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    The Relation Between Visibility and the Size-Number Distribution of Airborne Soil Particles

    Source: Journal of Applied Meteorology:;1976:;volume( 015 ):;issue: 005::page 470
    Author:
    Patterson, E. M.
    ,
    Gillette, D. A.
    ,
    Grams, G. W.
    DOI: 10.1175/1520-0450(1976)015<0470:TRBVAT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Simultaneous visibility observations and size-number distribution measurements of airborne soil particles were made during incidents of soil erosion in west Texas. Visibilities were calculated by applying Mie scattering theory to measured size distributions and were compared with observed visibilities. Agreement was found, and similar comparison with artifical modicications to the observed size distributions demonstrated that any major changes in the observed size distributions would result in significant discrepancies between the observed and the calculated visibilities. These comparisons confirm that under our experimental conditions the optically important particles are those in the size range 0.62 < r < 20 ?m. The sensitivity of the calculated visibility to modifications in the measured size distribution implies that such comparisons between calculated and observed visibility provide a means of confirming size distribution measurements under a variety of conditions.
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      The Relation Between Visibility and the Size-Number Distribution of Airborne Soil Particles

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4232519
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    contributor authorPatterson, E. M.
    contributor authorGillette, D. A.
    contributor authorGrams, G. W.
    date accessioned2017-06-09T17:38:35Z
    date available2017-06-09T17:38:35Z
    date copyright1976/05/01
    date issued1976
    identifier issn0021-8952
    identifier otherams-9071.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4232519
    description abstractSimultaneous visibility observations and size-number distribution measurements of airborne soil particles were made during incidents of soil erosion in west Texas. Visibilities were calculated by applying Mie scattering theory to measured size distributions and were compared with observed visibilities. Agreement was found, and similar comparison with artifical modicications to the observed size distributions demonstrated that any major changes in the observed size distributions would result in significant discrepancies between the observed and the calculated visibilities. These comparisons confirm that under our experimental conditions the optically important particles are those in the size range 0.62 < r < 20 ?m. The sensitivity of the calculated visibility to modifications in the measured size distribution implies that such comparisons between calculated and observed visibility provide a means of confirming size distribution measurements under a variety of conditions.
    publisherAmerican Meteorological Society
    titleThe Relation Between Visibility and the Size-Number Distribution of Airborne Soil Particles
    typeJournal Paper
    journal volume15
    journal issue5
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1976)015<0470:TRBVAT>2.0.CO;2
    journal fristpage470
    journal lastpage478
    treeJournal of Applied Meteorology:;1976:;volume( 015 ):;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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