@Article{EvangelistaMGPKTVSSAG:2007:SoTrUr,
author = "Evangelista, Heitor and Maldonado, J. and Godoi, R. H. M. and
Pereira, E. B. and Kock, D. and Tanizaki-Fonseca, K. and Van
Grieken, Rene and Sampaio, Marcelo and Setzer, Alberto Waingort
and Alencar, A. and Gon{\c{c}}alves, S. C.",
affiliation = "{Department of Biophysics and Biometry Rio de Janeiro State
University ( LARAMG/UERJ)} and Departamento de Geoquimica,
Universidade Fluminense and Gradutate Program in Environmental
Management , Centro Universit{\'a}rio Positivo - UnicemP and
{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Center for
Climate Systems Research} and {} and {} and {Instituto Nacional de
Pesquisas Espaciais} and {Instituto Nacional de Pesquisas
Espaciais}",
title = "Sources and transport of urban and biomass burning aerosol black
carbon at the South-West Atlantic coast",
journal = "Journal of Atmospheric Chemistry",
year = "2007",
volume = "56",
number = "3",
pages = "225--238",
month = "april",
note = "{DOI 10.1007/s10874-006-9052-8}",
keywords = "black carbon, South-West Atlantic, Antartic Penisula, back
trajectories, GCM.",
abstract = "The total extent of the atmospheric impacts associated to the
aerosol black carbon (BC) emissions from South America is not
completed described. This work presents results of BC monitored
during three scientific expeditions (2002, 2003 and 2004) on board
of a Brazilian oceanographic vessel Ary Rongel that covered the
South-West Atlantic coast between 22-62 degrees S. This
latitudinal band encloses major urban regions of South America and
the outflow region of the SACZ (South Atlantic Convergent Zone),
which is an important mechanism of advective transport of heat,
moisture, minor gases and aerosols from the South America
continental land to the Southern Atlantic Ocean. Our results
showed that aerosol BC enhanced concentrations from
urban/industrial origin can be transported to the South-West
Atlantic Ocean due to the migration of sub-polar fronts that
frequently reach tropical/subtropical regions. Despite the
decrease of aerosol BC concentrations southwards (from similar to
1,200 ng m(-3) at latitude 22 degrees S to similar to 10 ng m(-3)
at latitude 62 degrees S), several observed peak events were
attributed to regional urban activities. Most of such events could
be explained by the use of air mass back trajectories analysis. In
addition, a global model simulation is presented (Goddard
Institute for Space Studies - GISS GCM BC simulation) to explore
the origins of aerosol BC in the South-West Atlantic. The model
allowed isolating the biomass emissions from South America and
Africa and industrial (non-biomass) pollution from other regions
of the globe. This model suggests that the apportionment of about
half of the aerosol BC at the South-West Atlantic may derive from
South American biomass burning.",
copyholder = "SID/SCD",
issn = "0167-7764",
language = "en",
targetfile = "evangelistaH.pdf",
urlaccessdate = "13 maio 2024"
}