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    A Steady-State Stratospheric Aerosol Model

    Source: Journal of the Atmospheric Sciences:;1978:;Volume( 035 ):;issue: 007::page 1304
    Author:
    Rosen, J. M.
    ,
    Hofmann, D. J.
    ,
    Singh, S. P.
    DOI: 10.1175/1520-0469(1978)035<1304:ASSSAM>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: This paper deals with the development of a one-dimensional steady-state stratospheric aerosol model and the subsequent perturbations caused by including the expected space shuttle particulate effluents in the model. Two approaches to the basic modeling effort have been made: in one, enough simplifying assumptions were introduced so that a more or less exact solution to the descriptive equations could be obtained; in the other, very few simplifications were made and a computer technique was used to solve the equations. The most complete form of the model contains the effects of sedimentation, diffusion, particle growth and coagulation. The results indicate that the model is capable of describing many aspects of the stratospheric aerosol layer, such as size distribution and the vertical profile of particles >0.3 ?m diameter.
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      A Steady-State Stratospheric Aerosol Model

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4153422
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    • Journal of the Atmospheric Sciences

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    contributor authorRosen, J. M.
    contributor authorHofmann, D. J.
    contributor authorSingh, S. P.
    date accessioned2017-06-09T14:20:15Z
    date available2017-06-09T14:20:15Z
    date copyright1978/07/01
    date issued1978
    identifier issn0022-4928
    identifier otherams-17519.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153422
    description abstractThis paper deals with the development of a one-dimensional steady-state stratospheric aerosol model and the subsequent perturbations caused by including the expected space shuttle particulate effluents in the model. Two approaches to the basic modeling effort have been made: in one, enough simplifying assumptions were introduced so that a more or less exact solution to the descriptive equations could be obtained; in the other, very few simplifications were made and a computer technique was used to solve the equations. The most complete form of the model contains the effects of sedimentation, diffusion, particle growth and coagulation. The results indicate that the model is capable of describing many aspects of the stratospheric aerosol layer, such as size distribution and the vertical profile of particles >0.3 ?m diameter.
    publisherAmerican Meteorological Society
    titleA Steady-State Stratospheric Aerosol Model
    typeJournal Paper
    journal volume35
    journal issue7
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1978)035<1304:ASSSAM>2.0.CO;2
    journal fristpage1304
    journal lastpage1313
    treeJournal of the Atmospheric Sciences:;1978:;Volume( 035 ):;issue: 007
    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