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    A Rate Equation for the Inversion Height in a Nocturnal Boundary Layer

    Source: Journal of Applied Meteorology:;1979:;volume( 019 ):;issue: 012::page 1445
    Author:
    Nieuwstadt, F. T. M.
    DOI: 10.1175/1520-0450(1980)019<1445:AREFTI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The application of a self-similar profile in the integration of the temperature equation across the stable boundary layer leads to a rate equation for the inversion height. An analytic solution of the resulting equation is derived. Its behavior is determined by two processes; cooling by turbulent mixing and cooling by internal radiation, the latter is parameterized in terms of the surface cooling rate. This parameterization, which attributes the temperature change in the boundary layer close to the surface completely to internal radiation, leads to a monotonic growth of the inversion depth. When the radiation term is neglected and only the turbulent heat flux is taken into account, the solution is governed by a relaxation process.
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      A Rate Equation for the Inversion Height in a Nocturnal Boundary Layer

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4145073
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    contributor authorNieuwstadt, F. T. M.
    date accessioned2017-06-09T13:57:59Z
    date available2017-06-09T13:57:59Z
    date copyright1980/12/01
    date issued1979
    identifier issn0021-8952
    identifier otherams-10003.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145073
    description abstractThe application of a self-similar profile in the integration of the temperature equation across the stable boundary layer leads to a rate equation for the inversion height. An analytic solution of the resulting equation is derived. Its behavior is determined by two processes; cooling by turbulent mixing and cooling by internal radiation, the latter is parameterized in terms of the surface cooling rate. This parameterization, which attributes the temperature change in the boundary layer close to the surface completely to internal radiation, leads to a monotonic growth of the inversion depth. When the radiation term is neglected and only the turbulent heat flux is taken into account, the solution is governed by a relaxation process.
    publisherAmerican Meteorological Society
    titleA Rate Equation for the Inversion Height in a Nocturnal Boundary Layer
    typeJournal Paper
    journal volume19
    journal issue12
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1980)019<1445:AREFTI>2.0.CO;2
    journal fristpage1445
    journal lastpage1447
    treeJournal of Applied Meteorology:;1979:;volume( 019 ):;issue: 012
    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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