Distribution, Movement and Abundance of Polar Bears in Lancaster Sound, Northwest Territories
Mark-recapture studies show that polar bears are distributed at varying densities throughout Lancaster Sound during winter and spring. Major concentrations occur along the north and south coasts and the transverse floe edge at the mouth of the sound. As the ice melts, some bears move west whereas ot...
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1982
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ftunivcalgaryojs:oai:journalhosting.ucalgary.ca:article/65368 2023-05-15T14:19:16+02:00 Distribution, Movement and Abundance of Polar Bears in Lancaster Sound, Northwest Territories Schweinsburg, R.E. Lee, L.J. Latour, P.B. 1982-01-01 application/pdf https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65368 eng eng The Arctic Institute of North America https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65368/49282 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65368 ARCTIC; Vol. 35 No. 1 (1982): March: 1–240; 159-169 1923-1245 0004-0843 Animal distribution Animal migration Animal population Denning Polar bears Winter ecology Wildlife habitat Lancaster Sound Nunavut info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 1982 ftunivcalgaryojs 2022-03-22T21:22:25Z Mark-recapture studies show that polar bears are distributed at varying densities throughout Lancaster Sound during winter and spring. Major concentrations occur along the north and south coasts and the transverse floe edge at the mouth of the sound. As the ice melts, some bears move west whereas others move to nearby land areas. There is some evidence that as the ice forms, polar bears return from their summer locations to eastern Lancaster Sound. Polar bears of Lancaster Sound are part of the larger population whose western range extends to Barrow Strait, Prince Regent Inlet, Wellington Channel and Jones Sound. The southern and eastern range limits are unknown although this population may extend at least to Clyde River on northeastern Baffin Island and probably to Greenland. Maternity denning appears to be widespread over the study area probably because of the abundance of suitable habitat. We estimated a population of 1031 ± 236 polar bears in Lancaster Sound during 1979: however, more estimates are needed to determine if this relatively high number is normal for the area.Key words: polar bear, distribution, movement, abundance, Baffin Bay, Lancaster Sound, summer retreat, denning Article in Journal/Newspaper Arctic Baffin Bay Baffin Bay Baffin Island Baffin Clyde River Greenland Jones Sound Lancaster Sound Northwest Territories Nunavut polar bear Prince Regent Inlet University of Calgary Journal Hosting Baffin Bay Baffin Island Barrow Strait ENVELOPE(-94.168,-94.168,74.402,74.402) Clyde River ENVELOPE(-70.451,-70.451,69.854,69.854) Greenland Jones Sound ENVELOPE(-86.000,-86.000,76.002,76.002) Lancaster Sound ENVELOPE(-83.999,-83.999,74.218,74.218) Northwest Territories Nunavut Prince Regent Inlet ENVELOPE(-90.431,-90.431,72.993,72.993) Wellington Channel ENVELOPE(-93.201,-93.201,75.468,75.468) ARCTIC 35 1 |
institution |
Open Polar |
collection |
University of Calgary Journal Hosting |
op_collection_id |
ftunivcalgaryojs |
language |
English |
topic |
Animal distribution Animal migration Animal population Denning Polar bears Winter ecology Wildlife habitat Lancaster Sound Nunavut |
spellingShingle |
Animal distribution Animal migration Animal population Denning Polar bears Winter ecology Wildlife habitat Lancaster Sound Nunavut Schweinsburg, R.E. Lee, L.J. Latour, P.B. Distribution, Movement and Abundance of Polar Bears in Lancaster Sound, Northwest Territories |
topic_facet |
Animal distribution Animal migration Animal population Denning Polar bears Winter ecology Wildlife habitat Lancaster Sound Nunavut |
description |
Mark-recapture studies show that polar bears are distributed at varying densities throughout Lancaster Sound during winter and spring. Major concentrations occur along the north and south coasts and the transverse floe edge at the mouth of the sound. As the ice melts, some bears move west whereas others move to nearby land areas. There is some evidence that as the ice forms, polar bears return from their summer locations to eastern Lancaster Sound. Polar bears of Lancaster Sound are part of the larger population whose western range extends to Barrow Strait, Prince Regent Inlet, Wellington Channel and Jones Sound. The southern and eastern range limits are unknown although this population may extend at least to Clyde River on northeastern Baffin Island and probably to Greenland. Maternity denning appears to be widespread over the study area probably because of the abundance of suitable habitat. We estimated a population of 1031 ± 236 polar bears in Lancaster Sound during 1979: however, more estimates are needed to determine if this relatively high number is normal for the area.Key words: polar bear, distribution, movement, abundance, Baffin Bay, Lancaster Sound, summer retreat, denning |
format |
Article in Journal/Newspaper |
author |
Schweinsburg, R.E. Lee, L.J. Latour, P.B. |
author_facet |
Schweinsburg, R.E. Lee, L.J. Latour, P.B. |
author_sort |
Schweinsburg, R.E. |
title |
Distribution, Movement and Abundance of Polar Bears in Lancaster Sound, Northwest Territories |
title_short |
Distribution, Movement and Abundance of Polar Bears in Lancaster Sound, Northwest Territories |
title_full |
Distribution, Movement and Abundance of Polar Bears in Lancaster Sound, Northwest Territories |
title_fullStr |
Distribution, Movement and Abundance of Polar Bears in Lancaster Sound, Northwest Territories |
title_full_unstemmed |
Distribution, Movement and Abundance of Polar Bears in Lancaster Sound, Northwest Territories |
title_sort |
distribution, movement and abundance of polar bears in lancaster sound, northwest territories |
publisher |
The Arctic Institute of North America |
publishDate |
1982 |
url |
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65368 |
long_lat |
ENVELOPE(-94.168,-94.168,74.402,74.402) ENVELOPE(-70.451,-70.451,69.854,69.854) ENVELOPE(-86.000,-86.000,76.002,76.002) ENVELOPE(-83.999,-83.999,74.218,74.218) ENVELOPE(-90.431,-90.431,72.993,72.993) ENVELOPE(-93.201,-93.201,75.468,75.468) |
geographic |
Baffin Bay Baffin Island Barrow Strait Clyde River Greenland Jones Sound Lancaster Sound Northwest Territories Nunavut Prince Regent Inlet Wellington Channel |
geographic_facet |
Baffin Bay Baffin Island Barrow Strait Clyde River Greenland Jones Sound Lancaster Sound Northwest Territories Nunavut Prince Regent Inlet Wellington Channel |
genre |
Arctic Baffin Bay Baffin Bay Baffin Island Baffin Clyde River Greenland Jones Sound Lancaster Sound Northwest Territories Nunavut polar bear Prince Regent Inlet |
genre_facet |
Arctic Baffin Bay Baffin Bay Baffin Island Baffin Clyde River Greenland Jones Sound Lancaster Sound Northwest Territories Nunavut polar bear Prince Regent Inlet |
op_source |
ARCTIC; Vol. 35 No. 1 (1982): March: 1–240; 159-169 1923-1245 0004-0843 |
op_relation |
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65368/49282 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65368 |
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ARCTIC |
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35 |
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