@InProceedings{SutilPezzAlve:2017:AbNuAl,
               author = "Sutil, Ueslei Adriano and Pezzi, Luciano Ponzi and Alves, Rita de 
                         Cassia Marques",
          affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto 
                         Nacional de Pesquisas Espaciais (INPE)}",
                title = "Intera{\c{c}}{\~a}o oceano-atmosfera em um ciclone extratropical 
                         no Atl{\^a}ntico Sudoeste: uma abordagem num{\'e}rica em 
                         alt{\'{\i}}ssima resolu{\c{c}}{\~a}o",
            booktitle = "Anais...",
                 year = "2017",
               editor = "Gherardi, Douglas Francisco Marcolino and Arag{\~a}o, Luiz 
                         Eduardo Oliveira e Cruz de",
                pages = "5666--5673",
         organization = "Simp{\'o}sio Brasileiro de Sensoriamento Remoto, 18. (SBSR)",
            publisher = "Instituto Nacional de Pesquisas Espaciais (INPE)",
              address = "S{\~a}o Jos{\'e} dos Campos",
             abstract = "This present study shows an unpublished research about heat fluxes 
                         patterns of the ocean-atmosphere interaction processes during the 
                         passage of an extratropical cyclone in the Atlantic Southwest in 
                         02 to 05 of September 2006. The event created an intense storm 
                         surge in southern Brazils coast with a great horizontal 
                         displacement of the tide. A system of coupled regional models of 
                         the ocean and atmosphere (ROMS+WRF) and a regional atmospheric 
                         model (WRF) was used to simulate the extratropical cyclone event. 
                         A brief evaluation of the simulated output was made by comparing 
                         the simulated air temperature, wind speed and sea level pressure 
                         data with in situ (weather station) data. This comparison showed 
                         that both models have some bias (mainly wind), but the simulated 
                         output showed quite satisfactory results, allowing a good analysis 
                         of ocean-atmosphere interaction processes. The simulated thermal 
                         gradient increases the oceans heat fluxes to the atmosphere in the 
                         cold sector of the extratropical cyclone and, through the 
                         convergence of low levels winds, the humidity is transported to 
                         higher atmospheric levels, producing high amounts of water 
                         precipitation. The coupled system models showed a greater ability 
                         to simulate the intensity and trajectory of the extratropical 
                         cyclone, compared within the atmospheric model simulation.",
  conference-location = "Santos",
      conference-year = "28-31 maio 2017",
                 isbn = "978-85-17-00088-1",
                label = "59869",
             language = "pt",
         organisation = "Instituto Nacional de Pesquisas Espaciais (INPE)",
                  ibi = "8JMKD3MGP6W34M/3PSMBG8",
                  url = "http://urlib.net/ibi/8JMKD3MGP6W34M/3PSMBG8",
           targetfile = "59869.pdf",
                 type = "Oceanografia e sistemas costeiros",
        urlaccessdate = "27 abr. 2024"
}