X-Band Interferometric SAR Observations of Baltic Fast Ice

Detailed mapping of fast-ice deformation can be used to characterize the rheological behavior of fast ice and subsequently improve sea ice modeling. This study uses interferometric synthetic aperture radar to map fast-ice deformation with unprecedented spatial resolution (meter range) and sensitivit...

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Published in:IEEE Transactions on Geoscience and Remote Sensing
Main Authors: Berg, Anders, Dammert, Patrik, Eriksson, Leif
Language:unknown
Published: 2015
Subjects:
Online Access:https://doi.org/10.1109/TGRS.2014.2336752
https://research.chalmers.se/en/publication/205971
id ftchalmersuniv:oai:research.chalmers.se:205971
record_format openpolar
spelling ftchalmersuniv:oai:research.chalmers.se:205971 2023-05-15T18:17:50+02:00 X-Band Interferometric SAR Observations of Baltic Fast Ice Berg, Anders Dammert, Patrik Eriksson, Leif 2015 text https://doi.org/10.1109/TGRS.2014.2336752 https://research.chalmers.se/en/publication/205971 unknown http://dx.doi.org/10.1109/TGRS.2014.2336752 https://research.chalmers.se/en/publication/205971 Mechanical Engineering Aerospace Engineering Agricultural Science Oceanography Hydrology Water Resources Signal Processing interferometry synthetic aperture radar (SAR) sea ice Displacement measurement rheology 2015 ftchalmersuniv https://doi.org/10.1109/TGRS.2014.2336752 2022-12-11T07:12:48Z Detailed mapping of fast-ice deformation can be used to characterize the rheological behavior of fast ice and subsequently improve sea ice modeling. This study uses interferometric synthetic aperture radar to map fast-ice deformation with unprecedented spatial resolution (meter range) and sensitivity (cm-mm range). Two interferometric acquisitions, each with a temporal baseline of 24 h, were performed by the X-band SAR satellite constellation Cosmo-SkyMed over the northeast Bay of Bothnia in the middle of the 2012 ice season. The first interferogram shows deformation of the fast ice due to force from impinging drift ice, and the normal strain within the fast ice is measured. Complementary intensity correlation measurements reveal a slow movement of the drift ice toward the fast ice. The second interferogram exhibits a low fringe rate over the fast ice with fringes being aligned along the coastline. Deformation appears to be stronger around leads, skerries, and grounded ice ridges. It is also observed that the coherence images provide information that is complementary to the information in the backscatter images. Other/Unknown Material Sea ice Chalmers University of Technology: Chalmers research Northeast Bay ENVELOPE(-104.084,-104.084,56.583,56.583) IEEE Transactions on Geoscience and Remote Sensing 53 3 1248 1256
institution Open Polar
collection Chalmers University of Technology: Chalmers research
op_collection_id ftchalmersuniv
language unknown
topic Mechanical Engineering
Aerospace Engineering
Agricultural Science
Oceanography
Hydrology
Water Resources
Signal Processing
interferometry
synthetic aperture radar (SAR)
sea ice
Displacement measurement
rheology
spellingShingle Mechanical Engineering
Aerospace Engineering
Agricultural Science
Oceanography
Hydrology
Water Resources
Signal Processing
interferometry
synthetic aperture radar (SAR)
sea ice
Displacement measurement
rheology
Berg, Anders
Dammert, Patrik
Eriksson, Leif
X-Band Interferometric SAR Observations of Baltic Fast Ice
topic_facet Mechanical Engineering
Aerospace Engineering
Agricultural Science
Oceanography
Hydrology
Water Resources
Signal Processing
interferometry
synthetic aperture radar (SAR)
sea ice
Displacement measurement
rheology
description Detailed mapping of fast-ice deformation can be used to characterize the rheological behavior of fast ice and subsequently improve sea ice modeling. This study uses interferometric synthetic aperture radar to map fast-ice deformation with unprecedented spatial resolution (meter range) and sensitivity (cm-mm range). Two interferometric acquisitions, each with a temporal baseline of 24 h, were performed by the X-band SAR satellite constellation Cosmo-SkyMed over the northeast Bay of Bothnia in the middle of the 2012 ice season. The first interferogram shows deformation of the fast ice due to force from impinging drift ice, and the normal strain within the fast ice is measured. Complementary intensity correlation measurements reveal a slow movement of the drift ice toward the fast ice. The second interferogram exhibits a low fringe rate over the fast ice with fringes being aligned along the coastline. Deformation appears to be stronger around leads, skerries, and grounded ice ridges. It is also observed that the coherence images provide information that is complementary to the information in the backscatter images.
author Berg, Anders
Dammert, Patrik
Eriksson, Leif
author_facet Berg, Anders
Dammert, Patrik
Eriksson, Leif
author_sort Berg, Anders
title X-Band Interferometric SAR Observations of Baltic Fast Ice
title_short X-Band Interferometric SAR Observations of Baltic Fast Ice
title_full X-Band Interferometric SAR Observations of Baltic Fast Ice
title_fullStr X-Band Interferometric SAR Observations of Baltic Fast Ice
title_full_unstemmed X-Band Interferometric SAR Observations of Baltic Fast Ice
title_sort x-band interferometric sar observations of baltic fast ice
publishDate 2015
url https://doi.org/10.1109/TGRS.2014.2336752
https://research.chalmers.se/en/publication/205971
long_lat ENVELOPE(-104.084,-104.084,56.583,56.583)
geographic Northeast Bay
geographic_facet Northeast Bay
genre Sea ice
genre_facet Sea ice
op_relation http://dx.doi.org/10.1109/TGRS.2014.2336752
https://research.chalmers.se/en/publication/205971
op_doi https://doi.org/10.1109/TGRS.2014.2336752
container_title IEEE Transactions on Geoscience and Remote Sensing
container_volume 53
container_issue 3
container_start_page 1248
op_container_end_page 1256
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