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    A Theoretical Study of the Flow of Air and Fallout of Solid Precipitation Over Mountainous Terrain: Part I. Airflow Model

    Source: Journal of the Atmospheric Sciences:;1973:;Volume( 030 ):;issue: 005::page 801
    Author:
    Fraser, Alistair B.
    ,
    Easter, Richard C.
    ,
    Hobbs, Peter V.
    DOI: 10.1175/1520-0469(1973)030<0801:ATSOTF>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A model for airflow over mountainous terrain is presented. The equations for steady, two-dimensional, laminar inviscid flow, including pseudo-adiabatic latent heat release, are derived. Approximate solutions to the linearized equations are obtained for stably stratified conditions, and a terrain consisting of broad ridges (width?25 km), through an iterative transform technique which allows the nonlinear boundary conditions to be satisfied. The model indicates that the dynamical effects of latent heat are significant in some cases but are generally secondary to the barrier effect of the terrain.
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      A Theoretical Study of the Flow of Air and Fallout of Solid Precipitation Over Mountainous Terrain: Part I. Airflow Model

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4152168
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    • Journal of the Atmospheric Sciences

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    contributor authorFraser, Alistair B.
    contributor authorEaster, Richard C.
    contributor authorHobbs, Peter V.
    date accessioned2017-06-09T14:16:59Z
    date available2017-06-09T14:16:59Z
    date copyright1973/07/01
    date issued1973
    identifier issn0022-4928
    identifier otherams-16390.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152168
    description abstractA model for airflow over mountainous terrain is presented. The equations for steady, two-dimensional, laminar inviscid flow, including pseudo-adiabatic latent heat release, are derived. Approximate solutions to the linearized equations are obtained for stably stratified conditions, and a terrain consisting of broad ridges (width?25 km), through an iterative transform technique which allows the nonlinear boundary conditions to be satisfied. The model indicates that the dynamical effects of latent heat are significant in some cases but are generally secondary to the barrier effect of the terrain.
    publisherAmerican Meteorological Society
    titleA Theoretical Study of the Flow of Air and Fallout of Solid Precipitation Over Mountainous Terrain: Part I. Airflow Model
    typeJournal Paper
    journal volume30
    journal issue5
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1973)030<0801:ATSOTF>2.0.CO;2
    journal fristpage801
    journal lastpage812
    treeJournal of the Atmospheric Sciences:;1973:;Volume( 030 ):;issue: 005
    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