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    Salt Particles and Raindrops in Hawaii

    Source: Journal of the Atmospheric Sciences:;1971:;Volume( 028 ):;issue: 007::page 1252
    Author:
    Woodcock, Alfred H.
    ,
    Duce, Robert A.
    ,
    Moyers, Jarvis L.
    DOI: 10.1175/1520-0469(1971)028<1252:SPARIH>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Particles of sea salt of different size in the marine air of Hawaii exhibit different ratios of iodine to chlorine, whereas raindrops of various sizes in Hawaii warm orographic showers contain iodine and chlorine in a relatively constant ratio. The mean value of the I/Cl ratio for raindrops (?2.0 ? 10?3) corresponds to the mean found among the smaller of the salt particles of weight range ?10?12?10?14 gm. On the other hand, the mean I/Cl value among the giant salt particles of weight range of ?10?8?10?12 gm is shown to be ?3 ? 10?4. It appears that raindrop growth occurs through coalescence among cloud droplets formed on the 10?12?10?14 gm salt particles. This result is interpreted to mean that in warm oceanic tradewind clouds giant salt nuclei may not, after all, be essential to the formation of raindrops.
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      Salt Particles and Raindrops in Hawaii

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4151793
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    contributor authorWoodcock, Alfred H.
    contributor authorDuce, Robert A.
    contributor authorMoyers, Jarvis L.
    date accessioned2017-06-09T14:16:07Z
    date available2017-06-09T14:16:07Z
    date copyright1971/10/01
    date issued1971
    identifier issn0022-4928
    identifier otherams-16052.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151793
    description abstractParticles of sea salt of different size in the marine air of Hawaii exhibit different ratios of iodine to chlorine, whereas raindrops of various sizes in Hawaii warm orographic showers contain iodine and chlorine in a relatively constant ratio. The mean value of the I/Cl ratio for raindrops (?2.0 ? 10?3) corresponds to the mean found among the smaller of the salt particles of weight range ?10?12?10?14 gm. On the other hand, the mean I/Cl value among the giant salt particles of weight range of ?10?8?10?12 gm is shown to be ?3 ? 10?4. It appears that raindrop growth occurs through coalescence among cloud droplets formed on the 10?12?10?14 gm salt particles. This result is interpreted to mean that in warm oceanic tradewind clouds giant salt nuclei may not, after all, be essential to the formation of raindrops.
    publisherAmerican Meteorological Society
    titleSalt Particles and Raindrops in Hawaii
    typeJournal Paper
    journal volume28
    journal issue7
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1971)028<1252:SPARIH>2.0.CO;2
    journal fristpage1252
    journal lastpage1257
    treeJournal of the Atmospheric Sciences:;1971:;Volume( 028 ):;issue: 007
    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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