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    Finite Amplitude Free Convection as an Initial Value Problem—I

    Source: Journal of the Atmospheric Sciences:;1962:;Volume( 019 ):;issue: 004::page 329
    Author:
    Saltzman, Barry
    DOI: 10.1175/1520-0469(1962)019<0329:FAFCAA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The Oberbeck-Boussinesq equations are reduced to a two-dimensional form governing ?roll? convection between two free surfaces maintained at a constant temperature difference. These equations are then transformed to a set of ordinary differential equations governing the time variations of the double-Fourier coefficients for the motion and temperature fields. Non-linear transfer processes are retained and appear as quadratic interactions between the Fourier coefficients. Energy and heat transfer relations appropriate to this Fourier resolution, and a numerical method for solution from arbitrary initial conditions are given. As examples of the method, numerical solutions for a highly truncated Fourier representation are presented. These solutions, which are for a fixed Prandtl number and variable Rayleigh numbers, show the transient growth of convection from small perturbations, and in all cases studied approach steady states. The steady states obtained agree favorably with steady-state solutions obtained by previous investigators.
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      Finite Amplitude Free Convection as an Initial Value Problem—I

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4150463
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    contributor authorSaltzman, Barry
    date accessioned2017-06-09T14:12:55Z
    date available2017-06-09T14:12:55Z
    date copyright1962/07/01
    date issued1962
    identifier issn0022-4928
    identifier otherams-14856.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150463
    description abstractThe Oberbeck-Boussinesq equations are reduced to a two-dimensional form governing ?roll? convection between two free surfaces maintained at a constant temperature difference. These equations are then transformed to a set of ordinary differential equations governing the time variations of the double-Fourier coefficients for the motion and temperature fields. Non-linear transfer processes are retained and appear as quadratic interactions between the Fourier coefficients. Energy and heat transfer relations appropriate to this Fourier resolution, and a numerical method for solution from arbitrary initial conditions are given. As examples of the method, numerical solutions for a highly truncated Fourier representation are presented. These solutions, which are for a fixed Prandtl number and variable Rayleigh numbers, show the transient growth of convection from small perturbations, and in all cases studied approach steady states. The steady states obtained agree favorably with steady-state solutions obtained by previous investigators.
    publisherAmerican Meteorological Society
    titleFinite Amplitude Free Convection as an Initial Value Problem—I
    typeJournal Paper
    journal volume19
    journal issue4
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1962)019<0329:FAFCAA>2.0.CO;2
    journal fristpage329
    journal lastpage341
    treeJournal of the Atmospheric Sciences:;1962:;Volume( 019 ):;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
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