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    Cloud Microphysical Relationships in California Marine Stratus

    Source: Journal of Applied Meteorology:;1995:;volume( 034 ):;issue: 012::page 2655
    Author:
    Hudson, James G.
    ,
    Svensson, Gunilla
    DOI: 10.1175/1520-0450(1995)034<2655:CMRICM>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Cloud microphysical measurements off the southern California coast are presented and compared with in situ airborne measurements of cloud condensation nuclei (CCN) spectra. Large-scale variations in cloud droplet concentrations were due to CCN variations, some medium-scale variations may be a result of the conversion of droplets to drops by coalescence, while small-scale variations were due to different proportions of the CCN spectra being activated because of variations in updraft velocity at cloud base. This latter internal mixing process produces an inverse relationship between droplet concentration and mean size and an increase in droplet spectral width with mean droplet size. Drizzle drop concentrations are strongly associated with lower droplet concentrations, larger droplets, and greater droplet spectral width.
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      Cloud Microphysical Relationships in California Marine Stratus

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4147562
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    contributor authorHudson, James G.
    contributor authorSvensson, Gunilla
    date accessioned2017-06-09T14:05:31Z
    date available2017-06-09T14:05:31Z
    date copyright1995/12/01
    date issued1995
    identifier issn0894-8763
    identifier otherams-12244.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4147562
    description abstractCloud microphysical measurements off the southern California coast are presented and compared with in situ airborne measurements of cloud condensation nuclei (CCN) spectra. Large-scale variations in cloud droplet concentrations were due to CCN variations, some medium-scale variations may be a result of the conversion of droplets to drops by coalescence, while small-scale variations were due to different proportions of the CCN spectra being activated because of variations in updraft velocity at cloud base. This latter internal mixing process produces an inverse relationship between droplet concentration and mean size and an increase in droplet spectral width with mean droplet size. Drizzle drop concentrations are strongly associated with lower droplet concentrations, larger droplets, and greater droplet spectral width.
    publisherAmerican Meteorological Society
    titleCloud Microphysical Relationships in California Marine Stratus
    typeJournal Paper
    journal volume34
    journal issue12
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1995)034<2655:CMRICM>2.0.CO;2
    journal fristpage2655
    journal lastpage2666
    treeJournal of Applied Meteorology:;1995:;volume( 034 ):;issue: 012
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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