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    DIFFUSION OF SMOKE IN THE STRATOSPHERE

    Source: Journal of Meteorology:;1956:;volume( 013 ):;issue: 003::page 241
    Author:
    Kellogg, William W.
    DOI: 10.1175/1520-0469(1956)013<0241:DOSITS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Data from the High Altitude Dust Diffusion Project have been analyzed, and the rates of growth of 18 smoke puffs produced in the upper troposphere and stratosphere are presented. There was an increase in the rate of growth of the cloud size with increasing height, and a decrease in the rate of growth of the cloud mass with increasing stability of the atmosphere. From an initial diameter of 15 to 20 meters, the diameter of the smoke puffs increased fivefold in about 3 minutes, on the average. A theoretical analysis of the growth of a smoke puff resulted in an equation describing the visual diameter as a function of time and a variety of turbulence parameters. Comparison between theory and experiment, based on Taylor's theory of ?diffusion by continuous movement,? suggests that the root-mean-square eddy velocity in the stratosphere is of the order of 4 to 10 centimeters per second and increases with height.
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      DIFFUSION OF SMOKE IN THE STRATOSPHERE

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4149799
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    contributor authorKellogg, William W.
    date accessioned2017-06-09T14:11:27Z
    date available2017-06-09T14:11:27Z
    date copyright1956/06/01
    date issued1956
    identifier issn0095-9634
    identifier otherams-14258.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149799
    description abstractData from the High Altitude Dust Diffusion Project have been analyzed, and the rates of growth of 18 smoke puffs produced in the upper troposphere and stratosphere are presented. There was an increase in the rate of growth of the cloud size with increasing height, and a decrease in the rate of growth of the cloud mass with increasing stability of the atmosphere. From an initial diameter of 15 to 20 meters, the diameter of the smoke puffs increased fivefold in about 3 minutes, on the average. A theoretical analysis of the growth of a smoke puff resulted in an equation describing the visual diameter as a function of time and a variety of turbulence parameters. Comparison between theory and experiment, based on Taylor's theory of ?diffusion by continuous movement,? suggests that the root-mean-square eddy velocity in the stratosphere is of the order of 4 to 10 centimeters per second and increases with height.
    publisherAmerican Meteorological Society
    titleDIFFUSION OF SMOKE IN THE STRATOSPHERE
    typeJournal Paper
    journal volume13
    journal issue3
    journal titleJournal of Meteorology
    identifier doi10.1175/1520-0469(1956)013<0241:DOSITS>2.0.CO;2
    journal fristpage241
    journal lastpage250
    treeJournal of Meteorology:;1956:;volume( 013 ):;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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