@Misc{BrentKauSetTanWar:1991:OpPrAe,
               author = "Brent, N. H. and Kaufman, Y. I. and Setzer, Alberto Waingort and 
                         Tanre, D. D. and Ward, D. E.",
                title = "Optical properties of aerosol emissions from biomass burning in 
                         the tropics",
                 year = "1991",
         howpublished = "MIT Press",
                 city = "Cambridge",
             keywords = "ESTUDOS INTEGRADOS DO MEIO AMBIENTE, biomassa, fuma{\c{c}}a, 
                         aeross{\'o}is, desflorestamento, desmatamento, 
                         polui{\c{c}}{\~a}o ambiental, efeito estufa, biomass, aerosois, 
                         deforestation, environmental pollution, greenhouse effect, 
                         smoke.",
           targetfile = "INPE 8033.pdf",
             abstract = "The optical properties of smoke aerosol are discussed in the 
                         general context of biomass burning. Biomass burning in the 
                         tropics, a large source of trace gases, has expanded drastically 
                         in the last decade due to increases in the controlled and 
                         uncontrolled deforestation in South America (Tucker et al., 1984 
                         Malingreau and Tucker, 1988; Setzer et al., 1988; Setzer and 
                         Pereira, 1989)and due to increases in cultivated areas associated 
                         with expansion of population in Africa and South America (Seiler 
                         and Crutzen, 1980). Trace gases and particulates are emitted to 
                         the atmosphere from the burning process. The biomass burning 
                         process is linked to the need to understand the sources and sinks 
                         of the atmospheric trace gases and their atmospheric variations 
                         (GTC, 1986). The importance of these trace gases (in addition to 
                         C02)is in their greenhouse effect, which is comparable to that of 
                         C02 (Ramanathan et al., 1985), and in their effect on tropospheric 
                         chemistry (Crutzen, 1988).",
          affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)}",
           copyholder = "SID/SCD",
                label = "6842",
             language = "pt",
                pages = "9",
                  ibi = "6qtX3pFwXQZ3r59YD6/GP2gt",
                  url = "http://urlib.net/ibi/6qtX3pFwXQZ3r59YD6/GP2gt",
                 type = "PRE",
        urlaccessdate = "05 maio 2024"
}