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    A Three-Dimensional Study of Frontogenesis Using a Model Formulated in Stream-Axis Coordinates

    Source: Journal of the Atmospheric Sciences:;1977:;Volume( 034 ):;issue: 006::page 873
    Author:
    Price, G. V.
    DOI: 10.1175/1520-0469(1977)034<0873:ATDSOF>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A jet-based model is proposed to study the dynamics of frontal zone-jet stream systems. The model is developed in non-orthogonal stream-axis coordinates with a condition of gradient flow in the direction of the jet (no assumption is made on the flow in the cross-jet direction). Approximating functions are used to represent the spatial dependence of the variables, and the forecast is advanced using a Galerkin technique with an Euler-backward time extrapolation scheme. Three-dimensional forecast experiments are performed using a baroclinic zonal jet with a superimposed perturbation of the type studied numerically by Mudrick (1974). The model forecast develops surface and mid-tropospheric frontal zones which compare well with the results obtained by Madrick. The forecast frontogenesis mechanisms and circulation patterns are determined, and effects due to the trajectory curvature calculation and the resolution of the approximating functions are considered.
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      A Three-Dimensional Study of Frontogenesis Using a Model Formulated in Stream-Axis Coordinates

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4153176
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    contributor authorPrice, G. V.
    date accessioned2017-06-09T14:19:32Z
    date available2017-06-09T14:19:32Z
    date copyright1977/06/01
    date issued1977
    identifier issn0022-4928
    identifier otherams-17298.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153176
    description abstractA jet-based model is proposed to study the dynamics of frontal zone-jet stream systems. The model is developed in non-orthogonal stream-axis coordinates with a condition of gradient flow in the direction of the jet (no assumption is made on the flow in the cross-jet direction). Approximating functions are used to represent the spatial dependence of the variables, and the forecast is advanced using a Galerkin technique with an Euler-backward time extrapolation scheme. Three-dimensional forecast experiments are performed using a baroclinic zonal jet with a superimposed perturbation of the type studied numerically by Mudrick (1974). The model forecast develops surface and mid-tropospheric frontal zones which compare well with the results obtained by Madrick. The forecast frontogenesis mechanisms and circulation patterns are determined, and effects due to the trajectory curvature calculation and the resolution of the approximating functions are considered.
    publisherAmerican Meteorological Society
    titleA Three-Dimensional Study of Frontogenesis Using a Model Formulated in Stream-Axis Coordinates
    typeJournal Paper
    journal volume34
    journal issue6
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1977)034<0873:ATDSOF>2.0.CO;2
    journal fristpage873
    journal lastpage890
    treeJournal of the Atmospheric Sciences:;1977:;Volume( 034 ):;issue: 006
    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