@InProceedings{HolbenEcSeSlPeMaVa:1999:TeSpVa,
author = "Holben, Brent N. and Eck, Thomas F. and Setzer, Alberto Waingort
and Slutzker, Ilya and Pereira, Alfredo and Markham, Brian and
Vande-Castle, John",
title = "Temporal and spatial variability of aerosol loading and properties
during the Amazon, North American temperate, and boreal forest
burning seasons",
year = "1999",
pages = "618--636",
organization = "Biomass Burning and Global Change.",
abstract = "Biomass burning plays a significant part in the major terrestrial
ecosystems of the globe and recently has become the focus for
study on the influence of global climate forcing through direct
and indirect impacts on the radiation regime. The concentrations
and properties of aerosols contribute significantly to climate
radiative forcing. Hansen and Lacis (1990)state that {"}Aerosols
are the source of our greatest uncertainty about climate forcing.
Tropospheric aerosols are difficult to monitor because of their
spatial inhomogeneity, but they are a crucial variable because of
the strong anthropogenic influence on their amount.{"}
Addition-ally, modeling by Charlson et al. (1992), Penner et al.
(1992, 1994)suggests that the direct and indirect radiative
effects of sulfate and other aerosols in the tropo-sphere,
including those from biomass burning, may be sufficient worldwide
to offset the radiative effects of increases in greenhouse gases.
Penner et al. (1994)propose that synoptic-to-global-scale
observations be made of the radiation budget, as well as both the
com-position of the aerosols and their interactions with water
vapor.",
conference-location = "BR",
label = "9019",
targetfile = "INPE 8063.pdf",
urlaccessdate = "02 maio 2024"
}