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    Atmospheric Turbidity over the United States, 1961–1966

    Source: Journal of Applied Meteorology:;1969:;volume( 008 ):;issue: 006::page 955
    Author:
    Flowers, E. C.
    ,
    McCormick, R. A.
    ,
    Kurfis, K. R.
    DOI: 10.1175/1520-0450(1969)008<0955:ATOTUS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Five years of turbidity measurements from a network of stations in the United States are analyzed. Measurements are made with the Volz sunphotometer; the instrumentits calibration, and its use are described. The relationship of these measurements to those of Linke and Ångström is briefly discussed. Analysis of the data indicates the following: 1) an annual mean pattern of low turbidity (near 0.05) over the western plains and Rocky Mountains and high turbidity (near 0.14) in the east; 2) observed minimum turbidity near 0.02; 3) an annual cycle of low turbidity in winter and high in summer; 4) lowest turbidity in continental polar air masses and highest in maritime tropical; and 5) no noticeable lowering of turbidity following precipitation.
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      Atmospheric Turbidity over the United States, 1961–1966

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4221989
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    • Journal of Applied Meteorology

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    contributor authorFlowers, E. C.
    contributor authorMcCormick, R. A.
    contributor authorKurfis, K. R.
    date accessioned2017-06-09T17:05:29Z
    date available2017-06-09T17:05:29Z
    date copyright1969/12/01
    date issued1969
    identifier issn0021-8952
    identifier otherams-7923.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4221989
    description abstractFive years of turbidity measurements from a network of stations in the United States are analyzed. Measurements are made with the Volz sunphotometer; the instrumentits calibration, and its use are described. The relationship of these measurements to those of Linke and Ångström is briefly discussed. Analysis of the data indicates the following: 1) an annual mean pattern of low turbidity (near 0.05) over the western plains and Rocky Mountains and high turbidity (near 0.14) in the east; 2) observed minimum turbidity near 0.02; 3) an annual cycle of low turbidity in winter and high in summer; 4) lowest turbidity in continental polar air masses and highest in maritime tropical; and 5) no noticeable lowering of turbidity following precipitation.
    publisherAmerican Meteorological Society
    titleAtmospheric Turbidity over the United States, 1961–1966
    typeJournal Paper
    journal volume8
    journal issue6
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1969)008<0955:ATOTUS>2.0.CO;2
    journal fristpage955
    journal lastpage962
    treeJournal of Applied Meteorology:;1969:;volume( 008 ):;issue: 006
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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