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    Surface Cyclogenesis over South America

    Source: Monthly Weather Review:;1990:;volume( 119 ):;issue: 005::page 1293
    Author:
    Gan, Manoel Alonso
    ,
    Rao, Vadlamudi Brahmananda
    DOI: 10.1175/1520-0493(1991)119<1293:SCOSA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The frequency of surface cyclogenesis over South America (approximately the area enclosed by 15°?50°S and 30°?90°W) has been calculated using, 10 years (1979?1988) of data. The frequency of cyclogenesis is more in winter than in any other season. Highest frequency (139) is found in the month of May and the lowest frequency (71) is found in the month of December. In addition to seasonal, the frequency of cyclogenesis shows interannual variation. The occurrence of cyclogenesis is more during the years of negative Southern Oscillation index (El Niño years) and less during the years of positive Southern Oscillation index. The years of higher (lower) cyclogenesis are found to be associated with higher (lower) rainfall. This explains the negative correlation between the precipitation over southern Brazil and the Southern Oscillation index.
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      Surface Cyclogenesis over South America

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4202610
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    • Monthly Weather Review

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    contributor authorGan, Manoel Alonso
    contributor authorRao, Vadlamudi Brahmananda
    date accessioned2017-06-09T16:08:17Z
    date available2017-06-09T16:08:17Z
    date copyright1991/05/01
    date issued1990
    identifier issn0027-0644
    identifier otherams-61791.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4202610
    description abstractThe frequency of surface cyclogenesis over South America (approximately the area enclosed by 15°?50°S and 30°?90°W) has been calculated using, 10 years (1979?1988) of data. The frequency of cyclogenesis is more in winter than in any other season. Highest frequency (139) is found in the month of May and the lowest frequency (71) is found in the month of December. In addition to seasonal, the frequency of cyclogenesis shows interannual variation. The occurrence of cyclogenesis is more during the years of negative Southern Oscillation index (El Niño years) and less during the years of positive Southern Oscillation index. The years of higher (lower) cyclogenesis are found to be associated with higher (lower) rainfall. This explains the negative correlation between the precipitation over southern Brazil and the Southern Oscillation index.
    publisherAmerican Meteorological Society
    titleSurface Cyclogenesis over South America
    typeJournal Paper
    journal volume119
    journal issue5
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1991)119<1293:SCOSA>2.0.CO;2
    journal fristpage1293
    journal lastpage1302
    treeMonthly Weather Review:;1990:;volume( 119 ):;issue: 005
    contenttypeFulltext
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