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    The Field Distributions and Balances in a Baroclinic Annulus Wave

    Source: Monthly Weather Review:;1972:;volume( 100 ):;issue: 001::page 29
    Author:
    WILLIAMS, GARETH P.
    DOI: 10.1175/1520-0493(1972)100<0029:TFDABI>2.3.CO;2
    Publisher: American Meteorological Society
    Abstract: The detailed structure of a steady wave occurring in a rotating annulus of square cross-section and having a free surface is presented. The field distributions are obtained by numerical integration of the three-dimensional nonlinear Navier-Stokes equations. The distributions of pressure, temperature, and the three velocity components are displayed for the total fields and for the fields of deviation from the zonal means. Their dynamical balances are also discussed. The deviation wave is a type of Eady wave and the solution is used to discuss the structure of such waves in finite amplitude steady-state form under the influence of variations in baroclinicity, shear, and boundary layers. The side layers make little contribution to the characteristics of the wave in the deviation field although significant Ekman layer features do appear. The flow is essentially in hydrostatic and geostrophic balance except in the boundary layers. Heat conduction is important only in the side layers.
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      The Field Distributions and Balances in a Baroclinic Annulus Wave

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/4198838
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    • Monthly Weather Review

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    contributor authorWILLIAMS, GARETH P.
    date accessioned2017-06-09T15:59:50Z
    date available2017-06-09T15:59:50Z
    date copyright1972/01/01
    date issued1972
    identifier issn0027-0644
    identifier otherams-58396.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4198838
    description abstractThe detailed structure of a steady wave occurring in a rotating annulus of square cross-section and having a free surface is presented. The field distributions are obtained by numerical integration of the three-dimensional nonlinear Navier-Stokes equations. The distributions of pressure, temperature, and the three velocity components are displayed for the total fields and for the fields of deviation from the zonal means. Their dynamical balances are also discussed. The deviation wave is a type of Eady wave and the solution is used to discuss the structure of such waves in finite amplitude steady-state form under the influence of variations in baroclinicity, shear, and boundary layers. The side layers make little contribution to the characteristics of the wave in the deviation field although significant Ekman layer features do appear. The flow is essentially in hydrostatic and geostrophic balance except in the boundary layers. Heat conduction is important only in the side layers.
    publisherAmerican Meteorological Society
    titleThe Field Distributions and Balances in a Baroclinic Annulus Wave
    typeJournal Paper
    journal volume100
    journal issue1
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1972)100<0029:TFDABI>2.3.CO;2
    journal fristpage29
    journal lastpage41
    treeMonthly Weather Review:;1972:;volume( 100 ):;issue: 001
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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