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    A Simple Model of the Thermocline in a Bounded Ocean

    Source: Journal of Physical Oceanography:;1971:;Volume( 001 ):;issue: 001::page 7
    Author:
    Barcilon, Victor
    DOI: 10.1175/1520-0485(1971)001<0007:ASMOTT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A linear model of the thermocline is examined for an ocean bounded by both eastern and western coasts. The analysis is carried out on a ?-plane for an ocean in which diffusion of heat but not of momentum is important. Particular attention is devoted to the structure of the thermocline in the vicinity of the western coast along which a boundary layer exists. A unique feature of the present thermocline is the absence of any vertical velocity below the thermocline.
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      A Simple Model of the Thermocline in a Bounded Ocean

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4162007
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    contributor authorBarcilon, Victor
    date accessioned2017-06-09T14:43:26Z
    date available2017-06-09T14:43:26Z
    date copyright1971/01/01
    date issued1971
    identifier issn0022-3670
    identifier otherams-25245.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162007
    description abstractA linear model of the thermocline is examined for an ocean bounded by both eastern and western coasts. The analysis is carried out on a ?-plane for an ocean in which diffusion of heat but not of momentum is important. Particular attention is devoted to the structure of the thermocline in the vicinity of the western coast along which a boundary layer exists. A unique feature of the present thermocline is the absence of any vertical velocity below the thermocline.
    publisherAmerican Meteorological Society
    titleA Simple Model of the Thermocline in a Bounded Ocean
    typeJournal Paper
    journal volume1
    journal issue1
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1971)001<0007:ASMOTT>2.0.CO;2
    journal fristpage7
    journal lastpage11
    treeJournal of Physical Oceanography:;1971:;Volume( 001 ):;issue: 001
    contenttypeFulltext
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