@InProceedings{CarvalhoCabrFern:2003:CoOCa,
               author = "Carvalho, Gustavo de Ara{\'u}jo and Cabral, Alexandre Pereira and 
                         Fernandez, Marcos Ant{\^o}nio dos Santos",
          affiliation = "Oceansat and {Oceansat. Universidade do Estado do Rio de Janeiro 
                         (UERJ). Departamento de Oceanografia e Hidrologia.} and 
                         {Universidade do Estado do Rio de Janeiro (UERJ). Departamento de 
                         Oceanografia e Hidrologia.}",
                title = "Correla{\c{c}}{\~a}o entre o campo de vento m{\'e}dio e um 
                         {\'{\i}}ndice que define a intensidade da ressurg{\^e}ncia na 
                         regi{\~a}o do Cabo Frio (23ºS / 42ºW) atrav{\'e}s da 
                         an{\'a}lise de dados orbitais (QUIKSCAT / AVHRR)",
            booktitle = "Anais...",
                 year = "2003",
               editor = "Epiphanio, Jos{\'e} Carlos Neves and Fonseca, Leila Maria 
                         Garcia",
                pages = "1509--1514",
         organization = "Simp{\'o}sio Brasileiro de Sensoriamento Remoto, 11. (SBSR).",
            publisher = "INPE",
              address = "S{\~a}o Jos{\'e} dos Campos",
             keywords = "upwelling intensity, sea surface temperature, AVHRR, wind, 
                         QUIKSCAT, Cabo Frio (23ºS/42ºW).",
             abstract = "The aim of this study is to analyze the wind influence on the 
                         oceanic surface circulation over Cabo Frio (23ºS/42ºW) adjacent 
                         region and the presence of the upwelling phenomena scenery during 
                         2001 austral summer. A simple index (ITR) to classify the 
                         upwelling intensity was established through orbital Sea Surface 
                         Temperature data from AVHRR sensor, regarding upwelling area and 
                         SST it self. This index was correlated (Spearman) to local wind 
                         field average intensity and direction (QUIKSCAT), as well as to 
                         the wind components (parallel and longitudinal to the coastline). 
                         The preliminary results indicate that the upwelling intensity 
                         index (ITR) has significant correlation to the wind intensity and 
                         parallel wind component, with 12 and 24 hours before each 
                         upwelling condition. The wind direction and longitudinal wind 
                         component did not show statistical correlation to ITR.",
  conference-location = "Belo Horizonte",
      conference-year = "5-10 abr. 2003",
                 isbn = "85-17-00017-X",
             language = "pt",
         organisation = "Instituto Nacional de Pesquisas Espaciais",
                  ibi = "ltid.inpe.br/sbsr/2002/11.18.01.27",
                  url = "http://urlib.net/ibi/ltid.inpe.br/sbsr/2002/11.18.01.27",
           targetfile = "13_366.pdf",
                 type = "Oceanografia e Gerenciamento Costeiro / Oceanography and Coastal 
                         Management",
        urlaccessdate = "10 maio 2024"
}