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    EXACT PARTICLE TRAJECTORIES FOR NONVISCOUS FLOW IN A PLANE WITH A CONSTANT CORIOLIS PARAMETER

    Source: Journal of Meteorology:;1949:;volume( 006 ):;issue: 005::page 337
    Author:
    Forsythe, George E.
    DOI: 10.1175/1520-0469(1949)006<0337:EPTFNF>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The pressure and density fields are assumed known exactly for all time, and the wind is to be forecast by obtaining the trajectory of each air particle from the equations of nonviscous motion in a plane. The importance of initial conditions is stressed. For sufficiently simple pressure and density fields the particle trajectories and hodographs may be obtained explicitly without approximation. The appropriate mathematical methods are reviewed. When the pressure force depends only on time, the solutions are compared with the Brunt?Douglas ?isallobaric-wind? formula. For one case of stationary circular isobars the exact solution is shown to consist of a superposition of so-called ?normal? and ?abnormal? solutions of the gradient wind equation. Explicit trajectories believed to be new are found for an air parcel in a certain high-pressure center whose horizontal pressure gradient is equal to or greater than that of the so-called maximum anticyclone. The general nonlinear case of circular isobars is discussed. Several numerical examples are included.
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      EXACT PARTICLE TRAJECTORIES FOR NONVISCOUS FLOW IN A PLANE WITH A CONSTANT CORIOLIS PARAMETER

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/4149188
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    • Journal of Meteorology

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    contributor authorForsythe, George E.
    date accessioned2017-06-09T14:10:05Z
    date available2017-06-09T14:10:05Z
    date copyright1949/10/01
    date issued1949
    identifier issn0095-9634
    identifier otherams-13708.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149188
    description abstractThe pressure and density fields are assumed known exactly for all time, and the wind is to be forecast by obtaining the trajectory of each air particle from the equations of nonviscous motion in a plane. The importance of initial conditions is stressed. For sufficiently simple pressure and density fields the particle trajectories and hodographs may be obtained explicitly without approximation. The appropriate mathematical methods are reviewed. When the pressure force depends only on time, the solutions are compared with the Brunt?Douglas ?isallobaric-wind? formula. For one case of stationary circular isobars the exact solution is shown to consist of a superposition of so-called ?normal? and ?abnormal? solutions of the gradient wind equation. Explicit trajectories believed to be new are found for an air parcel in a certain high-pressure center whose horizontal pressure gradient is equal to or greater than that of the so-called maximum anticyclone. The general nonlinear case of circular isobars is discussed. Several numerical examples are included.
    publisherAmerican Meteorological Society
    titleEXACT PARTICLE TRAJECTORIES FOR NONVISCOUS FLOW IN A PLANE WITH A CONSTANT CORIOLIS PARAMETER
    typeJournal Paper
    journal volume6
    journal issue5
    journal titleJournal of Meteorology
    identifier doi10.1175/1520-0469(1949)006<0337:EPTFNF>2.0.CO;2
    journal fristpage337
    journal lastpage346
    treeJournal of Meteorology:;1949:;volume( 006 ):;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