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    Eddy Correlation Measurements of the Dry Deposition of Particles in Wintertime

    Source: Journal of Applied Meteorology:;1988:;volume( 027 ):;issue: 005::page 642
    Author:
    Duan, B.
    ,
    Fairall, C. W.
    ,
    Thomson, D. W.
    DOI: 10.1175/1520-0450(1988)027<0642:ECMOTD>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Eddy correlation measurements of the vertical fluxes of particles, momentum, heat and water vapor, were conducted over a partially snow covered field in central Pennsylvania during December 1985. The PMS ASASP-300 and CSASP-100-HV optical counters were used as sensors to measure particle-number fluxes. Overall, average dry deposition velocities for 28 half-hour runs were found to be 0.034 ± 0.014 and 0.021 ± 0.005 cm s?1 for particles in two size ranges, 0.15?30 and 0.5?1.0 ?m, respectively. The average deposition velocity was close to results from prior wind-tunnel and theoretical investigations. These results were also comparable with those reported by other authors over grass. Relatively large sampling rates reduced the effects of counting noise on deposition measurements of 0.5?;1.0 ?m particles. Small correlation coefficients between vertical velocity and the particle concentration were found even after corrections for the effects of counting noise. The normalized average surface deposition velocity vds/u* for particles in diameter of 0.15?0.30 and 0.5?1.0 ?m appeared to be 0.006 and 0.002, respectively, in nearly neutral and stable conditions.
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      Eddy Correlation Measurements of the Dry Deposition of Particles in Wintertime

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4146554
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    contributor authorDuan, B.
    contributor authorFairall, C. W.
    contributor authorThomson, D. W.
    date accessioned2017-06-09T14:02:19Z
    date available2017-06-09T14:02:19Z
    date copyright1988/05/01
    date issued1988
    identifier issn0894-8763
    identifier otherams-11337.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146554
    description abstractEddy correlation measurements of the vertical fluxes of particles, momentum, heat and water vapor, were conducted over a partially snow covered field in central Pennsylvania during December 1985. The PMS ASASP-300 and CSASP-100-HV optical counters were used as sensors to measure particle-number fluxes. Overall, average dry deposition velocities for 28 half-hour runs were found to be 0.034 ± 0.014 and 0.021 ± 0.005 cm s?1 for particles in two size ranges, 0.15?30 and 0.5?1.0 ?m, respectively. The average deposition velocity was close to results from prior wind-tunnel and theoretical investigations. These results were also comparable with those reported by other authors over grass. Relatively large sampling rates reduced the effects of counting noise on deposition measurements of 0.5?;1.0 ?m particles. Small correlation coefficients between vertical velocity and the particle concentration were found even after corrections for the effects of counting noise. The normalized average surface deposition velocity vds/u* for particles in diameter of 0.15?0.30 and 0.5?1.0 ?m appeared to be 0.006 and 0.002, respectively, in nearly neutral and stable conditions.
    publisherAmerican Meteorological Society
    titleEddy Correlation Measurements of the Dry Deposition of Particles in Wintertime
    typeJournal Paper
    journal volume27
    journal issue5
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1988)027<0642:ECMOTD>2.0.CO;2
    journal fristpage642
    journal lastpage652
    treeJournal of Applied Meteorology:;1988:;volume( 027 ):;issue: 005
    contenttypeFulltext
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