Comparison of ice/water classification in Fram Strait from C- A nd L-band SAR imagery

In this paper an algorithm for ice/water classification of C- A nd L-band dual polarization synthetic aperture radar data is presented. A comparison of the two different frequencies is made in order to investigate the potential to improve classification results with multi-frequency data. The algorit...

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Published in:Annals of Glaciology
Main Authors: Aldenhoff, Wiebke, Heuzé, Céline, Eriksson, Leif
Language:unknown
Published: 2018
Subjects:
Online Access:https://doi.org/10.1017/aog.2018.7
https://research.chalmers.se/en/publication/0818bf50-cdeb-4fef-8bde-906c2022c2c7
id ftchalmersuniv:oai:research.chalmers.se:504649
record_format openpolar
spelling ftchalmersuniv:oai:research.chalmers.se:504649 2023-05-15T16:18:07+02:00 Comparison of ice/water classification in Fram Strait from C- A nd L-band SAR imagery Aldenhoff, Wiebke Heuzé, Céline Eriksson, Leif 2018 text https://doi.org/10.1017/aog.2018.7 https://research.chalmers.se/en/publication/0818bf50-cdeb-4fef-8bde-906c2022c2c7 unknown http://dx.doi.org/10.1017/aog.2018.7 https://research.chalmers.se/en/publication/0818bf50-cdeb-4fef-8bde-906c2022c2c7 Remote Sensing Geophysics Geosciences Multidisciplinary polar and subpolar oceans sea ice ice and climate 2018 ftchalmersuniv https://doi.org/10.1017/aog.2018.7 2022-12-11T07:11:10Z In this paper an algorithm for ice/water classification of C- A nd L-band dual polarization synthetic aperture radar data is presented. A comparison of the two different frequencies is made in order to investigate the potential to improve classification results with multi-frequency data. The algorithm is based on backscatter intensities in co- A nd cross-polarization and autocorrelation as a texture feature. The mapping between image features and ice/water classification is made with a neural network. Accurate ice/water maps for both frequencies are produced by the algorithm and the results of two frequencies generally agree very well. Differences are found in the marginal ice zone, where the time difference between acquisitions causes motion of the ice pack. C-band reliably reproduces the outline of the ice edge, while L-band has its strengths for thin ice/calm water areas within the icepack. The classification shows good agreement with ice/water maps derived from met.no ice-charts and radiometer data from AMSR-2. Variations are found in the marginal ice zone where the generalization of the ice charts and lower accuracy of ice concentration from radiometer data introduce deviations. Usage of high-resolution dual frequency data could be beneficial for improving ice cover information for navigation and modelling. Other/Unknown Material Fram Strait ice pack Sea ice Chalmers University of Technology: Chalmers research Annals of Glaciology 59 76pt2 112 123
institution Open Polar
collection Chalmers University of Technology: Chalmers research
op_collection_id ftchalmersuniv
language unknown
topic Remote Sensing
Geophysics
Geosciences
Multidisciplinary
polar and subpolar oceans
sea ice
ice and climate
spellingShingle Remote Sensing
Geophysics
Geosciences
Multidisciplinary
polar and subpolar oceans
sea ice
ice and climate
Aldenhoff, Wiebke
Heuzé, Céline
Eriksson, Leif
Comparison of ice/water classification in Fram Strait from C- A nd L-band SAR imagery
topic_facet Remote Sensing
Geophysics
Geosciences
Multidisciplinary
polar and subpolar oceans
sea ice
ice and climate
description In this paper an algorithm for ice/water classification of C- A nd L-band dual polarization synthetic aperture radar data is presented. A comparison of the two different frequencies is made in order to investigate the potential to improve classification results with multi-frequency data. The algorithm is based on backscatter intensities in co- A nd cross-polarization and autocorrelation as a texture feature. The mapping between image features and ice/water classification is made with a neural network. Accurate ice/water maps for both frequencies are produced by the algorithm and the results of two frequencies generally agree very well. Differences are found in the marginal ice zone, where the time difference between acquisitions causes motion of the ice pack. C-band reliably reproduces the outline of the ice edge, while L-band has its strengths for thin ice/calm water areas within the icepack. The classification shows good agreement with ice/water maps derived from met.no ice-charts and radiometer data from AMSR-2. Variations are found in the marginal ice zone where the generalization of the ice charts and lower accuracy of ice concentration from radiometer data introduce deviations. Usage of high-resolution dual frequency data could be beneficial for improving ice cover information for navigation and modelling.
author Aldenhoff, Wiebke
Heuzé, Céline
Eriksson, Leif
author_facet Aldenhoff, Wiebke
Heuzé, Céline
Eriksson, Leif
author_sort Aldenhoff, Wiebke
title Comparison of ice/water classification in Fram Strait from C- A nd L-band SAR imagery
title_short Comparison of ice/water classification in Fram Strait from C- A nd L-band SAR imagery
title_full Comparison of ice/water classification in Fram Strait from C- A nd L-band SAR imagery
title_fullStr Comparison of ice/water classification in Fram Strait from C- A nd L-band SAR imagery
title_full_unstemmed Comparison of ice/water classification in Fram Strait from C- A nd L-band SAR imagery
title_sort comparison of ice/water classification in fram strait from c- a nd l-band sar imagery
publishDate 2018
url https://doi.org/10.1017/aog.2018.7
https://research.chalmers.se/en/publication/0818bf50-cdeb-4fef-8bde-906c2022c2c7
genre Fram Strait
ice pack
Sea ice
genre_facet Fram Strait
ice pack
Sea ice
op_relation http://dx.doi.org/10.1017/aog.2018.7
https://research.chalmers.se/en/publication/0818bf50-cdeb-4fef-8bde-906c2022c2c7
op_doi https://doi.org/10.1017/aog.2018.7
container_title Annals of Glaciology
container_volume 59
container_issue 76pt2
container_start_page 112
op_container_end_page 123
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