@Article{TarasovaNobrEckHolb:2000:MoGaAe,
author = "Tarasova, Tatiana Alekandrovna and Nobre, Carlos Afonso and Eck,
Thomas F. and Holben, Brent N.",
affiliation = "Instituto Nacional de Pesquisas Espaciais,(INPE/CPTEC) and
Instituto Nacional de Pesquisas Espaciais,(INPE/CPTEC) and
Ravtheon ITSS Corl>oration. NASA Goddard Space Flight Center,
Greenbelt, Marvland and NASA Goddard Space Flight Center,
Greenbelt, Marvland",
title = "Modeling of gaseous, aerosol, and cloudiness effects on surface
solar irradiance measured in Brazil's Amazonia 1992-1995",
journal = "Revista Brasileira de Geof{\'{\i}}sica",
year = "2000",
volume = "105",
number = "D 22",
pages = "26961--26969",
month = "Nov.",
keywords = "delta eddington approximation, radiation, weather, climate.",
abstract = "The effects of water vapor, aerosol, and cloudiness on the
incident surface solar irradiance continuously measured in
Brazil's Amazonia at six observational sites from 1992 to 1995 are
examined by means of a clear-sky broadband radiative transfer
model. The aerosol optical depth and precipitable water, both
retrieved from Sun photometer measurements, serve as inputs to the
model. Computed monthly mean values of clear-sky surface
irradiance are analyzed in conjunction with the monthly mean
values of all-sky surface irradiance measured on the ground. To
assess the effect of loudiness, we present the cloud radiative
forcing and cloud radiative forcing ratio at the surface, both
widely employed in cloud radiation budget studies, By its
definition the monthly mean cloud radiative forcing (cloud
radiative forcing; ratio)is the difference (ratio)between surface
solar irradiances under all-sky an clear-sky conditions. The
analysis of the irradiances, as computed and as measured, shows
that during the wet season the gaseous and cloudiness effects on
the! solar radiation attenuation in the a tmosphere are
comparable, while the aerosol influence is much smaller. The
aerosol effect increases and cloudiness effect decreases in the
second half of the dry season. Thus during the biomass burning
period ill southern Amazonia, the water vapor and aerosol effects
become comparable, while the cloudiness impact is 2-3 times
smaller. oth cloudiness and aerosol effects have strong seasonal
variations, while the gaseous effect changes slightly throughout
the year.",
copyholder = "SID/SCD",
issn = "0102-261X",
label = "10206",
language = "en",
targetfile = "Nobre_modeling.pdf",
urlaccessdate = "17 jun. 2024"
}