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    Linear Trends of Temperature at Intermediate and Deep Layers of the North Atlantic and the North Pacific Oceans: 1957–1981

    Source: Journal of Climate:;1993:;volume( 006 ):;issue: 010::page 1928
    Author:
    Antonov, John I.
    DOI: 10.1175/1520-0442(1993)006<1928:LTOTAI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Using all available hydrographic station data on ocean temperature observations from World Data Center-B (Obninsk, Russia), investigation of temperature changes in the North Atlantic and North Pacific oceans within the depth range of 300 to 3000 m has been carried out for the period 1957?1981. Results of statistical data analysis show that in the upper layer to about 500-m depths of both oceans, on average, seawater temperature declined. Deeper than 500?600 m in the North Pacific Ocean, no significant temperature changes have been revealed for this 25-year time interval. On average, for the North Atlantic Ocean, a statistically significant temperature rise (about 0.1°C 25 yr?1) is observed in the 800- to 2500-m layer.
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      Linear Trends of Temperature at Intermediate and Deep Layers of the North Atlantic and the North Pacific Oceans: 1957–1981

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4179478
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    contributor authorAntonov, John I.
    date accessioned2017-06-09T15:20:26Z
    date available2017-06-09T15:20:26Z
    date copyright1993/10/01
    date issued1993
    identifier issn0894-8755
    identifier otherams-4097.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4179478
    description abstractUsing all available hydrographic station data on ocean temperature observations from World Data Center-B (Obninsk, Russia), investigation of temperature changes in the North Atlantic and North Pacific oceans within the depth range of 300 to 3000 m has been carried out for the period 1957?1981. Results of statistical data analysis show that in the upper layer to about 500-m depths of both oceans, on average, seawater temperature declined. Deeper than 500?600 m in the North Pacific Ocean, no significant temperature changes have been revealed for this 25-year time interval. On average, for the North Atlantic Ocean, a statistically significant temperature rise (about 0.1°C 25 yr?1) is observed in the 800- to 2500-m layer.
    publisherAmerican Meteorological Society
    titleLinear Trends of Temperature at Intermediate and Deep Layers of the North Atlantic and the North Pacific Oceans: 1957–1981
    typeJournal Paper
    journal volume6
    journal issue10
    journal titleJournal of Climate
    identifier doi10.1175/1520-0442(1993)006<1928:LTOTAI>2.0.CO;2
    journal fristpage1928
    journal lastpage1942
    treeJournal of Climate:;1993:;volume( 006 ):;issue: 010
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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