Sea ice and snow phenology in the Canadian Arctic Archipelago from 1997 to 2018
The multiple islands and narrow channels that form the Canadian Arctic Archipelago (CAA) complicate snow/ice monitoring, as coarse resolution satellite observations are unable to resolve smaller-scale changes in snow/ice cover. We present the first study showing the utility of the Interactive Multis...
Published in: | Arctic Science |
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Format: | Article in Journal/Newspaper |
Language: | English French |
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Canadian Science Publishing
2021
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Online Access: | https://doi.org/10.1139/as-2020-0024 https://doaj.org/article/823b511a0d4148258a1daa8f897a3d50 |
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fttriple:oai:gotriple.eu:oai:doaj.org/article:823b511a0d4148258a1daa8f897a3d50 2023-05-15T14:22:25+02:00 Sea ice and snow phenology in the Canadian Arctic Archipelago from 1997 to 2018 Alicia L.A. Dauginis Laura C. Brown 2021-03-01 https://doi.org/10.1139/as-2020-0024 https://doaj.org/article/823b511a0d4148258a1daa8f897a3d50 en fr eng fre Canadian Science Publishing doi:10.1139/as-2020-0024 2368-7460 https://doaj.org/article/823b511a0d4148258a1daa8f897a3d50 undefined Arctic Science, Vol 7, Iss 1, Pp 182-207 (2021) cryosphere sea ice snow cover ims canadian arctic archipelago geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2021 fttriple https://doi.org/10.1139/as-2020-0024 2023-01-22T18:11:31Z The multiple islands and narrow channels that form the Canadian Arctic Archipelago (CAA) complicate snow/ice monitoring, as coarse resolution satellite observations are unable to resolve smaller-scale changes in snow/ice cover. We present the first study showing the utility of the Interactive Multisensor Snow and Ice Mapping System (IMS) 24 km (1997–2018) and 4 km (2004–2018) products to investigate changes in sea ice and snow phenology together in the CAA. Although ice break-up and snow retreat are shifting earlier (p > 0.05), on par with other Arctic regions, the final summer clearing of ice is shifting later. This, combined with trends towards earlier ice freeze and snow fall (p < 0.05), result in shorter open water and snow free seasons in the CAA. Spatial links between sea ice and snow are evident as significant clusters of trends were identified for all phenology parameters. The western regions were dominated by shifts towards shorter snow/ice seasons, whereas eastern regions tended to exhibit longer cover. Our research highlights the considerable regional and interannual variability in the timing of sea ice and snow advance/retreat within the CAA and emphasizes how the ice and snow dynamics in this complex region are responding to ongoing changing climate conditions. Article in Journal/Newspaper Arctic Arctic Archipelago Arctic Canadian Arctic Archipelago Sea ice Unknown Arctic Canadian Arctic Archipelago Arctic Science 7 1 182 207 |
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Open Polar |
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language |
English French |
topic |
cryosphere sea ice snow cover ims canadian arctic archipelago geo envir |
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cryosphere sea ice snow cover ims canadian arctic archipelago geo envir Alicia L.A. Dauginis Laura C. Brown Sea ice and snow phenology in the Canadian Arctic Archipelago from 1997 to 2018 |
topic_facet |
cryosphere sea ice snow cover ims canadian arctic archipelago geo envir |
description |
The multiple islands and narrow channels that form the Canadian Arctic Archipelago (CAA) complicate snow/ice monitoring, as coarse resolution satellite observations are unable to resolve smaller-scale changes in snow/ice cover. We present the first study showing the utility of the Interactive Multisensor Snow and Ice Mapping System (IMS) 24 km (1997–2018) and 4 km (2004–2018) products to investigate changes in sea ice and snow phenology together in the CAA. Although ice break-up and snow retreat are shifting earlier (p > 0.05), on par with other Arctic regions, the final summer clearing of ice is shifting later. This, combined with trends towards earlier ice freeze and snow fall (p < 0.05), result in shorter open water and snow free seasons in the CAA. Spatial links between sea ice and snow are evident as significant clusters of trends were identified for all phenology parameters. The western regions were dominated by shifts towards shorter snow/ice seasons, whereas eastern regions tended to exhibit longer cover. Our research highlights the considerable regional and interannual variability in the timing of sea ice and snow advance/retreat within the CAA and emphasizes how the ice and snow dynamics in this complex region are responding to ongoing changing climate conditions. |
format |
Article in Journal/Newspaper |
author |
Alicia L.A. Dauginis Laura C. Brown |
author_facet |
Alicia L.A. Dauginis Laura C. Brown |
author_sort |
Alicia L.A. Dauginis |
title |
Sea ice and snow phenology in the Canadian Arctic Archipelago from 1997 to 2018 |
title_short |
Sea ice and snow phenology in the Canadian Arctic Archipelago from 1997 to 2018 |
title_full |
Sea ice and snow phenology in the Canadian Arctic Archipelago from 1997 to 2018 |
title_fullStr |
Sea ice and snow phenology in the Canadian Arctic Archipelago from 1997 to 2018 |
title_full_unstemmed |
Sea ice and snow phenology in the Canadian Arctic Archipelago from 1997 to 2018 |
title_sort |
sea ice and snow phenology in the canadian arctic archipelago from 1997 to 2018 |
publisher |
Canadian Science Publishing |
publishDate |
2021 |
url |
https://doi.org/10.1139/as-2020-0024 https://doaj.org/article/823b511a0d4148258a1daa8f897a3d50 |
geographic |
Arctic Canadian Arctic Archipelago |
geographic_facet |
Arctic Canadian Arctic Archipelago |
genre |
Arctic Arctic Archipelago Arctic Canadian Arctic Archipelago Sea ice |
genre_facet |
Arctic Arctic Archipelago Arctic Canadian Arctic Archipelago Sea ice |
op_source |
Arctic Science, Vol 7, Iss 1, Pp 182-207 (2021) |
op_relation |
doi:10.1139/as-2020-0024 2368-7460 https://doaj.org/article/823b511a0d4148258a1daa8f897a3d50 |
op_rights |
undefined |
op_doi |
https://doi.org/10.1139/as-2020-0024 |
container_title |
Arctic Science |
container_volume |
7 |
container_issue |
1 |
container_start_page |
182 |
op_container_end_page |
207 |
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1766295003732115456 |