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    Stratospheric Particles

    Source: Journal of the Atmospheric Sciences:;1975:;Volume( 032 ):;issue: 005::page 910
    Author:
    Bigg, E. K.
    DOI: 10.1175/1520-0469(1975)032<0910:SP>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Particles were collected from the stratosphere by impaction onto specially treated electron microscope screens during six balloon flights in Wyoming in 1972. The submicron diameter particles were predominantly ammonium sulfate near the tropopause and sulfuric acid at higher altitudes, though the ratio of acid to non-acid decreased rapidly with particle diameter, even at the higher altitudes. The acid particles were often, but not always, in a frozen state and aggregates joined in irregular groups were often observed near 20 km altitude. Number concentrations were usually in reasonable agreement with those found by the University of Wyoming's optical counter carried on the same flight, though conspicuously lower concentrations were found near 20 km on two occasions. This is attributed to incomplete collection of frozen aggregates. Size distributions suggested a relatively large number of particles smaller than 0.2? am diameter near the tropopause but few above about 20 km. The distribution of mass with particle diameter implies that an impactor may sometimes underestimate the total mass.
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      Stratospheric Particles

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4152638
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    contributor authorBigg, E. K.
    date accessioned2017-06-09T14:18:09Z
    date available2017-06-09T14:18:09Z
    date copyright1975/05/01
    date issued1975
    identifier issn0022-4928
    identifier otherams-16813.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152638
    description abstractParticles were collected from the stratosphere by impaction onto specially treated electron microscope screens during six balloon flights in Wyoming in 1972. The submicron diameter particles were predominantly ammonium sulfate near the tropopause and sulfuric acid at higher altitudes, though the ratio of acid to non-acid decreased rapidly with particle diameter, even at the higher altitudes. The acid particles were often, but not always, in a frozen state and aggregates joined in irregular groups were often observed near 20 km altitude. Number concentrations were usually in reasonable agreement with those found by the University of Wyoming's optical counter carried on the same flight, though conspicuously lower concentrations were found near 20 km on two occasions. This is attributed to incomplete collection of frozen aggregates. Size distributions suggested a relatively large number of particles smaller than 0.2? am diameter near the tropopause but few above about 20 km. The distribution of mass with particle diameter implies that an impactor may sometimes underestimate the total mass.
    publisherAmerican Meteorological Society
    titleStratospheric Particles
    typeJournal Paper
    journal volume32
    journal issue5
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1975)032<0910:SP>2.0.CO;2
    journal fristpage910
    journal lastpage917
    treeJournal of the Atmospheric Sciences:;1975:;Volume( 032 ):;issue: 005
    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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