@InProceedings{KouadioMachServ:2006:ReWeAf,
               author = "Kouadio, Yves K. and Machado, Luiz Augusto Toledo and Servain, 
                         Jacques",
          affiliation = "Instituto Nacional de Pesquisas Espaciais (INPE), Centro de 
                         Previs{\~a}o de Tempo e Estudos Clim{\'a}ticos (CPTEC) and 
                         Instituto Nacional de Pesquisas Espaciais (INPE), Centro de 
                         Previs{\~a}o de Tempo e Estudos Clim{\'a}ticos and 
                         {Funda{\c{c}}{\~a}o Cearence de Meteorologia e Recursos 
                         H{\'{\i}}dricos - FUNCEME}",
                title = "The relationship between west Africa mesoscale convective systems 
                         and hurricanes in the tropical atlantic during 2004",
            booktitle = "Proceedings...",
                 year = "2006",
         organization = "Congresso Brasileiro de Meteorologia, 14. (CBMET).",
            publisher = "SBMET",
             keywords = "sistemas convectivos, furac{\~o}ess, nuvens estratiformes.",
             abstract = "Este trabalho avalia a hip{\'o}tese de que os sistemas 
                         convectivos de mesoescala (MCS), iniciados no oeste de 
                         {\'A}frica, s{\~a}o potenciais geradores dos cyclones tropicais 
                         no Oceano Atl{\^a}ntico. Observou-se que existem MCS iniciados na 
                         Africa cuja as fases da dissipa{\c{c}}{\~a}o e/ou de madura 
                         est{\~a}o associados {\`a} gera{\c{c}}{\~a}o de ciclones 
                         tropicais. Estes MCS s{\~a}o iniciados na {\'A}frica Ocidental 
                         entre 7°N-15°N e na faixa 0-12°W e aparentemente, a grande 
                         extens{\~a}o de nuvens estratioformes favorecem o in{\'{\i}}cio 
                         de um ciclone tropical. Apresentamos tamb{\'e}m um exemplo destes 
                         MCS que destaca essa influ{\^e}ncia da regi{\~a}o estratiforme, 
                         na fase madura do MCS e na posterior forma{\c{c}}{\~a}o de um 
                         cyclone tropical. We study a possible link between the Mesoscale 
                         Convective Systems (MCS) initiated in West Africa and the 
                         generation of the tropical cyclones. We showed that there is MCS 
                         initiated in Africa and whose dissipation phase or the mature 
                         phase corresponds to the generation of the tropical cyclones. 
                         These MCS are initiated in West Africa between 7°N-15°N and the 
                         band 0-12°W. We present in the same way an example of these 
                         stratiforms clouds associated to an MCS, at the mature phase, and 
                         the further generation of a tropical cyclone.",
  conference-location = "Florian{\'o}polis, SC",
      conference-year = "Nov.27 - 01 Dec.",
           copyholder = "SID/SCD",
             language = "pt",
         organisation = "Coordenadora Geral do Congresso - Maria Gertrudes Alvarez Justi 
                         (presidente da SBMET)",
           targetfile = "Machado.Relationship.pdf",
        urlaccessdate = "25 abr. 2024"
}