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    A Geometric Model of the Nonlinear Equilibration of Two-Dimensional Eady Waves

    Source: Journal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 002::page 328
    Author:
    Cullen, M. J. P.
    ,
    Roulstone, I.
    DOI: 10.1175/1520-0469(1993)050<0328:AGMOTN>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The initial-value problem for Eady's model is reexamined using a two-dimensional (x, z) Lagrangian semigeostrophic model. A basic-flow state in a periodic domain with a perturbation field imposed is represented by piecewise constant data. The Lagrangian conservation laws governing the motion allow the construction of a solution that describes the evolution of the unstable wave as it passes through the point of frontal collapse, reaches a maximum amplitude, and then decays. The integration is continued and a second cycle is observed. A similar experiment was performed by Nakamura and Held, using a primitive equation model with diffusion. Two integrations are carried out to investigate the sensitivity of the solution to the representation of the data by piecewise constant values and present observations and comparisons between these results and those of Nakamura and Held.
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      A Geometric Model of the Nonlinear Equilibration of Two-Dimensional Eady Waves

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4157115
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    contributor authorCullen, M. J. P.
    contributor authorRoulstone, I.
    date accessioned2017-06-09T14:31:15Z
    date available2017-06-09T14:31:15Z
    date copyright1993/01/01
    date issued1993
    identifier issn0022-4928
    identifier otherams-20842.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4157115
    description abstractThe initial-value problem for Eady's model is reexamined using a two-dimensional (x, z) Lagrangian semigeostrophic model. A basic-flow state in a periodic domain with a perturbation field imposed is represented by piecewise constant data. The Lagrangian conservation laws governing the motion allow the construction of a solution that describes the evolution of the unstable wave as it passes through the point of frontal collapse, reaches a maximum amplitude, and then decays. The integration is continued and a second cycle is observed. A similar experiment was performed by Nakamura and Held, using a primitive equation model with diffusion. Two integrations are carried out to investigate the sensitivity of the solution to the representation of the data by piecewise constant values and present observations and comparisons between these results and those of Nakamura and Held.
    publisherAmerican Meteorological Society
    titleA Geometric Model of the Nonlinear Equilibration of Two-Dimensional Eady Waves
    typeJournal Paper
    journal volume50
    journal issue2
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1993)050<0328:AGMOTN>2.0.CO;2
    journal fristpage328
    journal lastpage332
    treeJournal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 002
    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