Object-Based Detection of Linear Kinematic Features in Sea Ice

Inhomogenities in the sea ice motion field cause deformation zones, such as leads, cracks and pressure ridges. Due to their long and often narrow shape, those structures are referred to as Linear Kinematic Features (LKFs). In this paper we specifically address the identification and characterization...

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Published in:Remote Sensing
Main Authors: Stefanie Linow, Wolfgang Dierking
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2017
Subjects:
Online Access:https://doi.org/10.3390/rs9050493
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spelling ftmdpi:oai:mdpi.com:/2072-4292/9/5/493/ 2023-08-20T04:04:47+02:00 Object-Based Detection of Linear Kinematic Features in Sea Ice Stefanie Linow Wolfgang Dierking agris 2017-05-18 application/pdf https://doi.org/10.3390/rs9050493 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/rs9050493 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 9; Issue 5; Pages: 493 image processing computer vision object detection sea ice deformation linear kinematic features RGPS Arctic ocean Text 2017 ftmdpi https://doi.org/10.3390/rs9050493 2023-07-31T21:07:14Z Inhomogenities in the sea ice motion field cause deformation zones, such as leads, cracks and pressure ridges. Due to their long and often narrow shape, those structures are referred to as Linear Kinematic Features (LKFs). In this paper we specifically address the identification and characterization of variations and discontinuities in the spatial distribution of the total deformation, which appear as LKFs. The distribution of LKFs in the ice cover of the polar oceans is an important factor influencing the exchange of heat and matter at the ocean-atmosphere interface. Current analyses of the sea ice deformation field often ignore the spatial/geographical context of individual structures, e.g., their orientation relative to adjacent deformation zones. In this study, we adapt image processing techniques to develop a method for LKF detection which is able to resolve individual features. The data are vectorized to obtain results on an object-based level. We then apply a semantic postprocessing step to determine the angle of junctions and between crossing structures. The proposed object detection method is carefully validated. We found a localization uncertainty of 0.75 pixel and a length error of 12% in the identified LKFs. The detected features can be individually traced to their geographical position. Thus, a wide variety of new metrics for ice deformation can be easily derived, including spatial parameters as well as the temporal stability of individual features. Text Arctic Arctic Ocean Sea ice MDPI Open Access Publishing Arctic Arctic Ocean Remote Sensing 9 5 493
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic image processing
computer vision
object detection
sea ice deformation
linear kinematic features
RGPS
Arctic ocean
spellingShingle image processing
computer vision
object detection
sea ice deformation
linear kinematic features
RGPS
Arctic ocean
Stefanie Linow
Wolfgang Dierking
Object-Based Detection of Linear Kinematic Features in Sea Ice
topic_facet image processing
computer vision
object detection
sea ice deformation
linear kinematic features
RGPS
Arctic ocean
description Inhomogenities in the sea ice motion field cause deformation zones, such as leads, cracks and pressure ridges. Due to their long and often narrow shape, those structures are referred to as Linear Kinematic Features (LKFs). In this paper we specifically address the identification and characterization of variations and discontinuities in the spatial distribution of the total deformation, which appear as LKFs. The distribution of LKFs in the ice cover of the polar oceans is an important factor influencing the exchange of heat and matter at the ocean-atmosphere interface. Current analyses of the sea ice deformation field often ignore the spatial/geographical context of individual structures, e.g., their orientation relative to adjacent deformation zones. In this study, we adapt image processing techniques to develop a method for LKF detection which is able to resolve individual features. The data are vectorized to obtain results on an object-based level. We then apply a semantic postprocessing step to determine the angle of junctions and between crossing structures. The proposed object detection method is carefully validated. We found a localization uncertainty of 0.75 pixel and a length error of 12% in the identified LKFs. The detected features can be individually traced to their geographical position. Thus, a wide variety of new metrics for ice deformation can be easily derived, including spatial parameters as well as the temporal stability of individual features.
format Text
author Stefanie Linow
Wolfgang Dierking
author_facet Stefanie Linow
Wolfgang Dierking
author_sort Stefanie Linow
title Object-Based Detection of Linear Kinematic Features in Sea Ice
title_short Object-Based Detection of Linear Kinematic Features in Sea Ice
title_full Object-Based Detection of Linear Kinematic Features in Sea Ice
title_fullStr Object-Based Detection of Linear Kinematic Features in Sea Ice
title_full_unstemmed Object-Based Detection of Linear Kinematic Features in Sea Ice
title_sort object-based detection of linear kinematic features in sea ice
publisher Multidisciplinary Digital Publishing Institute
publishDate 2017
url https://doi.org/10.3390/rs9050493
op_coverage agris
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Sea ice
genre_facet Arctic
Arctic Ocean
Sea ice
op_source Remote Sensing; Volume 9; Issue 5; Pages: 493
op_relation https://dx.doi.org/10.3390/rs9050493
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs9050493
container_title Remote Sensing
container_volume 9
container_issue 5
container_start_page 493
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