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    The Level of No Motion in an Ideal Fluid

    Source: Journal of Physical Oceanography:;1984:;Volume( 014 ):;issue: 001::page 203
    Author:
    Olbers, D. J.
    ,
    Willebrand, J.
    DOI: 10.1175/1520-0485(1984)014<0203:TLONMI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The level of no motion plays a central role in the classical dynamic method and the more advanced diagnostic schemes of the ?-spiral (e.g., Stommel and Schott) and inverse method (Wunsch) to calculate the absolute velocity in the ocean. Following simple arguments, each velocity component should vanish on separate surfaces in the fluid and the absolute velocity vector vanishes on the intersection of these surfaces, i.e., on curves in the fluid. It has been suggested, however, that besides these simple configurations there may be surfaces in the fluid on which the velocity vector vanishes. Killworth has been a diagnostic scheme on this concept which is different from the ?-spiral approach and the inverse method. In this note we examine the possible configuration of the level of no-motion in a fluid using ideal fluid theory. It is shown that stagnation surfaces in the fluid, i.e. surfaces on which the velocity vector vanishes, normally do not exist.
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      The Level of No Motion in an Ideal Fluid

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    contributor authorOlbers, D. J.
    contributor authorWillebrand, J.
    date accessioned2017-06-09T14:46:57Z
    date available2017-06-09T14:46:57Z
    date copyright1984/01/01
    date issued1984
    identifier issn0022-3670
    identifier otherams-26642.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4163559
    description abstractThe level of no motion plays a central role in the classical dynamic method and the more advanced diagnostic schemes of the ?-spiral (e.g., Stommel and Schott) and inverse method (Wunsch) to calculate the absolute velocity in the ocean. Following simple arguments, each velocity component should vanish on separate surfaces in the fluid and the absolute velocity vector vanishes on the intersection of these surfaces, i.e., on curves in the fluid. It has been suggested, however, that besides these simple configurations there may be surfaces in the fluid on which the velocity vector vanishes. Killworth has been a diagnostic scheme on this concept which is different from the ?-spiral approach and the inverse method. In this note we examine the possible configuration of the level of no-motion in a fluid using ideal fluid theory. It is shown that stagnation surfaces in the fluid, i.e. surfaces on which the velocity vector vanishes, normally do not exist.
    publisherAmerican Meteorological Society
    titleThe Level of No Motion in an Ideal Fluid
    typeJournal Paper
    journal volume14
    journal issue1
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1984)014<0203:TLONMI>2.0.CO;2
    journal fristpage203
    journal lastpage212
    treeJournal of Physical Oceanography:;1984:;Volume( 014 ):;issue: 001
    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