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    Periodic Orbits and Disturbance Growth for Baroclinic Waves

    Source: Journal of the Atmospheric Sciences:;2001:;Volume( 058 ):;issue: 005::page 436
    Author:
    Samelson, R. M.
    DOI: 10.1175/1520-0469(2001)058<0436:POADGF>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The growth of linear disturbances to stable and unstable time-periodic basic states is analyzed in an asymptotic model of weakly nonlinear, baroclinic wave?mean interaction. In this model, an ordinary differential equation for the wave amplitude is coupled to a partial differential equation for the zonal-flow correction. Floquet vectors, the eigenmodes for linear disturbances to the oscillatory basic states, split into wave-dynamical and decaying zonal-flow modes. Singular vectors reflect the structure of the Floquet vectors: the most rapid amplification and decay are associated with the wave-dynamical Floquet vectors, while the intermediate singular vectors closely follow the decaying zonal-flow Floquet vectors. Singular values depend strongly on initial and optimization times. For initial times near wave amplitude maxima, the Floquet decomposition of the leading singular vector depends relatively weakly on optimization time. For the unstable oscillatory basic state in the chaotic regime, the leading Floquet vector is tangent to the large-scale structure of the attractor, while the leading singular vector is not. However, corresponding inferences about the accessibility of disturbed states rely on the simple attractor geometry, and may not easily generalize. The primary mechanism of disturbance growth on the wave timescale in this model involves a time-dependent phase shift along the basic wave cycle. The Floquet vectors illustrate that modal disturbances to time-dependent basic states can have time-dependent spatial structure, and that the latter need not indicate nonmodal dynamics. The dynamical splitting reduces the ?butterfly effect,? the ability of small-scale disturbances to influence the evolution of an unstable large-scale flow.
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      Periodic Orbits and Disturbance Growth for Baroclinic Waves

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4159270
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    contributor authorSamelson, R. M.
    date accessioned2017-06-09T14:36:43Z
    date available2017-06-09T14:36:43Z
    date copyright2001/03/01
    date issued2001
    identifier issn0022-4928
    identifier otherams-22782.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4159270
    description abstractThe growth of linear disturbances to stable and unstable time-periodic basic states is analyzed in an asymptotic model of weakly nonlinear, baroclinic wave?mean interaction. In this model, an ordinary differential equation for the wave amplitude is coupled to a partial differential equation for the zonal-flow correction. Floquet vectors, the eigenmodes for linear disturbances to the oscillatory basic states, split into wave-dynamical and decaying zonal-flow modes. Singular vectors reflect the structure of the Floquet vectors: the most rapid amplification and decay are associated with the wave-dynamical Floquet vectors, while the intermediate singular vectors closely follow the decaying zonal-flow Floquet vectors. Singular values depend strongly on initial and optimization times. For initial times near wave amplitude maxima, the Floquet decomposition of the leading singular vector depends relatively weakly on optimization time. For the unstable oscillatory basic state in the chaotic regime, the leading Floquet vector is tangent to the large-scale structure of the attractor, while the leading singular vector is not. However, corresponding inferences about the accessibility of disturbed states rely on the simple attractor geometry, and may not easily generalize. The primary mechanism of disturbance growth on the wave timescale in this model involves a time-dependent phase shift along the basic wave cycle. The Floquet vectors illustrate that modal disturbances to time-dependent basic states can have time-dependent spatial structure, and that the latter need not indicate nonmodal dynamics. The dynamical splitting reduces the ?butterfly effect,? the ability of small-scale disturbances to influence the evolution of an unstable large-scale flow.
    publisherAmerican Meteorological Society
    titlePeriodic Orbits and Disturbance Growth for Baroclinic Waves
    typeJournal Paper
    journal volume58
    journal issue5
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(2001)058<0436:POADGF>2.0.CO;2
    journal fristpage436
    journal lastpage450
    treeJournal of the Atmospheric Sciences:;2001:;Volume( 058 ):;issue: 005
    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