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@InProceedings{TarasovaNobr:2000:TeAeEf,
               author = "Tarasova, Tatiana Aleksandrovna and Nobre, Carlos Afonso",
          affiliation = "{CPTEC-INPE-Cachoeira Paulista-12630-000-SP-Brasil}",
                title = "On the temperature aerosol effect measured in Brazil's Amazonia 
                         during the dry season in smoke aerosol conditions",
            booktitle = "Proceedings...",
                 year = "2000",
         organization = "International Radiation Symposium 2000: Current problems in 
                         atmospheric radiation.",
            publisher = "Deepak Publishing",
             abstract = "The data of the daily minimum and maximum near surface ror 
                         temperatures obtained at the observational site Reserva Jaru in 
                         Brazil's Amazonia in August- September 1995 are analyzed in 
                         conjunction with the data of the incident solar irradiance and net 
                         thermal ir- radiance at the surface. The solar irradiance incoming 
                         at the surface decreases from the beginning of August to 
                         mid-September in accordance with the increase of the aerosol 
                         optical depth at the mid-visible wavelength from 0.3 to 1-3. The 
                         aerosol optical depth elevation is related to the emission of 
                         smoke by the biomass burn- ing. But the calculations show that the 
                         daily average net (downward minus upward) solar radiative flux at 
                         the top of the aerosollayer, 2 km, does not change with the 
                         aerosol optical depth elevation because both down- ward and upward 
                         fluxes increase simultaneously. Thus the absence of the trend in 
                         the daily maximum temper- ature from the beginning of August to 
                         mid-September is explained by the constant absorption of the solar 
                         radiation in both aerosol and surface layers while the positive 
                         trend in the daily minimum temperature can be explained by 
                         increasing in the night of the down- ward longwave radiative flux 
                         from the heated aerosol layer to the surface.",
  conference-location = "St. Petersburg, Russia",
      conference-year = "24-29 jul.",
           copyholder = "SID/SCD",
                label = "self-archiving-INPE-MCTIC-GOV-BR",
             language = "en",
           targetfile = "11364.pdf",
        urlaccessdate = "29 mar. 2024"
}


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