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    The Vertical Distribution of Cloud and Aitken Nuclei Downwind of Urban Pollution Sources

    Source: Journal of Applied Meteorology:;1972:;volume( 011 ):;issue: 001::page 141
    Author:
    Kocmond, W. C.
    ,
    Mack, E. J.
    DOI: 10.1175/1520-0450(1972)011<0141:TVDOCA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Simultaneous airborne observations of Aitken and cloud nuclei upwind and downwind of Buffalo, N.Y., were made in an effort to determine the effects of air pollution on condensation nucleus concentration. The data show significant increases over background concentrations of both Aitken and cloud nuclei (at 0.3% supersaturation) immediately downwind of pollution sources, and, also, that a secondary maximum in cloud nucleus concentration usually occurs about 10?15 mi farther downwind. In spite of these large increases in the total number of nuclei downwind of an industrial-urban complex such as the Niagara Frontier, the concentration of cloud and Aitken particulates approaches upwind background levels within 20?50 mi of the sources. Attempts to define the role (if any) of air pollution in cloud microstructure were confined to a single set of airborne observations. The limited drop-size distribution and cloud nucleus data were not sufficient to justify firm conclusions, and additional measurements are recommended.
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      The Vertical Distribution of Cloud and Aitken Nuclei Downwind of Urban Pollution Sources

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4226212
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    contributor authorKocmond, W. C.
    contributor authorMack, E. J.
    date accessioned2017-06-09T17:18:56Z
    date available2017-06-09T17:18:56Z
    date copyright1972/02/01
    date issued1972
    identifier issn0021-8952
    identifier otherams-8303.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4226212
    description abstractSimultaneous airborne observations of Aitken and cloud nuclei upwind and downwind of Buffalo, N.Y., were made in an effort to determine the effects of air pollution on condensation nucleus concentration. The data show significant increases over background concentrations of both Aitken and cloud nuclei (at 0.3% supersaturation) immediately downwind of pollution sources, and, also, that a secondary maximum in cloud nucleus concentration usually occurs about 10?15 mi farther downwind. In spite of these large increases in the total number of nuclei downwind of an industrial-urban complex such as the Niagara Frontier, the concentration of cloud and Aitken particulates approaches upwind background levels within 20?50 mi of the sources. Attempts to define the role (if any) of air pollution in cloud microstructure were confined to a single set of airborne observations. The limited drop-size distribution and cloud nucleus data were not sufficient to justify firm conclusions, and additional measurements are recommended.
    publisherAmerican Meteorological Society
    titleThe Vertical Distribution of Cloud and Aitken Nuclei Downwind of Urban Pollution Sources
    typeJournal Paper
    journal volume11
    journal issue1
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1972)011<0141:TVDOCA>2.0.CO;2
    journal fristpage141
    journal lastpage148
    treeJournal of Applied Meteorology:;1972:;volume( 011 ):;issue: 001
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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