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    Numerical Simulation of Three-Dimensional, Shape-Preserving Convective Elements

    Source: Journal of the Atmospheric Sciences:;1972:;Volume( 029 ):;issue: 002::page 322
    Author:
    Fox, Douglas G.
    DOI: 10.1175/1520-0469(1972)029<0322:NSOTDS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The motions resulting from the sudden release of a fixed amount of buoyancy in an incompressible fluid are simulated. Solutions are allowed to reach a steady state in the finite computed volume by the introduction of a dynamical stretching of the coordinate system. Fully nonlinear, transformed, and finite-differenced Navier-Stokes equations are integrated in time over a three-dimensional grid. It is shown that a steady-state solution to the transformed equations is equivalent to a self-preserving solution in real space. Physically realistic results are presented for a range of Reynolds numbers between 10 and 100. In a strongly diffusive regime the simulation agrees with an existing theoretical solution. Reynolds numbers of order 50 are sufficient to reproduce many of the features of laboratory experiments.
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      Numerical Simulation of Three-Dimensional, Shape-Preserving Convective Elements

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    contributor authorFox, Douglas G.
    date accessioned2017-06-09T14:16:17Z
    date available2017-06-09T14:16:17Z
    date copyright1972/03/01
    date issued1972
    identifier issn0022-4928
    identifier otherams-16128.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151877
    description abstractThe motions resulting from the sudden release of a fixed amount of buoyancy in an incompressible fluid are simulated. Solutions are allowed to reach a steady state in the finite computed volume by the introduction of a dynamical stretching of the coordinate system. Fully nonlinear, transformed, and finite-differenced Navier-Stokes equations are integrated in time over a three-dimensional grid. It is shown that a steady-state solution to the transformed equations is equivalent to a self-preserving solution in real space. Physically realistic results are presented for a range of Reynolds numbers between 10 and 100. In a strongly diffusive regime the simulation agrees with an existing theoretical solution. Reynolds numbers of order 50 are sufficient to reproduce many of the features of laboratory experiments.
    publisherAmerican Meteorological Society
    titleNumerical Simulation of Three-Dimensional, Shape-Preserving Convective Elements
    typeJournal Paper
    journal volume29
    journal issue2
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1972)029<0322:NSOTDS>2.0.CO;2
    journal fristpage322
    journal lastpage341
    treeJournal of the Atmospheric Sciences:;1972:;Volume( 029 ):;issue: 002
    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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