@Article{SouzaAlveNobr:1998:AnPrSe,
               author = "Souza, Everaldo B. de and Alves, Jos{\'e} Maria Brabo and Nobre, 
                         Paulo",
                title = "Anomalias de precipita{\c{c}}{\~a}o nos setores norte e leste do 
                         nordeste brasileiro em associac{\~a}o aos eventos do padr{\~a}o 
                         de dipolo observados na bacia do atlantico tropical",
              journal = "Revista Brasileira de Meteorologia",
                 year = "1998",
               volume = "13",
               number = "2",
                pages = "45--55",
             abstract = "The spatial configuration of the precipitation anomalies during 
                         pre-rainy-season and rain) {"} .. .r-- . . .. i . 1 1 1 tne 
                         nortnern ana eastern sectors or tne NEB is invesrigarea oy 
                         composires anaiyses caiculated for Dipole Pattern events observed 
                         over Tropical Atlantic. In particular, the pre- to rainy-season 
                         months, during the positive phase of Dipole (warm SST anomalies 
                         over North Basin and cold SST anomalies over South Atlantic Basin) 
                         are associated with manifestations of precipitation below normal 
                         in most states that composed the northern and eastern (except 
                         Sergipe, Alagoas e Bahia) sectors of NEB. On the other hand, 
                         during the negative phase of Dipole (cold SST anomalies over North 
                         Basin and warm SST anomalies over South Atlantic Basin) it was 
                         observed a widespread of precipitation above normal in entire NEB. 
                         In the negative phase, the region containing TSM22g°C (favorable 
                         to deep convection) and the confluence axis of the meridional wind 
                         at surface, positioning in the South Equatorial Atlantic, forined 
                         the proinising conditions that sustaining ITCZ over south of the 
                         equator (explaining the precipitation above normal observed in the 
                         NEB). However, during the positive phase, these conditions was 
                         observed over North Equatorial Atlantic and the ITCZ stayed 
                         anchoraged in the north of the equator (explaining the 
                         precipitation below of normal observ.",
                 issn = "0102-7786",
                label = "self-archiving-INPE-MCTI-GOV-BR",
             language = "pt",
           targetfile = "rbmet98v13n2p45-55.pdf",
        urlaccessdate = "21 maio 2024"
}