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    Removal of Aerosol Particles and Fractional Separation of HDO-H2O During Snowstorms

    Source: Journal of the Atmospheric Sciences:;1969:;Volume( 026 ):;issue: 002::page 289
    Author:
    Rosinski, J.
    ,
    Langer, G.
    ,
    Bleck, R.
    DOI: 10.1175/1520-0469(1969)026<0289:ROAPAF>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The concentrations of both deuterium and water-insoluble particles in snow collected during snowstorms in the mountains of Colorado were found to be proportional to the size of snowflakes. Large snowflakes were associated with high particle concentration and high deuterium content. Small snow crystals appear to have originated in deuterium and aerosol-particle depleted air. The small snow crystals appeared at times of highest ice-forming nuclei concentration in air. The ratios of concentrations of different sized particles present in snow collected during a brief snowshower in March reveal that the predominant particles within small snow crystals are indeed those corresponding to the size range of ice nuclei. The relationship between the number of different sized particles present in a single snow crystal and the mass of snow crystals is given. Analyses of trajectories of moisture-bearing air parcels explained the large difference between the deuterium content of snow from the two snowfalls.
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      Removal of Aerosol Particles and Fractional Separation of HDO-H2O During Snowstorms

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4151269
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    • Journal of the Atmospheric Sciences

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    contributor authorRosinski, J.
    contributor authorLanger, G.
    contributor authorBleck, R.
    date accessioned2017-06-09T14:14:48Z
    date available2017-06-09T14:14:48Z
    date copyright1969/03/01
    date issued1969
    identifier issn0022-4928
    identifier otherams-15581.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151269
    description abstractThe concentrations of both deuterium and water-insoluble particles in snow collected during snowstorms in the mountains of Colorado were found to be proportional to the size of snowflakes. Large snowflakes were associated with high particle concentration and high deuterium content. Small snow crystals appear to have originated in deuterium and aerosol-particle depleted air. The small snow crystals appeared at times of highest ice-forming nuclei concentration in air. The ratios of concentrations of different sized particles present in snow collected during a brief snowshower in March reveal that the predominant particles within small snow crystals are indeed those corresponding to the size range of ice nuclei. The relationship between the number of different sized particles present in a single snow crystal and the mass of snow crystals is given. Analyses of trajectories of moisture-bearing air parcels explained the large difference between the deuterium content of snow from the two snowfalls.
    publisherAmerican Meteorological Society
    titleRemoval of Aerosol Particles and Fractional Separation of HDO-H2O During Snowstorms
    typeJournal Paper
    journal volume26
    journal issue2
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1969)026<0289:ROAPAF>2.0.CO;2
    journal fristpage289
    journal lastpage301
    treeJournal of the Atmospheric Sciences:;1969:;Volume( 026 ):;issue: 002
    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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