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    Balloonborne Measurements of Condensation Nuclei

    Source: Journal of Applied Meteorology:;1977:;volume( 016 ):;issue: 001::page 56
    Author:
    Rosen, J. M.
    ,
    Hofmann, D. J.
    DOI: 10.1175/1520-0450(1977)016<0056:BMOCN>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A condensation nuclei (CN) counter has been developed for balloonborne use at ambient pressures in the troposphere and stratosphere. The instrument employs a thermal gradient diffusion cloud chamber to produce particle growth and a photoelectric particle counter for detection. After extensive laboratory tests, the instrument was successfully flown on several balloon soundings over Laramie. The results show a roughly constant mixing ratio in the stratosphere with a CN concentration of about 20 cm?3 at 15 km. The vertical profile of CN in the troposphere displayed concentration fluctuations ranging between 200 and 2000 cm?3 with a definite maximum in the mixing ratio just below the tropopause.
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      Balloonborne Measurements of Condensation Nuclei

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4232675
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    contributor authorRosen, J. M.
    contributor authorHofmann, D. J.
    date accessioned2017-06-09T17:38:55Z
    date available2017-06-09T17:38:55Z
    date copyright1977/01/01
    date issued1977
    identifier issn0021-8952
    identifier otherams-9211.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4232675
    description abstractA condensation nuclei (CN) counter has been developed for balloonborne use at ambient pressures in the troposphere and stratosphere. The instrument employs a thermal gradient diffusion cloud chamber to produce particle growth and a photoelectric particle counter for detection. After extensive laboratory tests, the instrument was successfully flown on several balloon soundings over Laramie. The results show a roughly constant mixing ratio in the stratosphere with a CN concentration of about 20 cm?3 at 15 km. The vertical profile of CN in the troposphere displayed concentration fluctuations ranging between 200 and 2000 cm?3 with a definite maximum in the mixing ratio just below the tropopause.
    publisherAmerican Meteorological Society
    titleBalloonborne Measurements of Condensation Nuclei
    typeJournal Paper
    journal volume16
    journal issue1
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1977)016<0056:BMOCN>2.0.CO;2
    journal fristpage56
    journal lastpage62
    treeJournal of Applied Meteorology:;1977:;volume( 016 ):;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
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