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    Leading Lyapunov Vectors of a Turbulent Baroclinic Jet in a Quasigeostrophic Model

    Source: Journal of the Atmospheric Sciences:;2003:;Volume( 060 ):;issue: 004::page 683
    Author:
    Snyder, Chris
    ,
    Hamill, Thomas M.
    DOI: 10.1175/1520-0469(2003)060<0683:LLVOAT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Leading Lyapunov exponents and vectors are calculated for a turbulent baroclinic jet in a quasigeostrophic model with O(105) degrees of freedom. The leading exponent is close to 0.4 day?1, and the unstable subspace has dimension between 30 and 40. The leading Lyapunov vectors exhibit a strong correlation of their potential vorticity (PV) with the PV gradients of the unperturbed flow. These perturbations do not, however, appear to be instabilities of smaller scale on the turbulent flow. Instead, they share the scales of the flow itself (at least if measured along PV contours) and often simply represent local phase shifts or displacements of existing features in the flow. Singular vectors constrained to the subspace of Lyapunov vectors are also calculated. Maximum amplification factors over 2 days are, on average, about 6, 7.5, and 9 (compared to the factor of 2 implied by the leading exponent) for subspaces of the leading 20, 35, and 60 Lyapunov vectors, respectively.
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      Leading Lyapunov Vectors of a Turbulent Baroclinic Jet in a Quasigeostrophic Model

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4159820
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    • Journal of the Atmospheric Sciences

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    contributor authorSnyder, Chris
    contributor authorHamill, Thomas M.
    date accessioned2017-06-09T14:38:11Z
    date available2017-06-09T14:38:11Z
    date copyright2003/02/01
    date issued2003
    identifier issn0022-4928
    identifier otherams-23277.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4159820
    description abstractLeading Lyapunov exponents and vectors are calculated for a turbulent baroclinic jet in a quasigeostrophic model with O(105) degrees of freedom. The leading exponent is close to 0.4 day?1, and the unstable subspace has dimension between 30 and 40. The leading Lyapunov vectors exhibit a strong correlation of their potential vorticity (PV) with the PV gradients of the unperturbed flow. These perturbations do not, however, appear to be instabilities of smaller scale on the turbulent flow. Instead, they share the scales of the flow itself (at least if measured along PV contours) and often simply represent local phase shifts or displacements of existing features in the flow. Singular vectors constrained to the subspace of Lyapunov vectors are also calculated. Maximum amplification factors over 2 days are, on average, about 6, 7.5, and 9 (compared to the factor of 2 implied by the leading exponent) for subspaces of the leading 20, 35, and 60 Lyapunov vectors, respectively.
    publisherAmerican Meteorological Society
    titleLeading Lyapunov Vectors of a Turbulent Baroclinic Jet in a Quasigeostrophic Model
    typeJournal Paper
    journal volume60
    journal issue4
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(2003)060<0683:LLVOAT>2.0.CO;2
    journal fristpage683
    journal lastpage688
    treeJournal of the Atmospheric Sciences:;2003:;Volume( 060 ):;issue: 004
    contenttypeFulltext
    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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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian