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    The Shape of the Main Thermocline

    Source: Journal of Physical Oceanography:;1982:;Volume( 012 ):;issue: 012::page 1458
    Author:
    Salmon, Rick
    DOI: 10.1175/1520-0485(1982)012<1458:TSOTMT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The mean ocean density field resembles the state of maximum entropy with given values for the upper water mass, total energy and potential enstrophy. Numerical experiments confirm that the thermocline of a freely evolving two-layer model spontaneously assumes the observed double-lobe shape.
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      The Shape of the Main Thermocline

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4163327
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    contributor authorSalmon, Rick
    date accessioned2017-06-09T14:46:24Z
    date available2017-06-09T14:46:24Z
    date copyright1982/12/01
    date issued1982
    identifier issn0022-3670
    identifier otherams-26433.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4163327
    description abstractThe mean ocean density field resembles the state of maximum entropy with given values for the upper water mass, total energy and potential enstrophy. Numerical experiments confirm that the thermocline of a freely evolving two-layer model spontaneously assumes the observed double-lobe shape.
    publisherAmerican Meteorological Society
    titleThe Shape of the Main Thermocline
    typeJournal Paper
    journal volume12
    journal issue12
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1982)012<1458:TSOTMT>2.0.CO;2
    journal fristpage1458
    journal lastpage1479
    treeJournal of Physical Oceanography:;1982:;Volume( 012 ):;issue: 012
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian