Impact of Arctic sea ice floe-scale anisotropy on airborne electromagnetic surveys

Abstract Airborne electromagnetic induction sensors have demonstrated their extensive capacities to measure sea-ice thickness distributions. However, biases can emerge when comparing these 1-D measurements to a broader 2-D regional scale due to the spatial anisotropy inherent to sea-ice cover. Autom...

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Published in:Annals of Glaciology
Main Authors: Negrel, Jean, Divine, Dmitry V., Gerland, Sebastian
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2020
Subjects:
Online Access:http://dx.doi.org/10.1017/aog.2020.61
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0260305520000610
id crcambridgeupr:10.1017/aog.2020.61
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spelling crcambridgeupr:10.1017/aog.2020.61 2024-06-09T07:38:28+00:00 Impact of Arctic sea ice floe-scale anisotropy on airborne electromagnetic surveys Negrel, Jean Divine, Dmitry V. Gerland, Sebastian 2020 http://dx.doi.org/10.1017/aog.2020.61 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0260305520000610 en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by/4.0/ Annals of Glaciology volume 61, issue 83, page 379-391 ISSN 0260-3055 1727-5644 journal-article 2020 crcambridgeupr https://doi.org/10.1017/aog.2020.61 2024-05-15T13:02:27Z Abstract Airborne electromagnetic induction sensors have demonstrated their extensive capacities to measure sea-ice thickness distributions. However, biases can emerge when comparing these 1-D measurements to a broader 2-D regional scale due to the spatial anisotropy inherent to sea-ice cover. Automated processing of available sea-ice maps could significantly ease the decision on how to set up an optimised flight pattern, which would result in representative ice thickness numbers for the region. In this study, first we investigate the extent to which the sea-ice anisotropy can influence the representativeness of an airborne survey compared to the regional situation. Second, we propose a method to process sea-ice maps prior to flights to help preparing the most representative flight plan possible for the local area. The method is based on automated segmentation of radar satellite images and extensive simulation of flight transects over the image. The spatial analysis of these transects enables for the identification of the most representative survey trajectories for the area. The method was applied for seven different synthetic aperture radar satellite images over Arctic sea ice north of Svalbard. The results indicate that the proposed method improved the representativeness of the airborne survey by identifying the most suitable transect over the ice pack. Article in Journal/Newspaper Annals of Glaciology Arctic ice pack Sea ice Svalbard Cambridge University Press Arctic Svalbard Annals of Glaciology 61 83 379 391
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract Airborne electromagnetic induction sensors have demonstrated their extensive capacities to measure sea-ice thickness distributions. However, biases can emerge when comparing these 1-D measurements to a broader 2-D regional scale due to the spatial anisotropy inherent to sea-ice cover. Automated processing of available sea-ice maps could significantly ease the decision on how to set up an optimised flight pattern, which would result in representative ice thickness numbers for the region. In this study, first we investigate the extent to which the sea-ice anisotropy can influence the representativeness of an airborne survey compared to the regional situation. Second, we propose a method to process sea-ice maps prior to flights to help preparing the most representative flight plan possible for the local area. The method is based on automated segmentation of radar satellite images and extensive simulation of flight transects over the image. The spatial analysis of these transects enables for the identification of the most representative survey trajectories for the area. The method was applied for seven different synthetic aperture radar satellite images over Arctic sea ice north of Svalbard. The results indicate that the proposed method improved the representativeness of the airborne survey by identifying the most suitable transect over the ice pack.
format Article in Journal/Newspaper
author Negrel, Jean
Divine, Dmitry V.
Gerland, Sebastian
spellingShingle Negrel, Jean
Divine, Dmitry V.
Gerland, Sebastian
Impact of Arctic sea ice floe-scale anisotropy on airborne electromagnetic surveys
author_facet Negrel, Jean
Divine, Dmitry V.
Gerland, Sebastian
author_sort Negrel, Jean
title Impact of Arctic sea ice floe-scale anisotropy on airborne electromagnetic surveys
title_short Impact of Arctic sea ice floe-scale anisotropy on airborne electromagnetic surveys
title_full Impact of Arctic sea ice floe-scale anisotropy on airborne electromagnetic surveys
title_fullStr Impact of Arctic sea ice floe-scale anisotropy on airborne electromagnetic surveys
title_full_unstemmed Impact of Arctic sea ice floe-scale anisotropy on airborne electromagnetic surveys
title_sort impact of arctic sea ice floe-scale anisotropy on airborne electromagnetic surveys
publisher Cambridge University Press (CUP)
publishDate 2020
url http://dx.doi.org/10.1017/aog.2020.61
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0260305520000610
geographic Arctic
Svalbard
geographic_facet Arctic
Svalbard
genre Annals of Glaciology
Arctic
ice pack
Sea ice
Svalbard
genre_facet Annals of Glaciology
Arctic
ice pack
Sea ice
Svalbard
op_source Annals of Glaciology
volume 61, issue 83, page 379-391
ISSN 0260-3055 1727-5644
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1017/aog.2020.61
container_title Annals of Glaciology
container_volume 61
container_issue 83
container_start_page 379
op_container_end_page 391
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