1; Pages: 43 sea ice deformation remote sensing radar interferometry GPRI Text 2020 ftmdpi https://doi.org/10.3390/rs13010043 2023-08-01T00:43:47Z In light of recent Arctic change, there is a need to better understand sea ice dynamic processes at the floe scale to evaluate sea ice stability, deformation, and fracturing. This work investigates the use of the Gamma portable radar interferometer (GPRI) to characterize sea ice displacement and surface topography. We find that the GPRI is best suited to derive lateral surface deformation due to mm-scale horizontal accuracy. We model interferometric phase signatures from sea ice displacement and evaluate possible errors related to noise and antenna motion. We compare the analysis with observations acquired during a drifting ice camp in the Beaufort Sea. We used repeat-scan and stare-mode interferometry to identify two-dimensional shear and to track continuous uni-directional convergence. This paper demonstrates the capacity of the GPRI to derive surface strain on the order of 10−7 and identify different dynamic regions based on sub-mm changes in displacement. The GPRI is thus a promising tool for sea ice applications due to its high accuracy that can potentially resolve pre- and post-fracture deformation relevant to sea ice stability and modeling. Text Arctic Beaufort Sea Sea ice MDPI Open Access Publishing Arctic Remote Sensing 13 1 43
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic sea ice
deformation
remote sensing
radar
interferometry
GPRI
spellingShingle sea ice
deformation
remote sensing
radar
interferometry
GPRI
Dyre Oliver Dammann
Mark A. Johnson
Emily R. Fedders
Andrew R. Mahoney
Charles L. Werner
Christopher M. Polashenski
Franz J. Meyer
Jennifer K. Hutchings
Ground-Based Radar Interferometry of Sea Ice
topic_facet sea ice
deformation
remote sensing
radar
interferometry
GPRI
description In light of recent Arctic change, there is a need to better understand sea ice dynamic processes at the floe scale to evaluate sea ice stability, deformation, and fracturing. This work investigates the use of the Gamma portable radar interferometer (GPRI) to characterize sea ice displacement and surface topography. We find that the GPRI is best suited to derive lateral surface deformation due to mm-scale horizontal accuracy. We model interferometric phase signatures from sea ice displacement and evaluate possible errors related to noise and antenna motion. We compare the analysis with observations acquired during a drifting ice camp in the Beaufort Sea. We used repeat-scan and stare-mode interferometry to identify two-dimensional shear and to track continuous uni-directional convergence. This paper demonstrates the capacity of the GPRI to derive surface strain on the order of 10−7 and identify different dynamic regions based on sub-mm changes in displacement. The GPRI is thus a promising tool for sea ice applications due to its high accuracy that can potentially resolve pre- and post-fracture deformation relevant to sea ice stability and modeling.
format Text
author Dyre Oliver Dammann
Mark A. Johnson
Emily R. Fedders
Andrew R. Mahoney
Charles L. Werner
Christopher M. Polashenski
Franz J. Meyer
Jennifer K. Hutchings
author_facet Dyre Oliver Dammann
Mark A. Johnson
Emily R. Fedders
Andrew R. Mahoney
Charles L. Werner
Christopher M. Polashenski
Franz J. Meyer
Jennifer K. Hutchings
author_sort Dyre Oliver Dammann
title Ground-Based Radar Interferometry of Sea Ice
title_short Ground-Based Radar Interferometry of Sea Ice
title_full Ground-Based Radar Interferometry of Sea Ice
title_fullStr Ground-Based Radar Interferometry of Sea Ice
title_full_unstemmed Ground-Based Radar Interferometry of Sea Ice
title_sort ground-based radar interferometry of sea ice
publisher Multidisciplinary Digital Publishing Institute
publishDate 2020
url https://doi.org/10.3390/rs13010043
op_coverage agris
geographic Arctic
geographic_facet Arctic
genre Arctic
Beaufort Sea
Sea ice
genre_facet Arctic
Beaufort Sea
Sea ice
op_source Remote Sensing; Volume 13; Issue 1; Pages: 43
op_relation Environmental Remote Sensing
https://dx.doi.org/10.3390/rs13010043
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs13010043
container_title Remote Sensing
container_volume 13
container_issue 1
container_start_page 43
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