@InProceedings{GouveiaCamDiaGhePez:2015:CoDaTe,
               author = "Gouveia, Mainara Biazati and Campos, Paula Costa and Dias, Daniela 
                         Faggiani and Gherardi, Douglas Francisco Marcolino and Pezzi, 
                         Luciano Ponzi",
          affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {} and 
                         {Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto 
                         Nacional de Pesquisas Espaciais (INPE)} and {Instituto Nacional de 
                         Pesquisas Espaciais (INPE)}",
                title = "Compara{\c{c}}{\~a}o entre os dados de temperatura da 
                         superf{\'{\i}}cie do mar do SODA 2.0.4, 2.2.4 e do AVHRR",
            booktitle = "Anais...",
                 year = "2015",
               editor = "Gherardi, Douglas Francisco Marcolino and Arag{\~a}o, Luiz 
                         Eduardo Oliveira e Cruz de",
                pages = "7595--7602",
         organization = "Simp{\'o}sio Brasileiro de Sensoriamento Remoto, 17. (SBSR)",
            publisher = "Instituto Nacional de Pesquisas Espaciais (INPE)",
              address = "S{\~a}o Jos{\'e} dos Campos",
             abstract = "Data from Simple Ocean Data Assimilation (SODA) data base are used 
                         as initial and boundary conditions in hydrodynamical numerical 
                         simulations. These data are validated using remote sensing 
                         microwave or infrared thermal data from radiometers, such as SST 
                         data obtained by the Advanced Very High Resolution Radiometer 
                         (AVHRR), from Pathfinder (NOAA). This study reveals the 
                         differences between two SODA reanalysis data bases. AVHRR SST data 
                         from 1982 to 2007 are used to support these analysis, in the 
                         Southwestern Atlantic Shelf (SWAS) region. AVHRR SST data shows 
                         the main ocean surface processes which occur in the continental 
                         shelf and slope of the study area. Summer SST data (January-March) 
                         from SODA v. 2.0.4 better represent SWAS seasonal variability and 
                         the Cape Frio (CF) upwelling, while the winter (June to August) 
                         northward intrusion of coastal water, reaching Cape Santa Marta 
                         (CSM), was better identified in SST data from SODA v.2.2.4. We 
                         enphasize the importance of such differences, which may interfere 
                         in numerical simulations performed using SODA reanalysis as 
                         initial and boundary conditions.",
  conference-location = "Jo{\~a}o Pessoa",
      conference-year = "25-29 abr. 2015",
                 isbn = "978-85-17-0076-8",
                label = "1748",
             language = "pt",
         organisation = "Instituto Nacional de Pesquisas Espaciais (INPE)",
                  ibi = "8JMKD3MGP6W34M/3JM4K92",
                  url = "http://urlib.net/ibi/8JMKD3MGP6W34M/3JM4K92",
           targetfile = "p1748.pdf",
                 type = "Sensoriamento remoto de microondas",
        urlaccessdate = "27 abr. 2024"
}