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@InProceedings{VeigaMareVadl:2000:InAnTS,
               author = "Veiga, Jose Augusto Paixao and Marengo, Jose Antonio and 
                         Vadlamudi, Brahmananda Rao",
          affiliation = "{Centro de Previs{\~a}o do Tempo e Estudos Clim{\'a}ticos - 
                         CPTEC/INPE}",
                title = "A influencia das anomalias de TSM dos oceano Pacifico e Atlantico 
                         sobre as chuvas de moncao da America do Sul",
            booktitle = "Anais...",
                 year = "2000",
                pages = "1020--1028",
         organization = "Congresso Brasileiro de Meteorologia, 11.",
            publisher = "SBMET",
             keywords = "climatologia.",
             abstract = "Monthly information of sea surface temperature (SST), and rainfall 
                         from 22 meteorological stations in eastern South America were used 
                         to identify the relation between rainfall characteristics of the 
                         South American Monsoon systems (SMAS) and the variability of SST 
                         over Pacific and Atlantic Oceans. The correlations between IMV and 
                         SST anomalies show that both Atlantic and Pacific affect the 
                         variability of rainfall on the region. In the Pacific, 4 areas 
                         that may exert some influence on the IMV were identified: Niņo 
                         3.4-Niņo 4, Chilean central coast, south central Pacific and the 
                         western Pacific off Northeast of Australia. On the Atlantic, the 
                         band of negative SST-rainfall correlations between 5° and 20° S 
                         can be explained throughout and intensification of the winds 
                         related to these SST anomalies, which entails a stronger moisture 
                         transport into the continent and thus an increment of rains on 
                         this area. In addition, an effect of convection and latent heat 
                         release in Amazonia combined with modifications in the 
                         intensity-location of the Bolivian high can also affect moisture 
                         transport from this region to the monsoon area, thus affecting the 
                         intensity of the summer rains on the monsoon area.",
  conference-location = "Rio de Janeiro (RJ)",
      conference-year = "16-20 out. 2000",
           copyholder = "SID/SCD",
             language = "pt",
           targetfile = "Veiga_A influencia das anomalias.pdf",
        urlaccessdate = "14 ago. 2020"
}


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