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...

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Published in:Arctic Science
Main Authors: Alicia L.A. Dauginis, Laura C. Brown
Format: Article in Journal/Newspaper
Language:English
French
Published: Canadian Science Publishing 2021
Subjects:
ims
Online Access:https://doi.org/10.1139/as-2020-0024
https://doaj.org/article/823b511a0d4148258a1daa8f897a3d50
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spelling ftdoajarticles:oai:doaj.org/article:823b511a0d4148258a1daa8f897a3d50 2023-05-15T14:23:37+02:00 Sea ice and snow phenology in the Canadian Arctic Archipelago from 1997 to 2018 Alicia L.A. Dauginis Laura C. Brown 2021-03-01T00:00:00Z https://doi.org/10.1139/as-2020-0024 https://doaj.org/article/823b511a0d4148258a1daa8f897a3d50 EN FR eng fre Canadian Science Publishing https://doi.org/10.1139/as-2020-0024 https://doaj.org/toc/2368-7460 doi:10.1139/as-2020-0024 2368-7460 https://doaj.org/article/823b511a0d4148258a1daa8f897a3d50 Arctic Science, Vol 7, Iss 1, Pp 182-207 (2021) cryosphere sea ice snow cover ims canadian arctic archipelago Environmental sciences GE1-350 Environmental engineering TA170-171 article 2021 ftdoajarticles https://doi.org/10.1139/as-2020-0024 2022-12-31T15:29:59Z 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 Directory of Open Access Journals: DOAJ Articles Arctic Canadian Arctic Archipelago Arctic Science 7 1 182 207
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
French
topic cryosphere
sea ice
snow cover
ims
canadian arctic archipelago
Environmental sciences
GE1-350
Environmental engineering
TA170-171
spellingShingle cryosphere
sea ice
snow cover
ims
canadian arctic archipelago
Environmental sciences
GE1-350
Environmental engineering
TA170-171
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
Environmental sciences
GE1-350
Environmental engineering
TA170-171
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 https://doi.org/10.1139/as-2020-0024
https://doaj.org/toc/2368-7460
doi:10.1139/as-2020-0024
2368-7460
https://doaj.org/article/823b511a0d4148258a1daa8f897a3d50
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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