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    Aerosol Extinction at 500 nm in Urban and Rural Air at Milwaukee in April 1976

    Source: Journal of Applied Meteorology:;1979:;volume( 018 ):;issue: 002::page 105
    Author:
    Bridgman, Howard A.
    DOI: 10.1175/1520-0450(1979)018<0105:AEANIU>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Aircraft measurements of aerosol size distributions were used to calculate aerosol extinction coefficients at 12 flight altitudes over an urban and a rural site at Milwaukee. Analysis of vertical-horizontal cross sections from four days of measurement in April 1976 indicated a well-defined influence of the urban area, creating higher aerosol extinction coefficients depending on the meteorological situation. On three of the four days, extinction coefficients decreased markedly above an inversion, where the air was much drier and cleaner. On 12 April, onshore flow below 625 m altitude prevented aerosols from moving over Lake Michigan, and the shoreline was sharply delineated. Westerly flow on the other three days created no such lake-city distinction. Comparison of the most polluted day with the other three days indicated that day-to-day variations in aerosol extinction may be greater than urban-rural differences.
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      Aerosol Extinction at 500 nm in Urban and Rural Air at Milwaukee in April 1976

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4233148
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    contributor authorBridgman, Howard A.
    date accessioned2017-06-09T17:39:51Z
    date available2017-06-09T17:39:51Z
    date copyright1979/02/01
    date issued1979
    identifier issn0021-8952
    identifier otherams-9638.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4233148
    description abstractAircraft measurements of aerosol size distributions were used to calculate aerosol extinction coefficients at 12 flight altitudes over an urban and a rural site at Milwaukee. Analysis of vertical-horizontal cross sections from four days of measurement in April 1976 indicated a well-defined influence of the urban area, creating higher aerosol extinction coefficients depending on the meteorological situation. On three of the four days, extinction coefficients decreased markedly above an inversion, where the air was much drier and cleaner. On 12 April, onshore flow below 625 m altitude prevented aerosols from moving over Lake Michigan, and the shoreline was sharply delineated. Westerly flow on the other three days created no such lake-city distinction. Comparison of the most polluted day with the other three days indicated that day-to-day variations in aerosol extinction may be greater than urban-rural differences.
    publisherAmerican Meteorological Society
    titleAerosol Extinction at 500 nm in Urban and Rural Air at Milwaukee in April 1976
    typeJournal Paper
    journal volume18
    journal issue2
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1979)018<0105:AEANIU>2.0.CO;2
    journal fristpage105
    journal lastpage116
    treeJournal of Applied Meteorology:;1979:;volume( 018 ):;issue: 002
    contenttypeFulltext
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