@Article{MartanoMarqSá:2015:LaTrPa,
               author = "Martano, Paolo and Marques Filho, Edson Pereira and S{\'a}, 
                         Leonardo Deane de Abreu",
          affiliation = "{Istituto di Scienze dell’Atmosfera e del Clima} and {Universidade 
                         Federal da Bahia (UFBA)} and {Instituto Nacional de Pesquisas 
                         Espaciais (INPE)}",
                title = "Land-atmosphere transfer parameters in the Brazilian Pantanal 
                         during the dry season",
              journal = "Atmosphere",
                 year = "2015",
               volume = "6",
                pages = "805--821",
             keywords = "Pantanal, roughness length, displacement length, similarity 
                         relations, nonlinear regression, Penman–Monteith equation.",
             abstract = "The Brazilian region of Pantanal is one of the largest wetlands in 
                         the world, characterized by a wet season, in which it is covered 
                         by a shallow water layer, and a dry season, in which the water 
                         layer disappears. The aim of this study is the estimation of the 
                         main parameters (drag coefficients and surface scale lengths) 
                         involved in modelling the surface atmosphere transfer of momentum, 
                         heat and water vapor from the dataset of the second 
                         Interdisciplinary Pantanal Experiment (IPE2). The roughness 
                         parameters and the stability correction parameters have been 
                         estimated in the framework of the similarity theory for the 
                         vertical profiles of wind speed and temperature. Thus, a 
                         previously-developed methodology was adapted to the available 
                         dataset from the IPE2 five-level mast. The results are in 
                         reasonable agreement with the available literature. An attempt to 
                         obtain the scalar transfer parameters for water vapor has been 
                         performed by a PenmanMonteith approach using a two-component 
                         surface resistance in parallel between a vegetation and a bare 
                         soil part. The parameters of the model have been calibrated using 
                         a non-linear regression method. The scalar drag coefficient 
                         retrieved in this way is in agreement with that calculated by the 
                         flux-gradient approach for the sensible heat flux. Eventually, an 
                         evaluation of the vegetation contribution to the total vapor flux 
                         is given.",
                  doi = "10.3390/atmos6060805",
                  url = "http://dx.doi.org/10.3390/atmos6060805",
                 issn = "2073-4433",
             language = "en",
           targetfile = "Martano_Marques-Filho_\&_Sa_2015_atmosphere-06-00805.pdf",
        urlaccessdate = "27 abr. 2024"
}