@Article{SellersDRBFBGDMNSFH:1997:MoExEn,
               author = "Sellers, P. J. and Dickinson, R. E. and Randall, D. A. and Betts, 
                         A. K. and F. G., Hall and Berry, J. A. and Gollatz, G. J. and 
                         Denning, A. S. and Mooney, H. A. and Nobre, Carlos Afonso and 
                         Sato, N. and Field, C. B. and HendersonSellers, A.",
                title = "Modeling the exchanges of energy, water, and carbon between 
                         continents and the atmosphere",
              journal = "Science",
                 year = "1997",
               volume = "275",
               number = "5299",
                pages = "502--509",
                month = "Jan.",
             keywords = "ESTUDO DO TEMPO E DO CLIMA, General circulation model, simple 
                         biosphere model, land-surface, climate models, tropical 
                         deforestation, stomatal conductance, Amazonian deforestation, 
                         canopy reflectance, July circulation, regional climate.",
             abstract = "Atmospheric general circulation models used for climate simulation 
                         and weather forecasting require the fluxes of radiation, heat, 
                         water vapor, and momentum across the land-atmosphere interlace to 
                         be specified. These fluxes are calculated by submodels called land 
                         surface parameterizations. Over the last 20 years, these 
                         parameterizations have evolved from sim pie, unrealistic schemes 
                         into credible representations of the global 
                         soil-vegetation-atmosphere transfer system as advances in plant 
                         physiological and hydrological research, advances in satellite 
                         data interpretation, and the results of large-scale field 
                         experiments have been exploited. Some modem schemes incorporate 
                         biogeochemical and ecological knowledge and, when coupled with 
                         advanced climate and ocean models, will be capable of modeling the 
                         biological and physical responses of the Earth system to global 
                         change, for example, increasing atmospheric carbon dioxide.",
           copyholder = "SID/SCD",
                 issn = "0036-8075 and 1095-9203",
                label = "10162",
           targetfile = "sellers_modeling.pdf",
        urlaccessdate = "20 maio 2024"
}