Ice ridge density signatures in high-resolution SAR images

The statistics of ice-ridging signatures were studied using high-resolution (1.25 m) and medium-resolution (20 m) SAR images over the Baltic Sea ice cover, acquired in 2016 and 2011, respectively. Ice surface profiles measured by the 2011 airborne campaign were used as validation data. The images di...

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Published in:The Cryosphere
Main Authors: Lensu, Mikko, Similä, Markku
Format: Text
Language:English
Published: 2022
Subjects:
Online Access:https://doi.org/10.5194/tc-16-4363-2022
https://tc.copernicus.org/articles/16/4363/2022/
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spelling ftcopernicus:oai:publications.copernicus.org:tc98931 2023-05-15T18:18:35+02:00 Ice ridge density signatures in high-resolution SAR images Lensu, Mikko Similä, Markku 2022-10-18 application/pdf https://doi.org/10.5194/tc-16-4363-2022 https://tc.copernicus.org/articles/16/4363/2022/ eng eng doi:10.5194/tc-16-4363-2022 https://tc.copernicus.org/articles/16/4363/2022/ eISSN: 1994-0424 Text 2022 ftcopernicus https://doi.org/10.5194/tc-16-4363-2022 2022-10-24T16:22:42Z The statistics of ice-ridging signatures were studied using high-resolution (1.25 m) and medium-resolution (20 m) SAR images over the Baltic Sea ice cover, acquired in 2016 and 2011, respectively. Ice surface profiles measured by the 2011 airborne campaign were used as validation data. The images did not delineate well the individual ridges as linear features. This was assigned to the random occurrence of ridge rubble arrangements that generate bright SAR returns. Instead, the ridging signatures were approached in terms of the local density of bright returns selected by a variably bright-pixel percentage (BPP). Density was quantified by counting bright-pixel numbers (BPNs) in pixel blocks with variable side length L . A statistical model for BPN distributions was determined by considering how the BPN values change with the BPP and was found to apply over a wide range of values for BPP and L . The statistical approach was also able to simulate a higher-BPP image when seeded by a low-BPP image. It was also found to apply to surface profile data analysed by counting ridge sail numbers in profile segments of variable length L . This provided a statistical connection between the bright-pixel density and the ridge density. The connection was studied for the 2011 data in terms of surface rubble coverage estimated both from the medium-resolution image and from the surface profiles. Apart from a scaling factor, both were found to follow the same distribution. Text Sea ice Copernicus Publications: E-Journals The Cryosphere 16 10 4363 4377
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The statistics of ice-ridging signatures were studied using high-resolution (1.25 m) and medium-resolution (20 m) SAR images over the Baltic Sea ice cover, acquired in 2016 and 2011, respectively. Ice surface profiles measured by the 2011 airborne campaign were used as validation data. The images did not delineate well the individual ridges as linear features. This was assigned to the random occurrence of ridge rubble arrangements that generate bright SAR returns. Instead, the ridging signatures were approached in terms of the local density of bright returns selected by a variably bright-pixel percentage (BPP). Density was quantified by counting bright-pixel numbers (BPNs) in pixel blocks with variable side length L . A statistical model for BPN distributions was determined by considering how the BPN values change with the BPP and was found to apply over a wide range of values for BPP and L . The statistical approach was also able to simulate a higher-BPP image when seeded by a low-BPP image. It was also found to apply to surface profile data analysed by counting ridge sail numbers in profile segments of variable length L . This provided a statistical connection between the bright-pixel density and the ridge density. The connection was studied for the 2011 data in terms of surface rubble coverage estimated both from the medium-resolution image and from the surface profiles. Apart from a scaling factor, both were found to follow the same distribution.
format Text
author Lensu, Mikko
Similä, Markku
spellingShingle Lensu, Mikko
Similä, Markku
Ice ridge density signatures in high-resolution SAR images
author_facet Lensu, Mikko
Similä, Markku
author_sort Lensu, Mikko
title Ice ridge density signatures in high-resolution SAR images
title_short Ice ridge density signatures in high-resolution SAR images
title_full Ice ridge density signatures in high-resolution SAR images
title_fullStr Ice ridge density signatures in high-resolution SAR images
title_full_unstemmed Ice ridge density signatures in high-resolution SAR images
title_sort ice ridge density signatures in high-resolution sar images
publishDate 2022
url https://doi.org/10.5194/tc-16-4363-2022
https://tc.copernicus.org/articles/16/4363/2022/
genre Sea ice
genre_facet Sea ice
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-16-4363-2022
https://tc.copernicus.org/articles/16/4363/2022/
op_doi https://doi.org/10.5194/tc-16-4363-2022
container_title The Cryosphere
container_volume 16
container_issue 10
container_start_page 4363
op_container_end_page 4377
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