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    A Note on the Mt. Saint Helens Volcanic Eruption

    Source: Monthly Weather Review:;1981:;volume( 109 ):;issue: 005::page 1103
    Author:
    Edman, Delain A.
    ,
    Selin, Richard
    DOI: 10.1175/1520-0493(1981)109<1103:ANOTMS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The violent eruption of the Mt. Saint Helens volcano on 18 May 1980 was examined using GOES-EAST satellite imagery. The University of Wisconsin McIDAS system was used to display the imagery and derive a number of plume measurements?including the plume's area, temperature, speed and an estimate of plume height. A thickening of the surrounding cirrus shield was observed (believed to be associated with gravity wave activity) as well as two distinct phases of volcanic activity that occurred during the eruption. A comparison of the Mt. Saint Helens eruption to the 1979 Soufriere eruptions revealed that the Mt. Saint Helens volcanic eruption produced a much larger plume, indicative of a more violent eruption. It is also shown that the height of the plume could not be reliably extracted from the infrared data due to the low tropopause in the vicinity of the volcano.
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      A Note on the Mt. Saint Helens Volcanic Eruption

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4200492
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    contributor authorEdman, Delain A.
    contributor authorSelin, Richard
    date accessioned2017-06-09T16:03:25Z
    date available2017-06-09T16:03:25Z
    date copyright1981/05/01
    date issued1981
    identifier issn0027-0644
    identifier otherams-59885.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4200492
    description abstractThe violent eruption of the Mt. Saint Helens volcano on 18 May 1980 was examined using GOES-EAST satellite imagery. The University of Wisconsin McIDAS system was used to display the imagery and derive a number of plume measurements?including the plume's area, temperature, speed and an estimate of plume height. A thickening of the surrounding cirrus shield was observed (believed to be associated with gravity wave activity) as well as two distinct phases of volcanic activity that occurred during the eruption. A comparison of the Mt. Saint Helens eruption to the 1979 Soufriere eruptions revealed that the Mt. Saint Helens volcanic eruption produced a much larger plume, indicative of a more violent eruption. It is also shown that the height of the plume could not be reliably extracted from the infrared data due to the low tropopause in the vicinity of the volcano.
    publisherAmerican Meteorological Society
    titleA Note on the Mt. Saint Helens Volcanic Eruption
    typeJournal Paper
    journal volume109
    journal issue5
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1981)109<1103:ANOTMS>2.0.CO;2
    journal fristpage1103
    journal lastpage1110
    treeMonthly Weather Review:;1981:;volume( 109 ):;issue: 005
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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