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    A CHEMICAL TRACER EXPERIMENT IN OROGRAPHIC CLOUDS

    Source: Journal of Meteorology:;1956:;volume( 013 ):;issue: 006::page 548
    Author:
    Eber, Laurence E.
    ,
    Seely, Ben K.
    DOI: 10.1175/1520-0469(1956)013<0548:ACTEIO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: In the summer of 1954, and experiment was conducted on the Island of Maui, Territory of Hawaii, in which a chemical tracer technique was exployed to ?tag? water droplets sprayed into an orographic cloud from a site near the base of a large cliff, oriented normal to the trade winds. A sampling method was used which permitted the individual drops to be identified and their size measured when they fell to the ground downwind from the spray site. The object of the experiment was to obtain data on the growth and final size distribution of the droplets. Samples of the spray were obtained up to six miles downwind from the spray site, and the lateral boundaries of the spray plume were determined approximately. Sampling results were negative during conditions when moderate to heavy rain prevailed or, at the other extreme, when the orographic cloud was weakly developed. A tendency for increasing drop size with distance from the spray site was indicated by the data.
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      A CHEMICAL TRACER EXPERIMENT IN OROGRAPHIC CLOUDS

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4149858
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    contributor authorEber, Laurence E.
    contributor authorSeely, Ben K.
    date accessioned2017-06-09T14:11:34Z
    date available2017-06-09T14:11:34Z
    date copyright1956/12/01
    date issued1956
    identifier issn0095-9634
    identifier otherams-14310.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149858
    description abstractIn the summer of 1954, and experiment was conducted on the Island of Maui, Territory of Hawaii, in which a chemical tracer technique was exployed to ?tag? water droplets sprayed into an orographic cloud from a site near the base of a large cliff, oriented normal to the trade winds. A sampling method was used which permitted the individual drops to be identified and their size measured when they fell to the ground downwind from the spray site. The object of the experiment was to obtain data on the growth and final size distribution of the droplets. Samples of the spray were obtained up to six miles downwind from the spray site, and the lateral boundaries of the spray plume were determined approximately. Sampling results were negative during conditions when moderate to heavy rain prevailed or, at the other extreme, when the orographic cloud was weakly developed. A tendency for increasing drop size with distance from the spray site was indicated by the data.
    publisherAmerican Meteorological Society
    titleA CHEMICAL TRACER EXPERIMENT IN OROGRAPHIC CLOUDS
    typeJournal Paper
    journal volume13
    journal issue6
    journal titleJournal of Meteorology
    identifier doi10.1175/1520-0469(1956)013<0548:ACTEIO>2.0.CO;2
    journal fristpage548
    journal lastpage553
    treeJournal of Meteorology:;1956:;volume( 013 ):;issue: 006
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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