Evidence of a Westward-Flowing "Subarctic Countercurrent" in the North Pacific Ocean

An examination of surface current velocity data obtained from two independent ship sources suggests the presence of a narrow, weak, westward-flowing countercurrent at a latitude of approximately 50°N in the subarctic Pacific region. Oceanographic survey data collected in the region from the summers...

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Published in:Journal of the Fisheries Research Board of Canada
Main Author: Tabata, S.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1976
Subjects:
Online Access:http://dx.doi.org/10.1139/f76-267
http://www.nrcresearchpress.com/doi/pdf/10.1139/f76-267
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spelling crcansciencepubl:10.1139/f76-267 2023-12-17T10:50:44+01:00 Evidence of a Westward-Flowing "Subarctic Countercurrent" in the North Pacific Ocean Tabata, S. 1976 http://dx.doi.org/10.1139/f76-267 http://www.nrcresearchpress.com/doi/pdf/10.1139/f76-267 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Journal of the Fisheries Research Board of Canada volume 33, issue 10, page 2168-2196 ISSN 0015-296X General Medicine journal-article 1976 crcansciencepubl https://doi.org/10.1139/f76-267 2023-11-19T13:38:56Z An examination of surface current velocity data obtained from two independent ship sources suggests the presence of a narrow, weak, westward-flowing countercurrent at a latitude of approximately 50°N in the subarctic Pacific region. Oceanographic survey data collected in the region from the summers of 1958 and 1959 also indicate such a countercurrent extending zonally for more than 1000 km. The countercurrent can be explained by consideration of the wind-stress vorticity field over the region. Article in Journal/Newspaper Subarctic Canadian Science Publishing (via Crossref) Pacific Journal of the Fisheries Research Board of Canada 33 10 2168 2196
institution Open Polar
collection Canadian Science Publishing (via Crossref)
op_collection_id crcansciencepubl
language English
topic General Medicine
spellingShingle General Medicine
Tabata, S.
Evidence of a Westward-Flowing "Subarctic Countercurrent" in the North Pacific Ocean
topic_facet General Medicine
description An examination of surface current velocity data obtained from two independent ship sources suggests the presence of a narrow, weak, westward-flowing countercurrent at a latitude of approximately 50°N in the subarctic Pacific region. Oceanographic survey data collected in the region from the summers of 1958 and 1959 also indicate such a countercurrent extending zonally for more than 1000 km. The countercurrent can be explained by consideration of the wind-stress vorticity field over the region.
format Article in Journal/Newspaper
author Tabata, S.
author_facet Tabata, S.
author_sort Tabata, S.
title Evidence of a Westward-Flowing "Subarctic Countercurrent" in the North Pacific Ocean
title_short Evidence of a Westward-Flowing "Subarctic Countercurrent" in the North Pacific Ocean
title_full Evidence of a Westward-Flowing "Subarctic Countercurrent" in the North Pacific Ocean
title_fullStr Evidence of a Westward-Flowing "Subarctic Countercurrent" in the North Pacific Ocean
title_full_unstemmed Evidence of a Westward-Flowing "Subarctic Countercurrent" in the North Pacific Ocean
title_sort evidence of a westward-flowing "subarctic countercurrent" in the north pacific ocean
publisher Canadian Science Publishing
publishDate 1976
url http://dx.doi.org/10.1139/f76-267
http://www.nrcresearchpress.com/doi/pdf/10.1139/f76-267
geographic Pacific
geographic_facet Pacific
genre Subarctic
genre_facet Subarctic
op_source Journal of the Fisheries Research Board of Canada
volume 33, issue 10, page 2168-2196
ISSN 0015-296X
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/f76-267
container_title Journal of the Fisheries Research Board of Canada
container_volume 33
container_issue 10
container_start_page 2168
op_container_end_page 2196
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