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    Transient Development of Perturbations in Stratified Shear Flow

    Source: Journal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 014::page 2201
    Author:
    Farrell, Brian F.
    ,
    Ioannou, Petros J.
    DOI: 10.1175/1520-0469(1993)050<2201:TDOPIS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Transient development of perturbations in inviscid stratified shear flow is investigated. Use is made of closed form analytic solutions that allow concise identification of optimally growing plane-wave solutions for the case of an unbounded flow with constant shear and stratification. For the case of channel flow, variational techniques are employed to determine the optimally growing disturbances. The maximum energy growth attained over a specific time interval decreases continuously with increasing stratification, and no special significance attaches to Ri = 0.25. Indeed, transient growth can be substantial even for Ri = O(1). A general lower bound on the energy growth attained by an optimal perturbation in a stratified flow over a given time interval is the square root of the growth attained by the corresponding perturbation in unstratified flow. Enhanced perturbation persistence is found for mean-flow stratification lying in the range 0.1 < Ri < 0.3. Small but finite perturbations in mean flow with Ri < 0.4 produce regions with locally negative total density gradient, which are expected to overturn. Although the perturbations are of wave form, buoyancy fluxes mediate transfer between perturbation kinetic and potential energy during transient development, thus implying that buoyancy flux is not a determinative diagnostic for distinguishing between waves and turbulence in stratified flows.
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      Transient Development of Perturbations in Stratified Shear Flow

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4157257
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    contributor authorFarrell, Brian F.
    contributor authorIoannou, Petros J.
    date accessioned2017-06-09T14:31:38Z
    date available2017-06-09T14:31:38Z
    date copyright1993/07/01
    date issued1993
    identifier issn0022-4928
    identifier otherams-20970.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4157257
    description abstractTransient development of perturbations in inviscid stratified shear flow is investigated. Use is made of closed form analytic solutions that allow concise identification of optimally growing plane-wave solutions for the case of an unbounded flow with constant shear and stratification. For the case of channel flow, variational techniques are employed to determine the optimally growing disturbances. The maximum energy growth attained over a specific time interval decreases continuously with increasing stratification, and no special significance attaches to Ri = 0.25. Indeed, transient growth can be substantial even for Ri = O(1). A general lower bound on the energy growth attained by an optimal perturbation in a stratified flow over a given time interval is the square root of the growth attained by the corresponding perturbation in unstratified flow. Enhanced perturbation persistence is found for mean-flow stratification lying in the range 0.1 < Ri < 0.3. Small but finite perturbations in mean flow with Ri < 0.4 produce regions with locally negative total density gradient, which are expected to overturn. Although the perturbations are of wave form, buoyancy fluxes mediate transfer between perturbation kinetic and potential energy during transient development, thus implying that buoyancy flux is not a determinative diagnostic for distinguishing between waves and turbulence in stratified flows.
    publisherAmerican Meteorological Society
    titleTransient Development of Perturbations in Stratified Shear Flow
    typeJournal Paper
    journal volume50
    journal issue14
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1993)050<2201:TDOPIS>2.0.CO;2
    journal fristpage2201
    journal lastpage2214
    treeJournal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 014
    contenttypeFulltext
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