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    Investigation of the Variability of Cloud Condensation Nuclei Concentrations at the Surface in Western North Dakota

    Source: Journal of Applied Meteorology and Climatology:;2010:;volume( 049 ):;issue: 001::page 136
    Author:
    Detwiler, Andrew
    ,
    Langerud, Darin
    ,
    Depue, Tracy
    DOI: 10.1175/2009JAMC2150.1
    Publisher: American Meteorological Society
    Abstract: Daily observations of cloud condensation nuclei (CCN) were made for three summer months in 2005 at a site in rural western North Dakota. The goal was to define the natural background CCN population characteristics and to lay the groundwork for investigating the potential impact of intentionally modifying clouds in this region using hygroscopic cloud-seeding techniques. Concentrations of CCN active at ?0.5% supersaturation, averaged over several midday hours on each day, ranged from less than 200 to more than 1700 cm?3. This is similar to variability in CCN concentrations that have been observed in past studies in other rural areas of the central and northern high plains of the United States. At this site, only 2 out of 17 days with active convection at that site were characterized by concentrations of less than 300 cm?3 active at 0.5% supersaturation, indicating that the region is characterized by typically continental CCN populations on most convective days. Operational seeding might be more effectively conducted if CCN population characteristics could be forecast based on source regions for air forecast to arrive in a particular region on a particular day. However, back-trajectory calculations were found to have limited use for predicting CCN concentrations based on prior history of the air arriving at this observation site during this period.
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      Investigation of the Variability of Cloud Condensation Nuclei Concentrations at the Surface in Western North Dakota

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4209853
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    contributor authorDetwiler, Andrew
    contributor authorLangerud, Darin
    contributor authorDepue, Tracy
    date accessioned2017-06-09T16:27:49Z
    date available2017-06-09T16:27:49Z
    date copyright2010/01/01
    date issued2010
    identifier issn1558-8424
    identifier otherams-68309.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4209853
    description abstractDaily observations of cloud condensation nuclei (CCN) were made for three summer months in 2005 at a site in rural western North Dakota. The goal was to define the natural background CCN population characteristics and to lay the groundwork for investigating the potential impact of intentionally modifying clouds in this region using hygroscopic cloud-seeding techniques. Concentrations of CCN active at ?0.5% supersaturation, averaged over several midday hours on each day, ranged from less than 200 to more than 1700 cm?3. This is similar to variability in CCN concentrations that have been observed in past studies in other rural areas of the central and northern high plains of the United States. At this site, only 2 out of 17 days with active convection at that site were characterized by concentrations of less than 300 cm?3 active at 0.5% supersaturation, indicating that the region is characterized by typically continental CCN populations on most convective days. Operational seeding might be more effectively conducted if CCN population characteristics could be forecast based on source regions for air forecast to arrive in a particular region on a particular day. However, back-trajectory calculations were found to have limited use for predicting CCN concentrations based on prior history of the air arriving at this observation site during this period.
    publisherAmerican Meteorological Society
    titleInvestigation of the Variability of Cloud Condensation Nuclei Concentrations at the Surface in Western North Dakota
    typeJournal Paper
    journal volume49
    journal issue1
    journal titleJournal of Applied Meteorology and Climatology
    identifier doi10.1175/2009JAMC2150.1
    journal fristpage136
    journal lastpage145
    treeJournal of Applied Meteorology and Climatology:;2010:;volume( 049 ):;issue: 001
    contenttypeFulltext
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