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    Convection of Isolated Masses of a Buoyant Fluid: A Numerical Calculation

    Source: Journal of the Atmospheric Sciences:;1962:;Volume( 019 ):;issue: 006::page 492
    Author:
    Ogura, Yoshimitsu
    DOI: 10.1175/1520-0469(1962)019<0492:COIMOA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The equations of motion for an incompressible fluid have been integrated numerically, as an initial value problem, for the axially-symmetric motion produced by release of an isolated lighter mass of the same fluid. The effect of viscosity is included only implicitly in the finite-difference numerical process. The numerical solutions exhibit the similarity (shape-preserving) stage assumed in theoretical treatments and observed in tank experiments. The computations have been repeated for different values of the total weight deficiency (or excess) of the ?thermal.? The results agree approximately with the relationships predicted by dimensional analysis. The values of various parameters are compared with those obtained in tank experiments and encouraging agreement between them is found. Truncation errors involved in the numerical integration are briefly discussed.
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      Convection of Isolated Masses of a Buoyant Fluid: A Numerical Calculation

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    contributor authorOgura, Yoshimitsu
    date accessioned2017-06-09T14:12:58Z
    date available2017-06-09T14:12:58Z
    date copyright1962/11/01
    date issued1962
    identifier issn0022-4928
    identifier otherams-14876.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150485
    description abstractThe equations of motion for an incompressible fluid have been integrated numerically, as an initial value problem, for the axially-symmetric motion produced by release of an isolated lighter mass of the same fluid. The effect of viscosity is included only implicitly in the finite-difference numerical process. The numerical solutions exhibit the similarity (shape-preserving) stage assumed in theoretical treatments and observed in tank experiments. The computations have been repeated for different values of the total weight deficiency (or excess) of the ?thermal.? The results agree approximately with the relationships predicted by dimensional analysis. The values of various parameters are compared with those obtained in tank experiments and encouraging agreement between them is found. Truncation errors involved in the numerical integration are briefly discussed.
    publisherAmerican Meteorological Society
    titleConvection of Isolated Masses of a Buoyant Fluid: A Numerical Calculation
    typeJournal Paper
    journal volume19
    journal issue6
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1962)019<0492:COIMOA>2.0.CO;2
    journal fristpage492
    journal lastpage502
    treeJournal of the Atmospheric Sciences:;1962:;Volume( 019 ):;issue: 006
    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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