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    Nonlinear Waves and Coherent Vortex Structures in Barotropic β-plane Jets

    Source: Journal of Physical Oceanography:;1987:;Volume( 017 ):;issue: 009::page 1408
    Author:
    Flierl, G. R.
    ,
    Malanotte-Rizzoli, P.
    ,
    Zabusky, N. J.
    DOI: 10.1175/1520-0485(1987)017<1408:NWACVS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: We examine the nonlinear evolution of barotropic ?-plane jets on a periodic domain with a pseudospectral. A calculation of the linear growth rate yields an infected U-shaped curve on the ? versus k0 plane which separates regions of stability and instability. This curve aids in clarifying the morphology of the nonlinear structures which evolve from monochromatic small-amplitude perturbations of wavenumber k0. At very small or zero ?, we recover and further quantify previously obtained results, including formation of: dipolar vortex structures or bound pools of opposite-signed vortex regions at small k0; staggered streets isolated vortex pools at intermediate k0; and ?cat-eyes? or staggered connected pools of vorticity at large but still unstable k0. As ? is increased, the jet exhibits quite different evolutionary patterns. At low k0, where the laminar jet may be stable, we find a multistage instability. First, neutrally stable long-wavelength modes of small amplitude interact nonlinearly to produce harmonics in the linear unstable band. These grow at an exponential rate until a near-steady wake appears. However, the wake is unstable to the initial long wavelength modes and a rapid merger (i.e., backward energy cascade) occurs. At an intermediate k0, the presence of ? causes a ?reversal? of vortex pools in the meridional direction of the near-steady vortex street. That is for a west-to-east flowing jet the Positive pools of vorticity are south of the negative pools causing a decrease in the near-steady velocity of the jet. Retrograde Rossby radiation is observed and weak ?shingles? or cast-away vortex pools are observed. The meander amplitude pulsates, pumping Rossby radiation into the far field. The merger and binding processes also occur on a jet excited by many harmonics, with an ensuing chaos that is very sensitive to initial conditions.
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      Nonlinear Waves and Coherent Vortex Structures in Barotropic β-plane Jets

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    contributor authorFlierl, G. R.
    contributor authorMalanotte-Rizzoli, P.
    contributor authorZabusky, N. J.
    date accessioned2017-06-09T14:48:32Z
    date available2017-06-09T14:48:32Z
    date copyright1987/09/01
    date issued1987
    identifier issn0022-3670
    identifier otherams-27231.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4164214
    description abstractWe examine the nonlinear evolution of barotropic ?-plane jets on a periodic domain with a pseudospectral. A calculation of the linear growth rate yields an infected U-shaped curve on the ? versus k0 plane which separates regions of stability and instability. This curve aids in clarifying the morphology of the nonlinear structures which evolve from monochromatic small-amplitude perturbations of wavenumber k0. At very small or zero ?, we recover and further quantify previously obtained results, including formation of: dipolar vortex structures or bound pools of opposite-signed vortex regions at small k0; staggered streets isolated vortex pools at intermediate k0; and ?cat-eyes? or staggered connected pools of vorticity at large but still unstable k0. As ? is increased, the jet exhibits quite different evolutionary patterns. At low k0, where the laminar jet may be stable, we find a multistage instability. First, neutrally stable long-wavelength modes of small amplitude interact nonlinearly to produce harmonics in the linear unstable band. These grow at an exponential rate until a near-steady wake appears. However, the wake is unstable to the initial long wavelength modes and a rapid merger (i.e., backward energy cascade) occurs. At an intermediate k0, the presence of ? causes a ?reversal? of vortex pools in the meridional direction of the near-steady vortex street. That is for a west-to-east flowing jet the Positive pools of vorticity are south of the negative pools causing a decrease in the near-steady velocity of the jet. Retrograde Rossby radiation is observed and weak ?shingles? or cast-away vortex pools are observed. The meander amplitude pulsates, pumping Rossby radiation into the far field. The merger and binding processes also occur on a jet excited by many harmonics, with an ensuing chaos that is very sensitive to initial conditions.
    publisherAmerican Meteorological Society
    titleNonlinear Waves and Coherent Vortex Structures in Barotropic β-plane Jets
    typeJournal Paper
    journal volume17
    journal issue9
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1987)017<1408:NWACVS>2.0.CO;2
    journal fristpage1408
    journal lastpage1438
    treeJournal of Physical Oceanography:;1987:;Volume( 017 ):;issue: 009
    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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