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    Effects of the El Chichón Volcanic Cloud on Solar Radiation Received at Fairbanks, Alaska

    Source: Bulletin of the American Meteorological Society:;1984:;volume( 065 ):;issue: 003::page 216
    Author:
    Wendler, Gerd
    DOI: 10.1175/1520-0477(1984)065<0216:EOTECV>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Detailed insulation measurements have been carried out in Fairbanks for the last four years. Beginning on 15 November 1982, these measurements showed substantial changes, believed to be due to the dust cloud of El Chichón. The volcano, situated in Mexico, erupted most intensely on 4 April 1982, putting a large amount of material into the atmosphere. The long travelling time to the North is in line with results found by Rao and Bradley (1983). Compared to clear-day data for previous years, clear days for the time period 15 November 1982?31 May 1983 showed a decrease in the direct beam of24.8%, an increase in the ratio of diffuse to global radiation of 76%, and a decrease in the global radiation of about 5%. A decrease in the direct beam, a substantial increase in the diffuse radiation, and a small decrease in the global radiation are typical for increased turbidity of the atmosphere, but the volcanic cloud caused changes greater than those due to "normal" turbidity changes.
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      Effects of the El Chichón Volcanic Cloud on Solar Radiation Received at Fairbanks, Alaska

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4160704
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    contributor authorWendler, Gerd
    date accessioned2017-06-09T14:40:09Z
    date available2017-06-09T14:40:09Z
    date copyright1984/03/01
    date issued1984
    identifier issn0003-0007
    identifier otherams-24072.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4160704
    description abstractDetailed insulation measurements have been carried out in Fairbanks for the last four years. Beginning on 15 November 1982, these measurements showed substantial changes, believed to be due to the dust cloud of El Chichón. The volcano, situated in Mexico, erupted most intensely on 4 April 1982, putting a large amount of material into the atmosphere. The long travelling time to the North is in line with results found by Rao and Bradley (1983). Compared to clear-day data for previous years, clear days for the time period 15 November 1982?31 May 1983 showed a decrease in the direct beam of24.8%, an increase in the ratio of diffuse to global radiation of 76%, and a decrease in the global radiation of about 5%. A decrease in the direct beam, a substantial increase in the diffuse radiation, and a small decrease in the global radiation are typical for increased turbidity of the atmosphere, but the volcanic cloud caused changes greater than those due to "normal" turbidity changes.
    publisherAmerican Meteorological Society
    titleEffects of the El Chichón Volcanic Cloud on Solar Radiation Received at Fairbanks, Alaska
    typeJournal Paper
    journal volume65
    journal issue3
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/1520-0477(1984)065<0216:EOTECV>2.0.CO;2
    journal fristpage216
    journal lastpage218
    treeBulletin of the American Meteorological Society:;1984:;volume( 065 ):;issue: 003
    contenttypeFulltext
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