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    A METHOD FOR THE INTEGRATION OF THE RADIATIVE-TRANSFER EQUATION

    Source: Journal of Meteorology:;1955:;volume( 012 ):;issue: 003::page 191
    Author:
    Plass, Gilbert N.
    ,
    Fivel, Daniel I.
    DOI: 10.1175/1520-0469(1955)012<0191:AMFTIO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The equations for radiative transfer are integrated exactly for a band of spectral lines which do not overlap and for an Elsasser band. The result of the two-fold integration of the absorption over frequency and over the atmospheric path can be expressed in terms of the Legendre functions. Here it is assumed that the mixing ratio is constant, that the line intensity is independent of temperature, and that the Lorentz line shape is valid. Asymptotic forms of the Legendre functions are used to obtain the solutions to the following problems from these exact results. The regions of validity of the single-line and strong-line approximations are precisely stated. It is shown that the strongest line in the band absorbs more radiation than any other line in an atmospheric layer, when the overlap of the lines can be neglected. For an Elsasser band, an expression is derived for the line strength that gives the maximum absorption in an atmospheric layer for radiation emitted either by a black body at another level or by another atmospheric layer.
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      A METHOD FOR THE INTEGRATION OF THE RADIATIVE-TRANSFER EQUATION

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4149691
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    • Journal of Meteorology

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    contributor authorPlass, Gilbert N.
    contributor authorFivel, Daniel I.
    date accessioned2017-06-09T14:11:13Z
    date available2017-06-09T14:11:13Z
    date copyright1955/06/01
    date issued1955
    identifier issn0095-9634
    identifier otherams-14160.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149691
    description abstractThe equations for radiative transfer are integrated exactly for a band of spectral lines which do not overlap and for an Elsasser band. The result of the two-fold integration of the absorption over frequency and over the atmospheric path can be expressed in terms of the Legendre functions. Here it is assumed that the mixing ratio is constant, that the line intensity is independent of temperature, and that the Lorentz line shape is valid. Asymptotic forms of the Legendre functions are used to obtain the solutions to the following problems from these exact results. The regions of validity of the single-line and strong-line approximations are precisely stated. It is shown that the strongest line in the band absorbs more radiation than any other line in an atmospheric layer, when the overlap of the lines can be neglected. For an Elsasser band, an expression is derived for the line strength that gives the maximum absorption in an atmospheric layer for radiation emitted either by a black body at another level or by another atmospheric layer.
    publisherAmerican Meteorological Society
    titleA METHOD FOR THE INTEGRATION OF THE RADIATIVE-TRANSFER EQUATION
    typeJournal Paper
    journal volume12
    journal issue3
    journal titleJournal of Meteorology
    identifier doi10.1175/1520-0469(1955)012<0191:AMFTIO>2.0.CO;2
    journal fristpage191
    journal lastpage200
    treeJournal of Meteorology:;1955:;volume( 012 ):;issue: 003
    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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