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    Characteristics of the ITCZ over the Eastern Pacific, 5–8 June 1979

    Source: Monthly Weather Review:;1985:;volume( 113 ):;issue: 001::page 99
    Author:
    Fernandez-Paptagas, J.
    ,
    Estoque, M. A.
    DOI: 10.1175/1520-0493(1985)113<0099:COTIOT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The thermal and moisture structures of the ITCZ over the Eastern Pacific-Central American region have been studied during a selected four-day period in June 1979 (FGGE). Composite structures were constructed by using soundings gathered from dropwindsondes, tropical wind observing ships, and land stations. The composited temperature structure shows that the ITCZ is cold-cored at middle levels and warm-cored at upper levels. At low levels, there is neither a distinct maximum or a minimum in the ITCZ; instead, there is a gradual decrease in temperature as one crosses the ITCZ from north to south. The moisture shows that the ITCZ, as expected, is characterized by a maximum moisture content. The maximum dew-point depression differences between the ITCZ and the environment are found at middle levels. These composites indicate that the ITCZ structure over the Eastern Pacific-Central American region on 5?8 June 1979 is similar to that of the easterly wave. This similarity in structure suggests a corresponding similarity in energetics.
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      Characteristics of the ITCZ over the Eastern Pacific, 5–8 June 1979

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4201264
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    contributor authorFernandez-Paptagas, J.
    contributor authorEstoque, M. A.
    date accessioned2017-06-09T16:05:10Z
    date available2017-06-09T16:05:10Z
    date copyright1985/01/01
    date issued1985
    identifier issn0027-0644
    identifier otherams-60579.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4201264
    description abstractThe thermal and moisture structures of the ITCZ over the Eastern Pacific-Central American region have been studied during a selected four-day period in June 1979 (FGGE). Composite structures were constructed by using soundings gathered from dropwindsondes, tropical wind observing ships, and land stations. The composited temperature structure shows that the ITCZ is cold-cored at middle levels and warm-cored at upper levels. At low levels, there is neither a distinct maximum or a minimum in the ITCZ; instead, there is a gradual decrease in temperature as one crosses the ITCZ from north to south. The moisture shows that the ITCZ, as expected, is characterized by a maximum moisture content. The maximum dew-point depression differences between the ITCZ and the environment are found at middle levels. These composites indicate that the ITCZ structure over the Eastern Pacific-Central American region on 5?8 June 1979 is similar to that of the easterly wave. This similarity in structure suggests a corresponding similarity in energetics.
    publisherAmerican Meteorological Society
    titleCharacteristics of the ITCZ over the Eastern Pacific, 5–8 June 1979
    typeJournal Paper
    journal volume113
    journal issue1
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1985)113<0099:COTIOT>2.0.CO;2
    journal fristpage99
    journal lastpage105
    treeMonthly Weather Review:;1985:;volume( 113 ):;issue: 001
    contenttypeFulltext
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