@Article{Kirchhoff:2004:MeCOAi,
author = "{Boian C} and Kirchhoff, Volker Walter Johann Heinrich",
affiliation = "Instituto Nacional de Pesquisas Espaciais, Divis{\~a}o de
Geof{\'{\i}}sica Espacial (INPE-DGE)",
title = "Measurements of CO in an aircraft experiment and their correlation
with biomass burning and air mass origin in South America",
journal = "Atmospheric Environment",
year = "2004",
volume = "38",
number = "37",
pages = "6337--6347",
month = "Dec.",
keywords = "biomass burning, aircraft measurements, carbon monoxide, fire
pixels, air mass transport / BRAZIL SCAR-Bv FIELD EXPERIMENT DRY
SEASON, TRACE, RADIATION, TRANSPORT, CLOUDS, SMOKE.",
abstract = "Carbon monoxide (CO) measurements are obtained in an aircraft
experiment during 1-7 September 2000, conducted over Central
Brazil in a special region of anticyclonic circulation. This is a
typical transport regime during the dry season (July September),
when intense biomass burning occurs, and which gives origin to the
transport of burning poluents from the source to distant regions.
This aircraft experiment included in situ measurements of CO
concentrations in three different scenarios: (1) areas of fresh
biomass burning air masses, or source areas; (2) areas of aged
biomass burning air masses; and (3) areas of clean air or pristine
air masses. The largest CO concentrations were of the order of
450ppbv in the source region near Conceicao do Araguaia (PA), and
the smallest value near 100 ppbv, was found in pristine air
masses, for example, near the northeast coastline (clean air, or
background region). The observed concentrations were compared to
the number of fire pixels seen by the AVHRR satellite instrument.
Backward isentropic trajectories were used to determine the origin
of the air masses at each sampling point. From the association of
the observed CO mixing ratios, fire pixels and air mass
trajectories, the previous scenarios may be subdivided as follows:
(1a) source regions of biomass burning with large CO
concentrations; (1b) regions with few local fire pixels and
absence of contributions by transport. Areas with these
characteristics include the northeast region of Brazil; (1c)
regions close to the source region and strongly affected by
transport (region of Para and Amazonas); (2) regions that have a
consistent convergence of air masses, that have traveled over
biomass burning areas during a few days (western part of the
Cerrado region); (3a) Pristine air masses with origin from the
ocean; (3b) regions with convergent transport that has passed over
areas of no biomass burning, such as frontal weather systems in
the southern regions. (C) 2004 Elsevier Ltd. All rights reserved.
.",
copyholder = "SID/SCD",
issn = "1352-2310",
language = "en",
targetfile = "measurement aircraft.pdf",
urlaccessdate = "23 maio 2024"
}