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    Environmental Conditions Associated with Amazonian Squall Lines: A Case Study

    Source: Monthly Weather Review:;1995:;volume( 123 ):;issue: 011::page 3163
    Author:
    Cohen, Júlia C. P.
    ,
    Silva Dias, Maria A. F.
    ,
    Nobre, Carlos A.
    DOI: 10.1175/1520-0493(1995)123<3163:ECAWAS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The environmental conditions associated with squall lines (SL) that were observed during the period of 13 April?13 May 1987 (GTE/ABLE-2B) originating at the northern coast of South America and propagating over the Amazon Basin are documented. The SL observed on 5?7 May are examined in more detail. The SL days had in common a stronger and deeper low-level jet when compared with the days without SL. Two possible explanations are found for the intensification of the low-level jet: propagating easterly waves in the tropical Atlantic, which eventually reach Manaus, and localized heat sources in the western Amazon. Both were observed on 5?6 May. It is suggested that numerical simulations should be performed to unravel the relative importance of each large-scale mechanism.
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      Environmental Conditions Associated with Amazonian Squall Lines: A Case Study

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4203535
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    contributor authorCohen, Júlia C. P.
    contributor authorSilva Dias, Maria A. F.
    contributor authorNobre, Carlos A.
    date accessioned2017-06-09T16:10:32Z
    date available2017-06-09T16:10:32Z
    date copyright1995/11/01
    date issued1995
    identifier issn0027-0644
    identifier otherams-62622.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4203535
    description abstractThe environmental conditions associated with squall lines (SL) that were observed during the period of 13 April?13 May 1987 (GTE/ABLE-2B) originating at the northern coast of South America and propagating over the Amazon Basin are documented. The SL observed on 5?7 May are examined in more detail. The SL days had in common a stronger and deeper low-level jet when compared with the days without SL. Two possible explanations are found for the intensification of the low-level jet: propagating easterly waves in the tropical Atlantic, which eventually reach Manaus, and localized heat sources in the western Amazon. Both were observed on 5?6 May. It is suggested that numerical simulations should be performed to unravel the relative importance of each large-scale mechanism.
    publisherAmerican Meteorological Society
    titleEnvironmental Conditions Associated with Amazonian Squall Lines: A Case Study
    typeJournal Paper
    journal volume123
    journal issue11
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1995)123<3163:ECAWAS>2.0.CO;2
    journal fristpage3163
    journal lastpage3174
    treeMonthly Weather Review:;1995:;volume( 123 ):;issue: 011
    contenttypeFulltext
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