Sea Ice and Migration of the Dolphin and Union Caribou Herd in the Canadian Arctic: An Uncertain Future

Caribou (Rangifer tarandus groenlandicus × pearyi) of the Dolphin and Union herd migrate across the sea ice between Victoria Island and the adjacent Canadian Arctic mainland twice each year, southward in fall–early winter and northward in late winter–spring. As a result of warmer temperatures, sea i...

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Published in:ARCTIC
Main Authors: Poole, Kim G., Gunn, Anne, Patterson, Brent R., Dumond, Mathieu
Format: Article in Journal/Newspaper
Language:English
Published: The Arctic Institute of North America 2010
Subjects:
Online Access:https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66382
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author Poole, Kim G.
Gunn, Anne
Patterson, Brent R.
Dumond, Mathieu
author_facet Poole, Kim G.
Gunn, Anne
Patterson, Brent R.
Dumond, Mathieu
author_sort Poole, Kim G.
collection Unknown
container_issue 4
container_title ARCTIC
container_volume 63
description Caribou (Rangifer tarandus groenlandicus × pearyi) of the Dolphin and Union herd migrate across the sea ice between Victoria Island and the adjacent Canadian Arctic mainland twice each year, southward in fall–early winter and northward in late winter–spring. As a result of warmer temperatures, sea ice between Victoria Island and the mainland now forms 8–10 days later than it did in 1982, raising questions about the impact of delayed ice formation on the ecology of the herd. We examined movements of female Dolphin and Union caribou as they relate to sea-ice crossings using four satellite collar datasets (46 caribou) obtained between 1987 and 2006. Since the late 1980s, Dolphin and Union caribou have been moving by early October to the southern coast of Victoria Island, where they stage until sea-ice formation allows migration across the sea ice to winter range on the mainland. Caribou spending the summer farther north on Victoria Island arrive later at the coast, which shortens their time spent on the staging area. During the study period, the collared caribou began crossings as soon as sea-ice formation allowed. Most caribou departed from just a few areas and tended to use the same departure areas each year. Highest mortality occurred during the fall–early winter ice crossing and in mid to late winter. Our research raises the question of how the Dolphin and Union caribou will persist in supporting harvesting if the crossing becomes riskier for them or if the seasonal migrations between Victoria Island and the mainland are interrupted. Les caribous (Rangifer tarandus groenlandicus × pearyi) du troupeau Dolphin-et-Union migrent en passant sur la glace de mer entre l’île Victoria et la partie continentale adjacente de l’Arctique canadien deux fois par année, se dirigeant vers le sud à l’automne et au début de l’hiver, et vers le nord à la fin de l’hiver et au printemps. En raison des températures plus chaudes, la glace de mer entre l’île Victoria et la partie continentale se forme maintenant de huit à dix jours ...
format Article in Journal/Newspaper
genre Arctic
Arctic
Nunavut
Rangifer tarandus
Sea ice
Victoria Island
victoria island
genre_facet Arctic
Arctic
Nunavut
Rangifer tarandus
Sea ice
Victoria Island
victoria island
geographic Arctic
Canada
Collier
Nunavut
geographic_facet Arctic
Canada
Collier
Nunavut
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op_source ARCTIC; Vol. 63 No. 4 (2010): December: 381–504; 414-428
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spelling ftunivcalgaryojs:oai:journalhosting.ucalgary.ca:article/66382 2025-06-15T14:14:24+00:00 Sea Ice and Migration of the Dolphin and Union Caribou Herd in the Canadian Arctic: An Uncertain Future Poole, Kim G. Gunn, Anne Patterson, Brent R. Dumond, Mathieu 2010-12-03 application/pdf https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66382 eng eng The Arctic Institute of North America https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66382/50295 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66382 ARCTIC; Vol. 63 No. 4 (2010): December: 381–504; 414-428 1923-1245 0004-0843 caribou Rangifer Dolphin and Union herd migration sea ice climate satellite collar Canada Nunavut troupeau de Dolphin-et-Union glace de mer climat collier-satellite info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 2010 ftunivcalgaryojs 2025-05-27T03:29:43Z Caribou (Rangifer tarandus groenlandicus × pearyi) of the Dolphin and Union herd migrate across the sea ice between Victoria Island and the adjacent Canadian Arctic mainland twice each year, southward in fall–early winter and northward in late winter–spring. As a result of warmer temperatures, sea ice between Victoria Island and the mainland now forms 8–10 days later than it did in 1982, raising questions about the impact of delayed ice formation on the ecology of the herd. We examined movements of female Dolphin and Union caribou as they relate to sea-ice crossings using four satellite collar datasets (46 caribou) obtained between 1987 and 2006. Since the late 1980s, Dolphin and Union caribou have been moving by early October to the southern coast of Victoria Island, where they stage until sea-ice formation allows migration across the sea ice to winter range on the mainland. Caribou spending the summer farther north on Victoria Island arrive later at the coast, which shortens their time spent on the staging area. During the study period, the collared caribou began crossings as soon as sea-ice formation allowed. Most caribou departed from just a few areas and tended to use the same departure areas each year. Highest mortality occurred during the fall–early winter ice crossing and in mid to late winter. Our research raises the question of how the Dolphin and Union caribou will persist in supporting harvesting if the crossing becomes riskier for them or if the seasonal migrations between Victoria Island and the mainland are interrupted. Les caribous (Rangifer tarandus groenlandicus × pearyi) du troupeau Dolphin-et-Union migrent en passant sur la glace de mer entre l’île Victoria et la partie continentale adjacente de l’Arctique canadien deux fois par année, se dirigeant vers le sud à l’automne et au début de l’hiver, et vers le nord à la fin de l’hiver et au printemps. En raison des températures plus chaudes, la glace de mer entre l’île Victoria et la partie continentale se forme maintenant de huit à dix jours ... Article in Journal/Newspaper Arctic Arctic Nunavut Rangifer tarandus Sea ice Victoria Island victoria island Unknown Arctic Canada Collier ENVELOPE(-61.864,-61.864,-70.221,-70.221) Nunavut ARCTIC 63 4
spellingShingle caribou
Rangifer
Dolphin and Union herd
migration
sea ice
climate
satellite collar
Canada
Nunavut
troupeau de Dolphin-et-Union
glace de mer
climat
collier-satellite
Poole, Kim G.
Gunn, Anne
Patterson, Brent R.
Dumond, Mathieu
Sea Ice and Migration of the Dolphin and Union Caribou Herd in the Canadian Arctic: An Uncertain Future
title Sea Ice and Migration of the Dolphin and Union Caribou Herd in the Canadian Arctic: An Uncertain Future
title_full Sea Ice and Migration of the Dolphin and Union Caribou Herd in the Canadian Arctic: An Uncertain Future
title_fullStr Sea Ice and Migration of the Dolphin and Union Caribou Herd in the Canadian Arctic: An Uncertain Future
title_full_unstemmed Sea Ice and Migration of the Dolphin and Union Caribou Herd in the Canadian Arctic: An Uncertain Future
title_short Sea Ice and Migration of the Dolphin and Union Caribou Herd in the Canadian Arctic: An Uncertain Future
title_sort sea ice and migration of the dolphin and union caribou herd in the canadian arctic: an uncertain future
topic caribou
Rangifer
Dolphin and Union herd
migration
sea ice
climate
satellite collar
Canada
Nunavut
troupeau de Dolphin-et-Union
glace de mer
climat
collier-satellite
topic_facet caribou
Rangifer
Dolphin and Union herd
migration
sea ice
climate
satellite collar
Canada
Nunavut
troupeau de Dolphin-et-Union
glace de mer
climat
collier-satellite
url https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66382