Evaluating landfast sea ice ridging near UtqiagVik Alaska Using TanDEM-X interferometry

Seasonal landfast sea ice stretches along most Arctic coastlines and serves as a platform for community travel and subsistence, industry operations, and as a habitat for marine mammals. Landfast ice can feature smooth ice and areas of m-scale roughness in the form of pressure ridges. Such ridges can...

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Published in:Remote Sensing
Main Authors: Marbouti, Marjan, Eriksson, Leif, Dammann, Dyre Oliver, Demchev, Denis, Jones, Joshua M., Berg, Anders, Antropov, Oleg
Language:unknown
Published: 2020
Subjects:
Online Access:https://doi.org/10.3390/RS12081247
https://research.chalmers.se/en/publication/fd2fd3e5-a2f4-4059-9370-70785250fae6
id ftchalmersuniv:oai:research.chalmers.se:517539
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spelling ftchalmersuniv:oai:research.chalmers.se:517539 2024-10-20T14:07:04+00:00 Evaluating landfast sea ice ridging near UtqiagVik Alaska Using TanDEM-X interferometry Marbouti, Marjan Eriksson, Leif Dammann, Dyre Oliver Demchev, Denis Jones, Joshua M. Berg, Anders Antropov, Oleg 2020 text https://doi.org/10.3390/RS12081247 https://research.chalmers.se/en/publication/fd2fd3e5-a2f4-4059-9370-70785250fae6 unknown http://dx.doi.org/10.3390/RS12081247 Remote Sensing Meteorology and Atmospheric Sciences Geosciences Multidisciplinary TanDEM-X Synthetic aperture radar InSAR Landfast sea ice Sea ice 2020 ftchalmersuniv https://doi.org/10.3390/RS12081247 2024-10-08T15:50:57Z Seasonal landfast sea ice stretches along most Arctic coastlines and serves as a platform for community travel and subsistence, industry operations, and as a habitat for marine mammals. Landfast ice can feature smooth ice and areas of m-scale roughness in the form of pressure ridges. Such ridges can significantly hamper trafficability, but if grounded can also serve to stabilize the shoreward ice. We investigate the use of synthetic aperture radar interferometry (InSAR) to assess the formation and movement of ridges in the landfast sea ice near Utqiagvik, Alaska. The evaluation is based on the InSAR-derived surface elevation change between two TanDEM-X bistatic image pairs acquired during January 2012. We compare the results with backscatter intensity, coastal radar data, and SAR-derived ice drift and evaluate the utility of this approach and its relevance for evaluation of ridge properties, as well as landfast sea ice evolution, dynamics, and stability. © 2020 by the authors. Other/Unknown Material Arctic Sea ice Alaska Chalmers University of Technology: Chalmers research Arctic Remote Sensing 12 8 1247
institution Open Polar
collection Chalmers University of Technology: Chalmers research
op_collection_id ftchalmersuniv
language unknown
topic Remote Sensing
Meteorology and Atmospheric Sciences
Geosciences
Multidisciplinary
TanDEM-X
Synthetic aperture radar
InSAR
Landfast sea ice
Sea ice
spellingShingle Remote Sensing
Meteorology and Atmospheric Sciences
Geosciences
Multidisciplinary
TanDEM-X
Synthetic aperture radar
InSAR
Landfast sea ice
Sea ice
Marbouti, Marjan
Eriksson, Leif
Dammann, Dyre Oliver
Demchev, Denis
Jones, Joshua M.
Berg, Anders
Antropov, Oleg
Evaluating landfast sea ice ridging near UtqiagVik Alaska Using TanDEM-X interferometry
topic_facet Remote Sensing
Meteorology and Atmospheric Sciences
Geosciences
Multidisciplinary
TanDEM-X
Synthetic aperture radar
InSAR
Landfast sea ice
Sea ice
description Seasonal landfast sea ice stretches along most Arctic coastlines and serves as a platform for community travel and subsistence, industry operations, and as a habitat for marine mammals. Landfast ice can feature smooth ice and areas of m-scale roughness in the form of pressure ridges. Such ridges can significantly hamper trafficability, but if grounded can also serve to stabilize the shoreward ice. We investigate the use of synthetic aperture radar interferometry (InSAR) to assess the formation and movement of ridges in the landfast sea ice near Utqiagvik, Alaska. The evaluation is based on the InSAR-derived surface elevation change between two TanDEM-X bistatic image pairs acquired during January 2012. We compare the results with backscatter intensity, coastal radar data, and SAR-derived ice drift and evaluate the utility of this approach and its relevance for evaluation of ridge properties, as well as landfast sea ice evolution, dynamics, and stability. © 2020 by the authors.
author Marbouti, Marjan
Eriksson, Leif
Dammann, Dyre Oliver
Demchev, Denis
Jones, Joshua M.
Berg, Anders
Antropov, Oleg
author_facet Marbouti, Marjan
Eriksson, Leif
Dammann, Dyre Oliver
Demchev, Denis
Jones, Joshua M.
Berg, Anders
Antropov, Oleg
author_sort Marbouti, Marjan
title Evaluating landfast sea ice ridging near UtqiagVik Alaska Using TanDEM-X interferometry
title_short Evaluating landfast sea ice ridging near UtqiagVik Alaska Using TanDEM-X interferometry
title_full Evaluating landfast sea ice ridging near UtqiagVik Alaska Using TanDEM-X interferometry
title_fullStr Evaluating landfast sea ice ridging near UtqiagVik Alaska Using TanDEM-X interferometry
title_full_unstemmed Evaluating landfast sea ice ridging near UtqiagVik Alaska Using TanDEM-X interferometry
title_sort evaluating landfast sea ice ridging near utqiagvik alaska using tandem-x interferometry
publishDate 2020
url https://doi.org/10.3390/RS12081247
https://research.chalmers.se/en/publication/fd2fd3e5-a2f4-4059-9370-70785250fae6
geographic Arctic
geographic_facet Arctic
genre Arctic
Sea ice
Alaska
genre_facet Arctic
Sea ice
Alaska
op_relation http://dx.doi.org/10.3390/RS12081247
op_doi https://doi.org/10.3390/RS12081247
container_title Remote Sensing
container_volume 12
container_issue 8
container_start_page 1247
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