YaBeSH Engineering and Technology Library

    • Journals
    • PaperQuest
    • YSE Standards
    • YaBeSH
    • Login
    View Item 
    •   YE&T Library
    • AMS
    • Journal of the Atmospheric Sciences
    • View Item
    •   YE&T Library
    • AMS
    • Journal of the Atmospheric Sciences
    • View Item
    • All Fields
    • Source Title
    • Year
    • Publisher
    • Title
    • Subject
    • Author
    • DOI
    • ISBN
    Advanced Search
    JavaScript is disabled for your browser. Some features of this site may not work without it.

    Archive

    Transient Dynamics of Nonsymmetric Perturbations versus Symmetric Instability in Baroclinic Zonal Shear Flows

    Source: Journal of the Atmospheric Sciences:;2010:;Volume( 067 ):;issue: 009::page 2972
    Author:
    Mamatsashvili, G. R.
    ,
    Avsarkisov, V. S.
    ,
    Chagelishvili, G. D.
    ,
    Chanishvili, R. G.
    ,
    Kalashnik, M. V.
    DOI: 10.1175/2010JAS3313.1
    Publisher: American Meteorological Society
    Abstract: The linear dynamics of symmetric and nonsymmetric perturbations in unbounded zonal inviscid flows with a constant vertical shear of velocity, when a fluid is incompressible and density is stably stratified along the vertical and meridional directions, is investigated. A small?Richardson number Ri ? 1 and large?Rossby number Ro ? 1 regime is considered, which satisfies the condition for symmetric instability. Specific features of this dynamics are closely related to the nonnormality of linear operators in shear flows and are well interpreted in the framework of the nonmodal approach by tracing the linear dynamics of spatial Fourier harmonics (Kelvin modes) of perturbations in time. The roles of stable stratification, the Coriolis parameter, and vertical shear in the dynamics of perturbations are analyzed. Classification of perturbations into two types or modes?vortex (i.e., quasigeostrophic balanced motions) and inertia?gravity wave?is made according to the value of potential vorticity. The emerging picture of the (linear) transient dynamics for these two modes at Ri ? 1 and Ro ? 1 indicates that vortex mode perturbations are able to gain basic flow energy and undergo exponential transient amplification and in this process generate inertia?gravity waves. Transient growth of the vortex mode and, consequently, the effectiveness of the wave generation both increase with decreasing Ri and increasing Ro. This linear coupling of perturbation modes is, in general, specific to shear flows but is not fully appreciated yet. A parallel analysis of the transient dynamics of nonsymmetric perturbations versus symmetric instability is also presented. It is shown that the nonnormality-induced transient growth of nonsymmetric perturbations can prevail over the symmetric instability for a wide range of Ri and Ro. The current analysis suggests that the dynamical activity of fronts and jet streaks at Ri ? 1 and Ro ? 1 should be determined by nonsymmetric perturbations rather than by symmetric ones, as was accepted in earlier papers. It is noteworthy that the transient growth of perturbations is asymmetric in the wavenumber space?the constant phase plane of maximally amplified perturbations is inclined in a direction northeast to the zonal one and the inclination angle is different for different Ri and Ro.
    • Download: (1016.Kb)
    • Show Full MetaData Hide Full MetaData
    • Item Order
    • Go To Publisher
    • Statistics

      Transient Dynamics of Nonsymmetric Perturbations versus Symmetric Instability in Baroclinic Zonal Shear Flows

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/4211922
    Collections
    • Journal of the Atmospheric Sciences

    Show full item record

    contributor authorMamatsashvili, G. R.
    contributor authorAvsarkisov, V. S.
    contributor authorChagelishvili, G. D.
    contributor authorChanishvili, R. G.
    contributor authorKalashnik, M. V.
    date accessioned2017-06-09T16:34:14Z
    date available2017-06-09T16:34:14Z
    date copyright2010/09/01
    date issued2010
    identifier issn0022-4928
    identifier otherams-70171.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4211922
    description abstractThe linear dynamics of symmetric and nonsymmetric perturbations in unbounded zonal inviscid flows with a constant vertical shear of velocity, when a fluid is incompressible and density is stably stratified along the vertical and meridional directions, is investigated. A small?Richardson number Ri ? 1 and large?Rossby number Ro ? 1 regime is considered, which satisfies the condition for symmetric instability. Specific features of this dynamics are closely related to the nonnormality of linear operators in shear flows and are well interpreted in the framework of the nonmodal approach by tracing the linear dynamics of spatial Fourier harmonics (Kelvin modes) of perturbations in time. The roles of stable stratification, the Coriolis parameter, and vertical shear in the dynamics of perturbations are analyzed. Classification of perturbations into two types or modes?vortex (i.e., quasigeostrophic balanced motions) and inertia?gravity wave?is made according to the value of potential vorticity. The emerging picture of the (linear) transient dynamics for these two modes at Ri ? 1 and Ro ? 1 indicates that vortex mode perturbations are able to gain basic flow energy and undergo exponential transient amplification and in this process generate inertia?gravity waves. Transient growth of the vortex mode and, consequently, the effectiveness of the wave generation both increase with decreasing Ri and increasing Ro. This linear coupling of perturbation modes is, in general, specific to shear flows but is not fully appreciated yet. A parallel analysis of the transient dynamics of nonsymmetric perturbations versus symmetric instability is also presented. It is shown that the nonnormality-induced transient growth of nonsymmetric perturbations can prevail over the symmetric instability for a wide range of Ri and Ro. The current analysis suggests that the dynamical activity of fronts and jet streaks at Ri ? 1 and Ro ? 1 should be determined by nonsymmetric perturbations rather than by symmetric ones, as was accepted in earlier papers. It is noteworthy that the transient growth of perturbations is asymmetric in the wavenumber space?the constant phase plane of maximally amplified perturbations is inclined in a direction northeast to the zonal one and the inclination angle is different for different Ri and Ro.
    publisherAmerican Meteorological Society
    titleTransient Dynamics of Nonsymmetric Perturbations versus Symmetric Instability in Baroclinic Zonal Shear Flows
    typeJournal Paper
    journal volume67
    journal issue9
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/2010JAS3313.1
    journal fristpage2972
    journal lastpage2989
    treeJournal of the Atmospheric Sciences:;2010:;Volume( 067 ):;issue: 009
    contenttypeFulltext
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian
     
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian