@Article{MartinsSilvGonç:2009:MoCaSt,
author = "Martins, J. A and Silva Dias, Maria Assun{\c{c}}{\~a}o Faus da
and Gon{\c{c}}alves, F. L. T.",
affiliation = "Univ Tecnol Fed Parana, Dept Environm Engn, BR-86020430 Londrina,
PR Brazil and {Instituto Nacional de Pesquisas Espaciais (INPE)}
and Univ Sao Paulo, Dept Atmospher Sci, Sao Paulo, Brazil",
title = "Impact of biomass burning aerosols on precipitation in the Amazon:
A modeling case study",
journal = "Revista Brasileira de Geof{\'{\i}}sica",
year = "2009",
volume = "114",
number = "D02207",
pages = "X",
month = "jan",
keywords = "cumulus cloud, clouds, drop growth.",
abstract = "A study of the potential role of aerosols in modifying clouds and
precipitation is presented using a numerical atmospheric model.
Measurements of cloud condensation nuclei (CCN) and cloud size
distribution properties taken in the southwestern Amazon region
during the transition from dry to wet seasons were used as
guidelines to define the microphysical parameters for the
simulations. Numerical simulations were carried out using the
Brazilian Development on Regional Atmospheric Modeling System, and
the results presented considerable sensitivity to changes in these
parameters. High CCN concentrations, typical of polluted days,
were found to result in increases or decreases in total
precipitation, depending on the level of pollution used as a
reference, showing a complexity that parallels the
aerosol-precipitation interaction. Our results show that on the
grids evaluated, higher CCN concentrations reduced low-to-moderate
rainfall rates and increased high rainfall rates. The principal
consequence of the increased pollution was a change from a warm to
a cold rain process, which affected the maximum and overall mean
accumulated precipitation. Under polluted conditions, cloud cover
diminished, allowing greater amounts of solar radiation to reach
the surface. Aerosol absorption of radiation in the lower layers
of the atmosphere delayed convective evolution but produced higher
maximum rainfall rates due to increased instability. In addition,
the intensity of the surface sensible heat flux, as well as that
of the latent heat flux, was reduced by the lower temperature
difference between surface and air, producing greater energy
stores at the surface.",
doi = "10.1029/2007JD009587",
url = "http://dx.doi.org/10.1029/2007JD009587",
issn = "0102-261X",
language = "en",
targetfile = "assuncao istec 675.pdf",
urlaccessdate = "01 maio 2024"
}