@Article{HolbenSetEckPerSlu:1996:EfDrSe,
author = "Holben, B. N. and Setzer, Alberto Waingort and Eck, T. F. and
Pereira, Alfredo and Slutsker, I.",
affiliation = "NASA/Goddard Space Flight Center, Greenbelt, MD, United States and
Instituto Nacional de Pesquisas Espaciais, Centro de Previs{\~a}o
do Tempo e Estudos Clim{\'a}ticos (INPE.CPTEC) and Hughes STX
Corporation, NASA/Goddard Space Flight Center, Greenbelt, MD,
United States and Instituto Nacional de Pesquisas Espaciais,
Centro de Previs{\~a}o do Tempo e Estudos Clim{\'a}ticos
(INPE.CPTEC) and Sci. Systems and Applications, Inc., NASA/Goddard
Space Flight Center, Greenbelt, MD, United States",
title = "Effect of dry season biomass burning on Amazon Basin aerosol
concentrations and optical properties, 1992-94",
journal = "Journal of Geophysical Research: Atmospheres",
year = "1996",
volume = "101",
number = "D 14",
pages = "19465 - 19481",
month = "Aug.",
keywords = "aerosol, biomass burning, dry season, optical thickness,
stratosphere, Brazil, Amazonia.",
abstract = "Aerosol concentrations and properties have been derived from a
network of ground-based Sun-sky radiometer measurements in
Brazil's Amazon basin region since 1992. The measurements
characterize the background aerosol environment and aerosol
emissions from biomass burning at eight selected sites. The
duration and frequency of the measurements provide the foundation
of an aerosol climatology based on direct sun measurements of
aerosol optical thickness and retrievals of size distribution from
solar aureole measurements. The aerosol optical thickness
measurements clearly illustrate that for sites located within
regions of biomass burning the duration of smoke above background
levels often exceeds 2 months and frequently at levels an order of
magnitude above background. The aerosol optical thickness range
during preburning conditions was 0.11 to 0.27 at 440 nm. Under
these conditions, stratospheric aerosols from Pinatubo constituted
a significant part of the signal in 1993 but were about 50% less
in 1994. During the burning season; smoke elevated the aerosol
optical thickness above 1.0 for seasonally averaged values
measured at 440 nm at sites located in active source regions in
Mate Grosso, Rondonia, and Tocantins states. The measurement sites
are located in the cerrado and forest conversion areas. Analysis
of the size distribution of the particles indicated that the
increase in aerosol optical thickness was associated with an
increase of an accumulation and coarse particle modes. The
asymmetry factor ''g'', computed from the phase function, showed
considerable spectral dependence between the preburning and
burning seasonal phases. The 1020-nm channel was reduced from 0.66
to similar to 0.53, while at 440 nm little seasonal phase
variation was noted. Conditions of burning were sufficiently
strong that the atmospheric conditions associated with the
climatological definition of a dry season was subdivided into (1)
preburning, (2) transition to burning, (3) burning, and (4)
transition to wet season phases for most sites. Averages and
frequency distributions were used to characterize each seasonal
phase by site. Changes in total column water vapor amount, also
retrieved from direct sun measurements, did not have an apparent
effect on the optical properties of the aerosols.",
copyholder = "SID/SCD",
issn = "0102-261X",
language = "en",
urlaccessdate = "08 maio 2024"
}