@Article{GuyonFWCARNKFSGCA:2005:AiMeTr,
               author = "Guyon, P. and Frank, G. and Welling, M. and Chand, D. and Artaxo, 
                         P. and Rizzo, L. and Nishioka, G. and Kolle, O. and Fritsch, H. 
                         and Silva Dias, Maria Assuncao Faus da and Gatti, L. V. and 
                         Cordova, M. and Andreae, M. O.",
          affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)/CPTEC}",
                title = "Airborne measurements of trace gas and aerosol particle emission 
                         from biomass burning in Amazonia",
              journal = "Atmospheric Chemistry and Physics Discussion",
                 year = "2005",
               volume = "5",
                pages = "2791--2831",
                month = "May.",
             keywords = "smoke, aerosols, clouds, rainfall, climate, Large-Scale 
                         biosphere-atmosphere, deforestation fires.",
             abstract = "As part of the LBA-SMOCC(Large-Scale Biosphere-Atmosphere 
                         Experiment in Amazonia-Smoke, Aerosols, Clouds, Rainfall, and 
                         Climate) 2002 campaingn, we studied the emission of carbon 
                         monoxide (CO), carbon dioxide (CO2), and aerosol particles from 
                         Amazonian deforestation fires using an instrumented aircraft, 
                         Emission ratios for aerosol number (CN) relative to CO (ERcn/co) 
                         fell in the range for most of the time, in agreement with values 
                         usually found from tropical savanna fires. The number of particles 
                         emitted per amount biomass burned was found to be dependant on the 
                         fire condition (combustion efficiency). Variability in the ERcn/co 
                         between fires was similar to the variability caused by variations 
                         in combustion behavior within each individual fire.Vertical 
                         transport of biomass-burning plumes from the boundary layer (BL) 
                         to the cloud detrainment layer (CDL) and the free troposphere (FT) 
                         was found to be a very common phenomenon. This small loss fraction 
                         sugggests that this mode of transport is very efficient in terms 
                         of particle released in the CDL and FT were larger due to 
                         coagulation. This smallloss fraction suggests cloud processing, 
                         atributable to in-cloud coagulation. This process may have 
                         significant may have significant atmospheric implications on a 
                         regional and larger scale.",
           copyholder = "SID/SCD",
                 issn = "1680-7375",
             language = "en",
           targetfile = "Guyon_SilvaDias_Airborne.pdf",
        urlaccessdate = "12 maio 2024"
}