Climatic Trends and Fluctuations in Yield of Marine Fisheries of the Northeast Pacific

Mean annual air temperature at San Francisco, California, New Westminster and Masset, British Columbia, all had a rising trend from 1920 to 1940, then declined to 1950. Amplitude was greatest at Masset, least at San Francisco. The 20-years' rise is similar to the story in the North Atlantic oce...

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Published in:Journal of the Fisheries Research Board of Canada
Main Author: Ketchen, K. S.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1956
Subjects:
Online Access:http://dx.doi.org/10.1139/f56-024
http://www.nrcresearchpress.com/doi/pdf/10.1139/f56-024
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author Ketchen, K. S.
author_facet Ketchen, K. S.
author_sort Ketchen, K. S.
collection Canadian Science Publishing
container_issue 3
container_start_page 357
container_title Journal of the Fisheries Research Board of Canada
container_volume 13
description Mean annual air temperature at San Francisco, California, New Westminster and Masset, British Columbia, all had a rising trend from 1920 to 1940, then declined to 1950. Amplitude was greatest at Masset, least at San Francisco. The 20-years' rise is similar to the story in the North Atlantic ocean, but the recent decline has no parallel there. Prior to 1920 there were considerable differences among the above three stations. Mean annual ocean temperature at Nanaimo, B.C., is similar to air temperature at New Westminster since 1915. "Winter" ocean temperatures (February–April) show similar but not identical trends, and are thought to best represent conditions at the time eggs and larvae of most commercial bottom fishes are in the water.Suggestive short-term correlations have been observed as follows: 1. a positive correlation between winter temperature and abundance of brill 6 years later; 2. a negative correlation between winter temperature and rock sole abundance 5 years later; 3. a negative correlation between winter temperature and strength of year-classes in lemon sole. Over a longer period, there is much resemblance between the temperature history since 1910 and the abundance of halibut broods, as indicated by catch per unit effort 10 years later (southern grounds) or 12 years later (Western grounds). The relationship is positive, and for western grounds is similar even in details. Over a somewhat shorter period, blackcod abundance has varied inversely with winter temperature. Marked changes in abundance and distribution of true (grey) cod since about 1900 cannot be related to temperature series available.
format Article in Journal/Newspaper
genre North Atlantic
genre_facet North Atlantic
geographic Pacific
Westminster
Masset
geographic_facet Pacific
Westminster
Masset
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language English
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op_doi https://doi.org/10.1139/f56-024
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op_source Journal of the Fisheries Research Board of Canada
volume 13, issue 3, page 357-374
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spelling crcansciencepubl:10.1139/f56-024 2025-01-16T23:42:54+00:00 Climatic Trends and Fluctuations in Yield of Marine Fisheries of the Northeast Pacific Ketchen, K. S. 1956 http://dx.doi.org/10.1139/f56-024 http://www.nrcresearchpress.com/doi/pdf/10.1139/f56-024 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Journal of the Fisheries Research Board of Canada volume 13, issue 3, page 357-374 ISSN 0015-296X General Medicine journal-article 1956 crcansciencepubl https://doi.org/10.1139/f56-024 2023-11-19T13:38:48Z Mean annual air temperature at San Francisco, California, New Westminster and Masset, British Columbia, all had a rising trend from 1920 to 1940, then declined to 1950. Amplitude was greatest at Masset, least at San Francisco. The 20-years' rise is similar to the story in the North Atlantic ocean, but the recent decline has no parallel there. Prior to 1920 there were considerable differences among the above three stations. Mean annual ocean temperature at Nanaimo, B.C., is similar to air temperature at New Westminster since 1915. "Winter" ocean temperatures (February–April) show similar but not identical trends, and are thought to best represent conditions at the time eggs and larvae of most commercial bottom fishes are in the water.Suggestive short-term correlations have been observed as follows: 1. a positive correlation between winter temperature and abundance of brill 6 years later; 2. a negative correlation between winter temperature and rock sole abundance 5 years later; 3. a negative correlation between winter temperature and strength of year-classes in lemon sole. Over a longer period, there is much resemblance between the temperature history since 1910 and the abundance of halibut broods, as indicated by catch per unit effort 10 years later (southern grounds) or 12 years later (Western grounds). The relationship is positive, and for western grounds is similar even in details. Over a somewhat shorter period, blackcod abundance has varied inversely with winter temperature. Marked changes in abundance and distribution of true (grey) cod since about 1900 cannot be related to temperature series available. Article in Journal/Newspaper North Atlantic Canadian Science Publishing Pacific Westminster ENVELOPE(169.367,169.367,-84.983,-84.983) Masset ENVELOPE(-132.147,-132.147,54.011,54.011) Journal of the Fisheries Research Board of Canada 13 3 357 374
spellingShingle General Medicine
Ketchen, K. S.
Climatic Trends and Fluctuations in Yield of Marine Fisheries of the Northeast Pacific
title Climatic Trends and Fluctuations in Yield of Marine Fisheries of the Northeast Pacific
title_full Climatic Trends and Fluctuations in Yield of Marine Fisheries of the Northeast Pacific
title_fullStr Climatic Trends and Fluctuations in Yield of Marine Fisheries of the Northeast Pacific
title_full_unstemmed Climatic Trends and Fluctuations in Yield of Marine Fisheries of the Northeast Pacific
title_short Climatic Trends and Fluctuations in Yield of Marine Fisheries of the Northeast Pacific
title_sort climatic trends and fluctuations in yield of marine fisheries of the northeast pacific
topic General Medicine
topic_facet General Medicine
url http://dx.doi.org/10.1139/f56-024
http://www.nrcresearchpress.com/doi/pdf/10.1139/f56-024