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    Meridional Flow Field of Axisymmetric Flows in a Rotating Annulus

    Source: Journal of the Atmospheric Sciences:;2000:;Volume( 057 ):;issue: 018::page 3109
    Author:
    Tajima, T.
    ,
    Nakamura, T.
    DOI: 10.1175/1520-0469(2000)057<3109:MFFOAF>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Measurements of the flow field were made of the axisymmetric flow in a differentially heated rotating fluid annulus by using a long-term tracking of a tracer particle. Its meridional flow profile is composed of a flow circulating in a large direct (Hadley) cell, which consists of thin boundary and top horizontal layers, and another one in the interior of that cell. Our measurements show that little mixing of the flow between the Hadley cell and the interior occurs and two secondary cells exist in the interior. These cells cause a trajectory of the tracer particle to be chaotic, where the particle follows the main cyclic route but is occasionally trapped in the secondary cells for indefinite times. Very close to the transition to the wave regime, a mixed structure appears consisting of both the axisymmetric and the wave flows in the meridional flow field: an unsteady wave flow occurs in the interior of the Hadley cell.
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      Meridional Flow Field of Axisymmetric Flows in a Rotating Annulus

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4159183
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    contributor authorTajima, T.
    contributor authorNakamura, T.
    date accessioned2017-06-09T14:36:31Z
    date available2017-06-09T14:36:31Z
    date copyright2000/09/01
    date issued2000
    identifier issn0022-4928
    identifier otherams-22703.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4159183
    description abstractMeasurements of the flow field were made of the axisymmetric flow in a differentially heated rotating fluid annulus by using a long-term tracking of a tracer particle. Its meridional flow profile is composed of a flow circulating in a large direct (Hadley) cell, which consists of thin boundary and top horizontal layers, and another one in the interior of that cell. Our measurements show that little mixing of the flow between the Hadley cell and the interior occurs and two secondary cells exist in the interior. These cells cause a trajectory of the tracer particle to be chaotic, where the particle follows the main cyclic route but is occasionally trapped in the secondary cells for indefinite times. Very close to the transition to the wave regime, a mixed structure appears consisting of both the axisymmetric and the wave flows in the meridional flow field: an unsteady wave flow occurs in the interior of the Hadley cell.
    publisherAmerican Meteorological Society
    titleMeridional Flow Field of Axisymmetric Flows in a Rotating Annulus
    typeJournal Paper
    journal volume57
    journal issue18
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(2000)057<3109:MFFOAF>2.0.CO;2
    journal fristpage3109
    journal lastpage3121
    treeJournal of the Atmospheric Sciences:;2000:;Volume( 057 ):;issue: 018
    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