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    Microphysical Effects of Seeding Wintertime Stratiform Clouds Near the Sierra Nevada Mountains

    Source: Journal of Applied Meteorology:;1982:;volume( 021 ):;issue: 006::page 874
    Author:
    Stewart, Ronald E.
    ,
    Marwitz, John D.
    DOI: 10.1175/1520-0450(1982)021<0874:MEOSWS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The microphysical consequences of seeding stratiform clouds near the Sierra Nevada Mountains are examined. Airborne seeding was conducted with droppable AgI flares released every 250 m and with dry ice pellets released at a rate of 0.1 g m?1 into the clouds having widespread liquid water contents ?0.1 g m?3. The Wyoming King Air penetrated the AgI curtains for ?1 h after seeding. The CO2 ice crystal curtain could not be determined beyond ?10 min because of natural cloud glaciation. Precipitation sized particles grew mainly by diffusion, and particle size spectra at particular levels below cloud top reached and maintained equilibrium shapes as a consequence of particles falling from higher levels.
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      Microphysical Effects of Seeding Wintertime Stratiform Clouds Near the Sierra Nevada Mountains

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4145391
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    contributor authorStewart, Ronald E.
    contributor authorMarwitz, John D.
    date accessioned2017-06-09T13:58:50Z
    date available2017-06-09T13:58:50Z
    date copyright1982/06/01
    date issued1982
    identifier issn0021-8952
    identifier otherams-10290.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145391
    description abstractThe microphysical consequences of seeding stratiform clouds near the Sierra Nevada Mountains are examined. Airborne seeding was conducted with droppable AgI flares released every 250 m and with dry ice pellets released at a rate of 0.1 g m?1 into the clouds having widespread liquid water contents ?0.1 g m?3. The Wyoming King Air penetrated the AgI curtains for ?1 h after seeding. The CO2 ice crystal curtain could not be determined beyond ?10 min because of natural cloud glaciation. Precipitation sized particles grew mainly by diffusion, and particle size spectra at particular levels below cloud top reached and maintained equilibrium shapes as a consequence of particles falling from higher levels.
    publisherAmerican Meteorological Society
    titleMicrophysical Effects of Seeding Wintertime Stratiform Clouds Near the Sierra Nevada Mountains
    typeJournal Paper
    journal volume21
    journal issue6
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1982)021<0874:MEOSWS>2.0.CO;2
    journal fristpage874
    journal lastpage880
    treeJournal of Applied Meteorology:;1982:;volume( 021 ):;issue: 006
    contenttypeFulltext
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