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    Water Vapor Characteristics over Northeast Brazil during Two Contrasting Years

    Source: Journal of Climate and Applied Meteorology:;1984:;volume( 023 ):;issue: 003::page 440
    Author:
    Brahmananda Rao, Vadlamudi
    ,
    Da Silva Marques, Valdo
    DOI: 10.1175/1520-0450(1984)023<0440:WVCONB>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Water vapor characteristics over northeast Brazil for two contrasting years are discussed. During the wet year 1974, the precipitation efficiencies were less than 20% over the interior dry region and during the dry year 1976, they were reduced to 10% or less. The reduction is mainly due to low precipitation in 1976. Calculation of water vapor flux showed that in both wet and dry years, the flux is inward in the east sector and outward in the west sector. This suggests the importance of the South Atlantic Ocean in providing water vapor for NE Brazil. During the wet year, the lower tropospheric flow is convergent and in the northwest part, the direction of flow is more northerly/less southerly. During the dry year the opposite occurred. This indicates the possible role of the Intertropical Convergence Zone in the interannual variations of climate over NE Brazil.
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      Water Vapor Characteristics over Northeast Brazil during Two Contrasting Years

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4145826
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    contributor authorBrahmananda Rao, Vadlamudi
    contributor authorDa Silva Marques, Valdo
    date accessioned2017-06-09T14:00:04Z
    date available2017-06-09T14:00:04Z
    date copyright1984/03/01
    date issued1984
    identifier issn0733-3021
    identifier otherams-10682.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145826
    description abstractWater vapor characteristics over northeast Brazil for two contrasting years are discussed. During the wet year 1974, the precipitation efficiencies were less than 20% over the interior dry region and during the dry year 1976, they were reduced to 10% or less. The reduction is mainly due to low precipitation in 1976. Calculation of water vapor flux showed that in both wet and dry years, the flux is inward in the east sector and outward in the west sector. This suggests the importance of the South Atlantic Ocean in providing water vapor for NE Brazil. During the wet year, the lower tropospheric flow is convergent and in the northwest part, the direction of flow is more northerly/less southerly. During the dry year the opposite occurred. This indicates the possible role of the Intertropical Convergence Zone in the interannual variations of climate over NE Brazil.
    publisherAmerican Meteorological Society
    titleWater Vapor Characteristics over Northeast Brazil during Two Contrasting Years
    typeJournal Paper
    journal volume23
    journal issue3
    journal titleJournal of Climate and Applied Meteorology
    identifier doi10.1175/1520-0450(1984)023<0440:WVCONB>2.0.CO;2
    journal fristpage440
    journal lastpage444
    treeJournal of Climate and Applied Meteorology:;1984:;volume( 023 ):;issue: 003
    contenttypeFulltext
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