Evolution of the dynamics of Airdrop Glacier, western Axel Heiberg Island, over a seven-decade-long advance
Various remotely sensed data, including historical aerial photographs, declassified intelligence satellite photographs, optical satellite imagery, and synthetic aperture radar data, were used to undertake the first comprehensive reconstruction of the dynamics of Airdrop Glacier on Axel Heiberg Islan...
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Canadian Science Publishing
2023
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Online Access: | http://dx.doi.org/10.1139/as-2022-0045 https://cdnsciencepub.com/doi/full-xml/10.1139/as-2022-0045 https://cdnsciencepub.com/doi/pdf/10.1139/as-2022-0045 |
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crcansciencepubl:10.1139/as-2022-0045 2023-12-17T10:22:41+01:00 Evolution of the dynamics of Airdrop Glacier, western Axel Heiberg Island, over a seven-decade-long advance Lauzon, Benoît Copland, Luke Van Wychen, Wesley Kochtitzky, William McNabb, Robert Natural Sciences and Engineering Research Council of Canada ArcticNet University of Ottawa University of Manitoba 2023 http://dx.doi.org/10.1139/as-2022-0045 https://cdnsciencepub.com/doi/full-xml/10.1139/as-2022-0045 https://cdnsciencepub.com/doi/pdf/10.1139/as-2022-0045 en eng Canadian Science Publishing https://creativecommons.org/licenses/by/4.0/deed.en_GB Arctic Science ISSN 2368-7460 General Earth and Planetary Sciences General Agricultural and Biological Sciences General Environmental Science journal-article 2023 crcansciencepubl https://doi.org/10.1139/as-2022-0045 2023-11-19T13:39:03Z Various remotely sensed data, including historical aerial photographs, declassified intelligence satellite photographs, optical satellite imagery, and synthetic aperture radar data, were used to undertake the first comprehensive reconstruction of the dynamics of Airdrop Glacier on Axel Heiberg Island, Nunavut. Observations show a continuous terminus advance totalling ∼6 km since 1950 and notably less variability in its surface velocities in comparison to adjacent Iceberg Glacier. This advance is concurrent with relatively high flow rates over its entire surface, resulting in significant thickening near the terminus and thinning at higher elevations. Velocities have more than halved from the mid-2000s to 2021, but without any definitive evidence of previous flow instabilities, we cannot confirm whether Airdrop's behaviour is cyclic in nature and therefore characteristic of a surge. Instead, Airdrop Glacier could be experiencing a delayed response to the positive mass balance conditions of the Little Ice Age, which could also explain the advance of other nearby glaciers. Its recent slowdown could then be indicative of a gradual adjustment to recent climatic conditions. This study highlights the need for comprehensive studies of glacier dynamics in the Canadian Arctic to improve our understanding of the factors triggering dynamic instabilities and causing the observed variety of behaviours. Article in Journal/Newspaper Arctic Arctic Axel Heiberg Island Iceberg* Nunavut Canadian Science Publishing (via Crossref) Arctic Nunavut Heiberg ENVELOPE(13.964,13.964,66.424,66.424) Axel Heiberg Island ENVELOPE(-91.001,-91.001,79.752,79.752) Iceberg Glacier ENVELOPE(-92.134,-92.134,79.517,79.517) Arctic Science |
institution |
Open Polar |
collection |
Canadian Science Publishing (via Crossref) |
op_collection_id |
crcansciencepubl |
language |
English |
topic |
General Earth and Planetary Sciences General Agricultural and Biological Sciences General Environmental Science |
spellingShingle |
General Earth and Planetary Sciences General Agricultural and Biological Sciences General Environmental Science Lauzon, Benoît Copland, Luke Van Wychen, Wesley Kochtitzky, William McNabb, Robert Evolution of the dynamics of Airdrop Glacier, western Axel Heiberg Island, over a seven-decade-long advance |
topic_facet |
General Earth and Planetary Sciences General Agricultural and Biological Sciences General Environmental Science |
description |
Various remotely sensed data, including historical aerial photographs, declassified intelligence satellite photographs, optical satellite imagery, and synthetic aperture radar data, were used to undertake the first comprehensive reconstruction of the dynamics of Airdrop Glacier on Axel Heiberg Island, Nunavut. Observations show a continuous terminus advance totalling ∼6 km since 1950 and notably less variability in its surface velocities in comparison to adjacent Iceberg Glacier. This advance is concurrent with relatively high flow rates over its entire surface, resulting in significant thickening near the terminus and thinning at higher elevations. Velocities have more than halved from the mid-2000s to 2021, but without any definitive evidence of previous flow instabilities, we cannot confirm whether Airdrop's behaviour is cyclic in nature and therefore characteristic of a surge. Instead, Airdrop Glacier could be experiencing a delayed response to the positive mass balance conditions of the Little Ice Age, which could also explain the advance of other nearby glaciers. Its recent slowdown could then be indicative of a gradual adjustment to recent climatic conditions. This study highlights the need for comprehensive studies of glacier dynamics in the Canadian Arctic to improve our understanding of the factors triggering dynamic instabilities and causing the observed variety of behaviours. |
author2 |
Natural Sciences and Engineering Research Council of Canada ArcticNet University of Ottawa University of Manitoba |
format |
Article in Journal/Newspaper |
author |
Lauzon, Benoît Copland, Luke Van Wychen, Wesley Kochtitzky, William McNabb, Robert |
author_facet |
Lauzon, Benoît Copland, Luke Van Wychen, Wesley Kochtitzky, William McNabb, Robert |
author_sort |
Lauzon, Benoît |
title |
Evolution of the dynamics of Airdrop Glacier, western Axel Heiberg Island, over a seven-decade-long advance |
title_short |
Evolution of the dynamics of Airdrop Glacier, western Axel Heiberg Island, over a seven-decade-long advance |
title_full |
Evolution of the dynamics of Airdrop Glacier, western Axel Heiberg Island, over a seven-decade-long advance |
title_fullStr |
Evolution of the dynamics of Airdrop Glacier, western Axel Heiberg Island, over a seven-decade-long advance |
title_full_unstemmed |
Evolution of the dynamics of Airdrop Glacier, western Axel Heiberg Island, over a seven-decade-long advance |
title_sort |
evolution of the dynamics of airdrop glacier, western axel heiberg island, over a seven-decade-long advance |
publisher |
Canadian Science Publishing |
publishDate |
2023 |
url |
http://dx.doi.org/10.1139/as-2022-0045 https://cdnsciencepub.com/doi/full-xml/10.1139/as-2022-0045 https://cdnsciencepub.com/doi/pdf/10.1139/as-2022-0045 |
long_lat |
ENVELOPE(13.964,13.964,66.424,66.424) ENVELOPE(-91.001,-91.001,79.752,79.752) ENVELOPE(-92.134,-92.134,79.517,79.517) |
geographic |
Arctic Nunavut Heiberg Axel Heiberg Island Iceberg Glacier |
geographic_facet |
Arctic Nunavut Heiberg Axel Heiberg Island Iceberg Glacier |
genre |
Arctic Arctic Axel Heiberg Island Iceberg* Nunavut |
genre_facet |
Arctic Arctic Axel Heiberg Island Iceberg* Nunavut |
op_source |
Arctic Science ISSN 2368-7460 |
op_rights |
https://creativecommons.org/licenses/by/4.0/deed.en_GB |
op_doi |
https://doi.org/10.1139/as-2022-0045 |
container_title |
Arctic Science |
_version_ |
1785551380091502592 |