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    Atmospheric Turbidity at Tucson, Arizona, 1956–83: Variations and Their Causes

    Source: Journal of Climate and Applied Meteorology:;1985:;Volume( 024 ):;Issue: 007::page 725
    Author:
    Szymber, R. J.
    ,
    Sellers, W. D.
    DOI: 10.1175/1520-0450(1985)024<0725:ATATAV>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Solar radiation data collected over the last 27 years at the University of Arizona have been analyzed to determine the major causes of time variations in the local turbidity of the atmosphere. The most extreme perturbations have been associated with significant volcanic eruptions, Agung on Bali in 1963 and, especially, El Chichón in Mexico in 1982. There is also evidence for a correlation of turbidity with local climatic factors and local smelter activity, but no detectable long-term upward or downward trend in turbidity has been observed. Routine pyrheliometric measurements were used to calculate monthly Linke turbidity factors for the period from June 1956 to June 1983 and related monthly aerosol values for the period from January 1977 to February 1983.
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      Atmospheric Turbidity at Tucson, Arizona, 1956–83: Variations and Their Causes

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4146036
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    contributor authorSzymber, R. J.
    contributor authorSellers, W. D.
    date accessioned2017-06-09T14:00:41Z
    date available2017-06-09T14:00:41Z
    date copyright1985/07/01
    date issued1985
    identifier issn0733-3021
    identifier otherams-10871.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146036
    description abstractSolar radiation data collected over the last 27 years at the University of Arizona have been analyzed to determine the major causes of time variations in the local turbidity of the atmosphere. The most extreme perturbations have been associated with significant volcanic eruptions, Agung on Bali in 1963 and, especially, El Chichón in Mexico in 1982. There is also evidence for a correlation of turbidity with local climatic factors and local smelter activity, but no detectable long-term upward or downward trend in turbidity has been observed. Routine pyrheliometric measurements were used to calculate monthly Linke turbidity factors for the period from June 1956 to June 1983 and related monthly aerosol values for the period from January 1977 to February 1983.
    publisherAmerican Meteorological Society
    titleAtmospheric Turbidity at Tucson, Arizona, 1956–83: Variations and Their Causes
    typeJournal Paper
    journal volume24
    journal issue7
    journal titleJournal of Climate and Applied Meteorology
    identifier doi10.1175/1520-0450(1985)024<0725:ATATAV>2.0.CO;2
    journal fristpage725
    journal lastpage734
    treeJournal of Climate and Applied Meteorology:;1985:;Volume( 024 ):;Issue: 007
    contenttypeFulltext
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