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    Stochastic Forcing of Perturbation Variance in Unbounded Shear and Deformation Flows

    Source: Journal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 002::page 200
    Author:
    Farrell, Brian F.
    ,
    Ioannou, Petros J.
    DOI: 10.1175/1520-0469(1993)050<0200:SFOPVI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The problem of growth of small perturbations in fluid flow and the related problem of maintenance of perturbation variance has traditionally been studied by appeal to exponential modal instability of the flow. In the event that a flow supports an exponentially growing modal solution, the initially unbounded growth of the mode is taken as more or less compelling evidence for eventual flow breakdown. However, atmospheric flows are characterized by large thermally forced background rates of strain and are subject to perturbations that are not infinitesimal in amplitude. Under these circumstances there is an alternative mechanism for growth and maintenance of perturbation variance: amplification in a straining flow of stochastically forced perturbations in the absence of exponential instabilities. From this viewpoint the flow is regarded as a driven amplifier rather than as an unstable oscillator. We explore this mechanism using as examples unbounded constant shear and pure deformation flow for which closed-form solutions are available and neither of which supports a nonsingular mode. With diffusive dissipation we find that amplification of isotropic band-limited stochastic driving is unbounded for the case of pure deformation and bounded by a threefold increase at large shear for the case of a linear velocity profile. A phenomenological model of the contribution of linear and nonlinear damped modes to the maintenance of variance results in variance levels increasing linearly with shear. We conclude that amplification of stochastic forcing in a straining field can maintain a variance field substantially more energetic than that resulting from the same forcing in the absence of a background straining flow. Our results further indicate that existence of linear and nonlinear damped modes is important in maintaining high levels of variance by the mechanism of stochastic excitation.
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      Stochastic Forcing of Perturbation Variance in Unbounded Shear and Deformation Flows

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4157107
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    contributor authorFarrell, Brian F.
    contributor authorIoannou, Petros J.
    date accessioned2017-06-09T14:31:13Z
    date available2017-06-09T14:31:13Z
    date copyright1993/01/01
    date issued1993
    identifier issn0022-4928
    identifier otherams-20835.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4157107
    description abstractThe problem of growth of small perturbations in fluid flow and the related problem of maintenance of perturbation variance has traditionally been studied by appeal to exponential modal instability of the flow. In the event that a flow supports an exponentially growing modal solution, the initially unbounded growth of the mode is taken as more or less compelling evidence for eventual flow breakdown. However, atmospheric flows are characterized by large thermally forced background rates of strain and are subject to perturbations that are not infinitesimal in amplitude. Under these circumstances there is an alternative mechanism for growth and maintenance of perturbation variance: amplification in a straining flow of stochastically forced perturbations in the absence of exponential instabilities. From this viewpoint the flow is regarded as a driven amplifier rather than as an unstable oscillator. We explore this mechanism using as examples unbounded constant shear and pure deformation flow for which closed-form solutions are available and neither of which supports a nonsingular mode. With diffusive dissipation we find that amplification of isotropic band-limited stochastic driving is unbounded for the case of pure deformation and bounded by a threefold increase at large shear for the case of a linear velocity profile. A phenomenological model of the contribution of linear and nonlinear damped modes to the maintenance of variance results in variance levels increasing linearly with shear. We conclude that amplification of stochastic forcing in a straining field can maintain a variance field substantially more energetic than that resulting from the same forcing in the absence of a background straining flow. Our results further indicate that existence of linear and nonlinear damped modes is important in maintaining high levels of variance by the mechanism of stochastic excitation.
    publisherAmerican Meteorological Society
    titleStochastic Forcing of Perturbation Variance in Unbounded Shear and Deformation Flows
    typeJournal Paper
    journal volume50
    journal issue2
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1993)050<0200:SFOPVI>2.0.CO;2
    journal fristpage200
    journal lastpage211
    treeJournal of the Atmospheric Sciences:;1993:;Volume( 050 ):;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
    yabeshDSpacePersian