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    Aggregation and Scaling of Ice Crystal Size Distributions

    Source: Journal of the Atmospheric Sciences:;2003:;Volume( 060 ):;issue: 003::page 544
    Author:
    Field, Paul R.
    ,
    Heymsfield, Andrew J.
    DOI: 10.1175/1520-0469(2003)060<0544:AASOIC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Ice particle size distributions (PSDs) can be scaled onto a single exponential distribution for a wide range of observed conditions as demonstrated using data from Atmospheric Research Measurement (ARM) cirrus uncinus, Tropical Rainfall Measurement Mission (TRMM) tropical anvils, and First International Satellite Cloud Climatalogy Project (ISCCP) Regional Experiment (FIRE1) midlatitude cirrus field programs. The successful scaling of the PSDs is the result of the dominance of the aggregation process. The PSD is found to be a function of mean particle size and precipitation rate only. A correlation between precipitation rate and particle mass and fall speed relations is demonstrated and made use of in a semiempirical model of ice cloud that predicts the evolution of PSDs.
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      Aggregation and Scaling of Ice Crystal Size Distributions

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4159809
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    contributor authorField, Paul R.
    contributor authorHeymsfield, Andrew J.
    date accessioned2017-06-09T14:38:09Z
    date available2017-06-09T14:38:09Z
    date copyright2003/02/01
    date issued2003
    identifier issn0022-4928
    identifier otherams-23267.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4159809
    description abstractIce particle size distributions (PSDs) can be scaled onto a single exponential distribution for a wide range of observed conditions as demonstrated using data from Atmospheric Research Measurement (ARM) cirrus uncinus, Tropical Rainfall Measurement Mission (TRMM) tropical anvils, and First International Satellite Cloud Climatalogy Project (ISCCP) Regional Experiment (FIRE1) midlatitude cirrus field programs. The successful scaling of the PSDs is the result of the dominance of the aggregation process. The PSD is found to be a function of mean particle size and precipitation rate only. A correlation between precipitation rate and particle mass and fall speed relations is demonstrated and made use of in a semiempirical model of ice cloud that predicts the evolution of PSDs.
    publisherAmerican Meteorological Society
    titleAggregation and Scaling of Ice Crystal Size Distributions
    typeJournal Paper
    journal volume60
    journal issue3
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(2003)060<0544:AASOIC>2.0.CO;2
    journal fristpage544
    journal lastpage560
    treeJournal of the Atmospheric Sciences:;2003:;Volume( 060 ):;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
    yabeshDSpacePersian