Anomalous Conditions in the Slope Water Area in 1959

An oceanographic section made with the research vessel Crawford in June 1959 showed that the proportion of Labrador-Coastal Water to Slope Water at the meridian 57°30′W was unusually large. Data from this section combined with bathythermograms taken elsewhere in the Slope Water area and direct deep...

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Published in:Journal of the Fisheries Research Board of Canada
Main Author: Worthington, L. V.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1964
Subjects:
Online Access:http://dx.doi.org/10.1139/f64-025
http://www.nrcresearchpress.com/doi/pdf/10.1139/f64-025
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spelling crcansciencepubl:10.1139/f64-025 2023-12-17T10:46:27+01:00 Anomalous Conditions in the Slope Water Area in 1959 Worthington, L. V. 1964 http://dx.doi.org/10.1139/f64-025 http://www.nrcresearchpress.com/doi/pdf/10.1139/f64-025 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Journal of the Fisheries Research Board of Canada volume 21, issue 2, page 327-333 ISSN 0015-296X General Medicine journal-article 1964 crcansciencepubl https://doi.org/10.1139/f64-025 2023-11-19T13:39:36Z An oceanographic section made with the research vessel Crawford in June 1959 showed that the proportion of Labrador-Coastal Water to Slope Water at the meridian 57°30′W was unusually large. Data from this section combined with bathythermograms taken elsewhere in the Slope Water area and direct deep current measurements suggest that there was an abnormal influx of cold water from the Labrador Basin in 1959. This suggestion is strengthened by the high incidence of coastal fog in the summer of 1959. It is suggested that the cause of this influx was an abnormal North Atlantic weather pattern in January 1959. Article in Journal/Newspaper North Atlantic Canadian Science Publishing (via Crossref) Crawford ENVELOPE(-86.467,-86.467,-77.717,-77.717) Journal of the Fisheries Research Board of Canada 21 2 327 333
institution Open Polar
collection Canadian Science Publishing (via Crossref)
op_collection_id crcansciencepubl
language English
topic General Medicine
spellingShingle General Medicine
Worthington, L. V.
Anomalous Conditions in the Slope Water Area in 1959
topic_facet General Medicine
description An oceanographic section made with the research vessel Crawford in June 1959 showed that the proportion of Labrador-Coastal Water to Slope Water at the meridian 57°30′W was unusually large. Data from this section combined with bathythermograms taken elsewhere in the Slope Water area and direct deep current measurements suggest that there was an abnormal influx of cold water from the Labrador Basin in 1959. This suggestion is strengthened by the high incidence of coastal fog in the summer of 1959. It is suggested that the cause of this influx was an abnormal North Atlantic weather pattern in January 1959.
format Article in Journal/Newspaper
author Worthington, L. V.
author_facet Worthington, L. V.
author_sort Worthington, L. V.
title Anomalous Conditions in the Slope Water Area in 1959
title_short Anomalous Conditions in the Slope Water Area in 1959
title_full Anomalous Conditions in the Slope Water Area in 1959
title_fullStr Anomalous Conditions in the Slope Water Area in 1959
title_full_unstemmed Anomalous Conditions in the Slope Water Area in 1959
title_sort anomalous conditions in the slope water area in 1959
publisher Canadian Science Publishing
publishDate 1964
url http://dx.doi.org/10.1139/f64-025
http://www.nrcresearchpress.com/doi/pdf/10.1139/f64-025
long_lat ENVELOPE(-86.467,-86.467,-77.717,-77.717)
geographic Crawford
geographic_facet Crawford
genre North Atlantic
genre_facet North Atlantic
op_source Journal of the Fisheries Research Board of Canada
volume 21, issue 2, page 327-333
ISSN 0015-296X
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/f64-025
container_title Journal of the Fisheries Research Board of Canada
container_volume 21
container_issue 2
container_start_page 327
op_container_end_page 333
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