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    Local Energy Generation in Barotropic Flows

    Source: Journal of the Atmospheric Sciences:;2002:;Volume( 059 ):;issue: 013::page 2153
    Author:
    Iacono, R.
    DOI: 10.1175/1520-0469(2002)059<2153:LEGIBF>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The local growth of disturbances to a steady, nondivergent shear flow is investigated in the context of the barotropic vorticity equation (BVE). A new expression for the instantaneous energy generation rate is derived by using a local coordinate frame defined by the directions parallel and perpendicular to the basic flow. The equilibrium information enters this expression through two scalar coefficients, which can be interpreted as local components of an ?effective shear? vector S (S coincides with the shear vector for irrotational flows). A simple picture of local instability results: the magnitude of S gives the maximum possible energy growth rate for localized unstable disturbances, while its orientation determines the direction of maximum energy growth, which is given by the perpendicular to the bisector of the angle between S and the equilibrium velocity. This allows extension of the familiar ?leaning against the shear? instability picture, developed for zonal currents, to generic, two-dimensional (2D), steady-state solutions of the BVE. Applications of the new approach to some simple basic flows of interest for atmospheric dynamics are discussed.
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      Local Energy Generation in Barotropic Flows

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4159671
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    contributor authorIacono, R.
    date accessioned2017-06-09T14:37:46Z
    date available2017-06-09T14:37:46Z
    date copyright2002/07/01
    date issued2002
    identifier issn0022-4928
    identifier otherams-23142.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4159671
    description abstractThe local growth of disturbances to a steady, nondivergent shear flow is investigated in the context of the barotropic vorticity equation (BVE). A new expression for the instantaneous energy generation rate is derived by using a local coordinate frame defined by the directions parallel and perpendicular to the basic flow. The equilibrium information enters this expression through two scalar coefficients, which can be interpreted as local components of an ?effective shear? vector S (S coincides with the shear vector for irrotational flows). A simple picture of local instability results: the magnitude of S gives the maximum possible energy growth rate for localized unstable disturbances, while its orientation determines the direction of maximum energy growth, which is given by the perpendicular to the bisector of the angle between S and the equilibrium velocity. This allows extension of the familiar ?leaning against the shear? instability picture, developed for zonal currents, to generic, two-dimensional (2D), steady-state solutions of the BVE. Applications of the new approach to some simple basic flows of interest for atmospheric dynamics are discussed.
    publisherAmerican Meteorological Society
    titleLocal Energy Generation in Barotropic Flows
    typeJournal Paper
    journal volume59
    journal issue13
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(2002)059<2153:LEGIBF>2.0.CO;2
    journal fristpage2153
    journal lastpage2163
    treeJournal of the Atmospheric Sciences:;2002:;Volume( 059 ):;issue: 013
    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