@InProceedings{GiarollaCampDiasCama:2000:VaNiMa,
               author = "Giarolla, Emanuel and Campos, Edmo J. D. and Dias, Pedro L. S. and 
                         Camargo, Ricardo de",
          affiliation = "{Centro de Previsao de Tempo e Estudos Climaticos - CPTEC/INPE} 
                         and {Departamento de Oceanografia F{\'{\i}}sica / Instituto 
                         Oceanogr{\'a}fico da USP} and {Departamento de Ci{\^e}ncias 
                         Atmosf{\'e}ricas / Instituto Astron{\^o}mico e 
                         Geof{\'{\i}}sico da USP}",
                title = "Variabilidade no nivel do mar no atlantico ocidental Sul causada 
                         por mecanismos internos e pela passagem de ciclones atmosfericos",
            booktitle = "Anais...",
                 year = "2000",
                pages = "2655--2662",
         organization = "Congresso Brasileiro de Meteorologia, 11.",
             keywords = "variabilidade, meteorologia.",
             abstract = "The Miami Isopycnic Coordinate Ocean Model (MICOM) was used to 
                         study the sea surface elevation variability in the Southwestern 
                         Atlantic, caused by internal mechanisms (basically eddies 
                         influence) and by an atmospheric cyclone passage over the ocean. 
                         Considering the variability due to internal mechanisms, in the 
                         Brazil-Malvinas Confluence zone, the displacement of the zero 
                         elevation line (the approximated confluence position) reached over 
                         2.5 latitude degrees, caused mainly by eddy activity. Considering 
                         the effects due to atmospheric cyclones passage, two experiments 
                         were carried out, the first one with a 5 degree radius cyclone and 
                         the other one considering a cyclone with a half of this radius. 
                         The smaller cyclone perturbs a smaller area, but this perturbation 
                         last much longer than those produced by the large one. The waves 
                         generated in the adjustment process propagate energy to the west, 
                         and it can be seen that part of this energy is trapped near the 
                         continent when waves reflect on the coast, an additional energy 
                         input to the confluence variability.",
  conference-location = "Rio de Janeiro (RJ)",
      conference-year = "16-20 out. 2000",
           copyholder = "SID/SCD",
             language = "pt",
         organisation = "SBMET",
           targetfile = "Giarolla_Variabilidade do nivel.pdf",
                 type = "PRE",
        urlaccessdate = "15 jun. 2024"
}