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    Cloud Microstructure as Determined by an Optical Cloud Particle Spectrometer

    Source: Journal of Applied Meteorology:;1972:;volume( 011 ):;issue: 001::page 149
    Author:
    Ryan, R. T.
    ,
    Blau, H. H.
    ,
    von Thüna, P. C.
    ,
    Cohen, M. L.
    ,
    Roberts, G. D.
    DOI: 10.1175/1520-0450(1972)011<0149:CMADBA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: An improved single-particle light scattering instrument for measurement of cloud microstructure has been built and used in field studies. Cloud particle size and number information is measured over 12 sizing intervals, in the range 4 to 85 ? diameter. The microstructure can be observed in real time and with a spatial resolution not previously reported. The general features of water cloud droplet size and number distributions are consistent with previous direct capture and replication studies. The transition from water to ice phase regions in cumuliform clouds can be inferred from dramatic changes observed in the distribution features. Results are also presented for stratus and cirrus cloud penetrations.
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      Cloud Microstructure as Determined by an Optical Cloud Particle Spectrometer

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4226223
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    contributor authorRyan, R. T.
    contributor authorBlau, H. H.
    contributor authorvon Thüna, P. C.
    contributor authorCohen, M. L.
    contributor authorRoberts, G. D.
    date accessioned2017-06-09T17:18:57Z
    date available2017-06-09T17:18:57Z
    date copyright1972/02/01
    date issued1972
    identifier issn0021-8952
    identifier otherams-8304.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4226223
    description abstractAn improved single-particle light scattering instrument for measurement of cloud microstructure has been built and used in field studies. Cloud particle size and number information is measured over 12 sizing intervals, in the range 4 to 85 ? diameter. The microstructure can be observed in real time and with a spatial resolution not previously reported. The general features of water cloud droplet size and number distributions are consistent with previous direct capture and replication studies. The transition from water to ice phase regions in cumuliform clouds can be inferred from dramatic changes observed in the distribution features. Results are also presented for stratus and cirrus cloud penetrations.
    publisherAmerican Meteorological Society
    titleCloud Microstructure as Determined by an Optical Cloud Particle Spectrometer
    typeJournal Paper
    journal volume11
    journal issue1
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1972)011<0149:CMADBA>2.0.CO;2
    journal fristpage149
    journal lastpage156
    treeJournal of Applied Meteorology:;1972:;volume( 011 ):;issue: 001
    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