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    A Generalization of Bernoulli's Theorem

    Source: Journal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 010::page 1437
    Author:
    Schär, Christoph
    DOI: 10.1175/1520-0469(1993)050<1437:AGOBT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The conservation of potential vorticity Q can be expressed as ?(?Q/?t + ?·J = 0, where J denotes the total flux of potential vorticity. It is shown that J is related under statistically steady conditions to the Bernoulli function B by J = ?? ? ?B,where ? is the potential temperature. This relation is valid even in the nonhydrostatic limit and in the presence of arbitrary nonconservative forces (such as internal friction) and heating rates. In essence, it can be interpreted as a generalization of Bernoulli's theorem to the frictional and diabatic regime. The classical Bernoulli theorem?valid for inviscid adiabatic and steady flows?states that the intersections of surfaces of constant potential temperature and constant Bernoulli function yield streamlines. In the presence of frictional and diabatic effects, these intersections yield the flux lines along which potential vorticity is transported.
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      A Generalization of Bernoulli's Theorem

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4157197
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    contributor authorSchär, Christoph
    date accessioned2017-06-09T14:31:27Z
    date available2017-06-09T14:31:27Z
    date copyright1993/05/01
    date issued1993
    identifier issn0022-4928
    identifier otherams-20916.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4157197
    description abstractThe conservation of potential vorticity Q can be expressed as ?(?Q/?t + ?·J = 0, where J denotes the total flux of potential vorticity. It is shown that J is related under statistically steady conditions to the Bernoulli function B by J = ?? ? ?B,where ? is the potential temperature. This relation is valid even in the nonhydrostatic limit and in the presence of arbitrary nonconservative forces (such as internal friction) and heating rates. In essence, it can be interpreted as a generalization of Bernoulli's theorem to the frictional and diabatic regime. The classical Bernoulli theorem?valid for inviscid adiabatic and steady flows?states that the intersections of surfaces of constant potential temperature and constant Bernoulli function yield streamlines. In the presence of frictional and diabatic effects, these intersections yield the flux lines along which potential vorticity is transported.
    publisherAmerican Meteorological Society
    titleA Generalization of Bernoulli's Theorem
    typeJournal Paper
    journal volume50
    journal issue10
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1993)050<1437:AGOBT>2.0.CO;2
    journal fristpage1437
    journal lastpage1443
    treeJournal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 010
    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