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    The Salinity Effect in a Mixed Layer Ocean Model

    Source: Journal of Physical Oceanography:;1976:;Volume( 006 ):;issue: 001::page 29
    Author:
    Miller, James R.
    DOI: 10.1175/1520-0485(1976)006<0029:TSEIAM>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A model of the thermally mixed layer in the upper ocean as developed by Kraus and Turner and extended by Denman is further extended to investigate the effects of salinity. In the tropical and subtropical Atlantic Ocean rapid increases in salinity occur at the bottom of a uniformly mixed surface layer. The most significant effects produced by the inclusion of salinity are the reduction of the deepening rate and the corresponding change in the heating characteristics of the mixed layer. If the net surface heating is positive, but small, salinity effects must be included to determine whether the mixed layer temperature will increase or decrease. Precipitation over tropical oceans leads to the development of a shallow stable layer accompanied by a decrease in the temperature and salinity at the sea surface.
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      The Salinity Effect in a Mixed Layer Ocean Model

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    contributor authorMiller, James R.
    date accessioned2017-06-09T14:44:11Z
    date available2017-06-09T14:44:11Z
    date copyright1976/01/01
    date issued1976
    identifier issn0022-3670
    identifier otherams-25566.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162363
    description abstractA model of the thermally mixed layer in the upper ocean as developed by Kraus and Turner and extended by Denman is further extended to investigate the effects of salinity. In the tropical and subtropical Atlantic Ocean rapid increases in salinity occur at the bottom of a uniformly mixed surface layer. The most significant effects produced by the inclusion of salinity are the reduction of the deepening rate and the corresponding change in the heating characteristics of the mixed layer. If the net surface heating is positive, but small, salinity effects must be included to determine whether the mixed layer temperature will increase or decrease. Precipitation over tropical oceans leads to the development of a shallow stable layer accompanied by a decrease in the temperature and salinity at the sea surface.
    publisherAmerican Meteorological Society
    titleThe Salinity Effect in a Mixed Layer Ocean Model
    typeJournal Paper
    journal volume6
    journal issue1
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1976)006<0029:TSEIAM>2.0.CO;2
    journal fristpage29
    journal lastpage35
    treeJournal of Physical Oceanography:;1976:;Volume( 006 ):;issue: 001
    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
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