@InProceedings{CarvalhoMarLobBarNov:2017:CaLaGr,
               author = "Carvalho, Lino Augusto Sander de and Martins, Vitor Souza and 
                         Lobo, Felipe de Lucia and Barbosa, Cl{\'a}udio Clemente Faria and 
                         Novo, Evlyn M{\'a}rcia Le{\~a}o de Moraes",
          affiliation = "{} and {} and {} and {Instituto Nacional de Pesquisas Espaciais 
                         (INPE)} and {Instituto Nacional de Pesquisas Espaciais (INPE)}",
                title = "Investigating empirical models to retrieve the backscattering 
                         slope from Landsat 8 Images - The case of Lago Grande Curuai",
            booktitle = "Anais...",
                 year = "2017",
               editor = "Gherardi, Douglas Francisco Marcolino and Arag{\~a}o, Luiz 
                         Eduardo Oliveira e Cruz de",
                pages = "2067--2074",
         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 paper aims on the investigation of well-established models to 
                         retrieve the backscattering slope \γbbp from remote sensing 
                         images applied to a particular Amazon floodplain lake, named 
                         Curuai Lake. Lee, Carder e Arnone (2002) \γbbp model and its 
                         derivation, Pan et al. (2015) model, were applied to measured 
                         Remote Sensing Reflectance and retrieved bbp was compared to 
                         measured bbp taken in two distinct hydrological periods: receding 
                         and rising water periods (August 2013 and April 2014). Also, an 
                         empirical model, based on Lee, Carder e Arnone (2002) approach, 
                         was derived from a nonlinear fittingto the measured dataset, 
                         considering only Landsat 8 bands combination. Lee, Carder e Arnone 
                         (2002)and Pan et al. (2015) models were not suitable to retrieve 
                         backscattering slope in Curuai Lake whistthe empirical model using 
                         bands B4(655)/B5(865) presented the best result considering both 
                         hydrologicalperiods and was therefore applied to Landsat 8 images 
                         acquired in August 2013 and April 2014. Thequalitative inspection 
                         of both images reveal consistent backscattering slope retrievals 
                         which, with furtheranalysis, could lead to a suitable proxy for 
                         particle size in Curuai Lake.",
  conference-location = "Santos",
      conference-year = "28-31 maio 2017",
                 isbn = "978-85-17-00088-1",
                label = "59254",
             language = "en",
         organisation = "Instituto Nacional de Pesquisas Espaciais (INPE)",
                  ibi = "8JMKD3MGP6W34M/3PSLPT6",
                  url = "http://urlib.net/ibi/8JMKD3MGP6W34M/3PSLPT6",
           targetfile = "59254.pdf",
                 type = "Sensoriamento remoto de {\'a}guas interiores",
        urlaccessdate = "27 abr. 2024"
}