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    A Numerical Study in Three Space Dimensions of Bénard Convection in a Rotating Fluid

    Source: Journal of the Atmospheric Sciences:;1973:;Volume( 030 ):;issue: 004::page 590
    Author:
    Somerville, Richard C. J.
    ,
    Lipps, Frank B.
    DOI: 10.1175/1520-0469(1973)030<0590:ANSITS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The primitive, nonlinear, Boussinesq equations of motion, continuity and thermodynamic energy are integrated numerically in three space dimensions and time to study convection driven by unstable vertical density gradients and subject to Coriolis forces. Parameter values are chosen to permit quantitative comparison with data from laboratory experiments for rotating Bénard convection in water. The model realistically simulates the structure of the convection cells, their horizontal scale, and the mean vertical heat transport. The experimentally observed phenomenon of a non-monotone dependence of heat transport on rotation rate is reproduced and shown to be a consequence of the rotational constraint on the wavelength of the cells.
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      A Numerical Study in Three Space Dimensions of Bénard Convection in a Rotating Fluid

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4152141
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    contributor authorSomerville, Richard C. J.
    contributor authorLipps, Frank B.
    date accessioned2017-06-09T14:16:55Z
    date available2017-06-09T14:16:55Z
    date copyright1973/05/01
    date issued1973
    identifier issn0022-4928
    identifier otherams-16366.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152141
    description abstractThe primitive, nonlinear, Boussinesq equations of motion, continuity and thermodynamic energy are integrated numerically in three space dimensions and time to study convection driven by unstable vertical density gradients and subject to Coriolis forces. Parameter values are chosen to permit quantitative comparison with data from laboratory experiments for rotating Bénard convection in water. The model realistically simulates the structure of the convection cells, their horizontal scale, and the mean vertical heat transport. The experimentally observed phenomenon of a non-monotone dependence of heat transport on rotation rate is reproduced and shown to be a consequence of the rotational constraint on the wavelength of the cells.
    publisherAmerican Meteorological Society
    titleA Numerical Study in Three Space Dimensions of Bénard Convection in a Rotating Fluid
    typeJournal Paper
    journal volume30
    journal issue4
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1973)030<0590:ANSITS>2.0.CO;2
    journal fristpage590
    journal lastpage596
    treeJournal of the Atmospheric Sciences:;1973:;Volume( 030 ):;issue: 004
    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