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    THE THEORY OF LOCAL ADVECTION: I

    Source: Journal of Meteorology:;1959:;volume( 016 ):;issue: 005::page 535
    Author:
    Philip, J. R.
    DOI: 10.1175/1520-0469(1959)016<0535:TTOLAI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: This paper is the first of a series in which the theory of local advection (the exchange due to horizontal heterogeneity) of energy and moisture will be developed and applied to a number of problems of practical and theoretical interest. The paper provides an introduction to the practical implications and physical basis of local advection, but it is mainly devoted to developing methods of analysis to be applied in later papers. The treatment aims to provide simple and rapid numerical procedures for the solution of advection problems. Methods are given for solving the two-dimensional atmospheric-diffusion equation subject to ?concentration,? ?flux,? and ?radiation? types of boundary conditions. Appendices give discussions of the properties of the functions entering the solutions and provide simple means for their computation. Extensive tables of the relevant functions are given for the case m = 1/7, n = 6/7 (m, n being the exponents in the power-law approximations to the vertical profiles of mean wind speed and eddy diffusivity, respectively). The rudiments of a quantitative theory of advective inversion are developed, expressions being obtained for the equation of the inversion surface, and for the maximum height and downwind extent of the inversion.
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      THE THEORY OF LOCAL ADVECTION: I

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4150133
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    contributor authorPhilip, J. R.
    date accessioned2017-06-09T14:12:12Z
    date available2017-06-09T14:12:12Z
    date copyright1959/10/01
    date issued1959
    identifier issn0095-9634
    identifier otherams-14559.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150133
    description abstractThis paper is the first of a series in which the theory of local advection (the exchange due to horizontal heterogeneity) of energy and moisture will be developed and applied to a number of problems of practical and theoretical interest. The paper provides an introduction to the practical implications and physical basis of local advection, but it is mainly devoted to developing methods of analysis to be applied in later papers. The treatment aims to provide simple and rapid numerical procedures for the solution of advection problems. Methods are given for solving the two-dimensional atmospheric-diffusion equation subject to ?concentration,? ?flux,? and ?radiation? types of boundary conditions. Appendices give discussions of the properties of the functions entering the solutions and provide simple means for their computation. Extensive tables of the relevant functions are given for the case m = 1/7, n = 6/7 (m, n being the exponents in the power-law approximations to the vertical profiles of mean wind speed and eddy diffusivity, respectively). The rudiments of a quantitative theory of advective inversion are developed, expressions being obtained for the equation of the inversion surface, and for the maximum height and downwind extent of the inversion.
    publisherAmerican Meteorological Society
    titleTHE THEORY OF LOCAL ADVECTION: I
    typeJournal Paper
    journal volume16
    journal issue5
    journal titleJournal of Meteorology
    identifier doi10.1175/1520-0469(1959)016<0535:TTOLAI>2.0.CO;2
    journal fristpage535
    journal lastpage547
    treeJournal of Meteorology:;1959:;volume( 016 ):;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
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