Oceanographic Features of the Canadian Archipelago

Oceanographic data collected during the first cruise of H.M.C.S. Labrador to the Canadian Arctic in August and September 1954 permit comparisons of the vertical temperature and salinity structures in Baffin Bay, the Canadian Archipelago and the Arctic Ocean. From a comparison of the temperature–sali...

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Published in:Journal of the Fisheries Research Board of Canada
Main Author: Bailey, W. B.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1957
Subjects:
Online Access:http://dx.doi.org/10.1139/f57-030
http://www.nrcresearchpress.com/doi/pdf/10.1139/f57-030
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spelling crcansciencepubl:10.1139/f57-030 2024-09-15T17:53:08+00:00 Oceanographic Features of the Canadian Archipelago Bailey, W. B. 1957 http://dx.doi.org/10.1139/f57-030 http://www.nrcresearchpress.com/doi/pdf/10.1139/f57-030 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Journal of the Fisheries Research Board of Canada volume 14, issue 5, page 731-769 ISSN 0015-296X journal-article 1957 crcansciencepubl https://doi.org/10.1139/f57-030 2024-07-25T04:10:03Z Oceanographic data collected during the first cruise of H.M.C.S. Labrador to the Canadian Arctic in August and September 1954 permit comparisons of the vertical temperature and salinity structures in Baffin Bay, the Canadian Archipelago and the Arctic Ocean. From a comparison of the temperature–salinity characteristics of the waters in the Arctic Ocean (Beaufort Sea) with those in Baffin Bay, it is found that: (a) the surface waters of the Arctic Ocean are much less saline than those in Baffin Bay, but minimum temperatures are the same (−1.8 °C), (b) the waters of the upper 200 m. in Baffin Bay are denser than those found at corresponding depths in the Arctic Ocean, (c) below 200 m., Arctic waters are the denser, and below 500 m. they are denser than any waters found in Baffin Bay, and (d) waters found at 250 m. in the Beaufort Sea, at 500 m. in Smith Sound, and at 1250 m. in central Baffin Bay, have identical temperature and salinity characteristics (−0.3 °C., 34.4‰).In addition the data permitted limited investigations into the effect of drifting ice floes on the vertical temperature structure of the water, the origin of the "north water", long-term variations in the oceanographic conditions in Baffin Bay, and dynamic calculations of currents and volume transports of the waters through the channels leading into Baffin Bay. Article in Journal/Newspaper Arctic Ocean Baffin Bay Baffin Bay Baffin Beaufort Sea Canadian Archipelago Smith sound Canadian Science Publishing Journal of the Fisheries Research Board of Canada 14 5 731 769
institution Open Polar
collection Canadian Science Publishing
op_collection_id crcansciencepubl
language English
description Oceanographic data collected during the first cruise of H.M.C.S. Labrador to the Canadian Arctic in August and September 1954 permit comparisons of the vertical temperature and salinity structures in Baffin Bay, the Canadian Archipelago and the Arctic Ocean. From a comparison of the temperature–salinity characteristics of the waters in the Arctic Ocean (Beaufort Sea) with those in Baffin Bay, it is found that: (a) the surface waters of the Arctic Ocean are much less saline than those in Baffin Bay, but minimum temperatures are the same (−1.8 °C), (b) the waters of the upper 200 m. in Baffin Bay are denser than those found at corresponding depths in the Arctic Ocean, (c) below 200 m., Arctic waters are the denser, and below 500 m. they are denser than any waters found in Baffin Bay, and (d) waters found at 250 m. in the Beaufort Sea, at 500 m. in Smith Sound, and at 1250 m. in central Baffin Bay, have identical temperature and salinity characteristics (−0.3 °C., 34.4‰).In addition the data permitted limited investigations into the effect of drifting ice floes on the vertical temperature structure of the water, the origin of the "north water", long-term variations in the oceanographic conditions in Baffin Bay, and dynamic calculations of currents and volume transports of the waters through the channels leading into Baffin Bay.
format Article in Journal/Newspaper
author Bailey, W. B.
spellingShingle Bailey, W. B.
Oceanographic Features of the Canadian Archipelago
author_facet Bailey, W. B.
author_sort Bailey, W. B.
title Oceanographic Features of the Canadian Archipelago
title_short Oceanographic Features of the Canadian Archipelago
title_full Oceanographic Features of the Canadian Archipelago
title_fullStr Oceanographic Features of the Canadian Archipelago
title_full_unstemmed Oceanographic Features of the Canadian Archipelago
title_sort oceanographic features of the canadian archipelago
publisher Canadian Science Publishing
publishDate 1957
url http://dx.doi.org/10.1139/f57-030
http://www.nrcresearchpress.com/doi/pdf/10.1139/f57-030
genre Arctic Ocean
Baffin Bay
Baffin Bay
Baffin
Beaufort Sea
Canadian Archipelago
Smith sound
genre_facet Arctic Ocean
Baffin Bay
Baffin Bay
Baffin
Beaufort Sea
Canadian Archipelago
Smith sound
op_source Journal of the Fisheries Research Board of Canada
volume 14, issue 5, page 731-769
ISSN 0015-296X
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/f57-030
container_title Journal of the Fisheries Research Board of Canada
container_volume 14
container_issue 5
container_start_page 731
op_container_end_page 769
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