@InCollection{UlkeLongFrei:2011:TrPaIm,
author = "Ulke, Ana Graciela and Longo, Karla M. and Freitas, Saulo Ribeiro
de",
title = "Biomass Burning in South America: Transport Patterns and Impacts",
booktitle = "Biomass - Detection, Production and Usage",
publisher = "Intech",
year = "2011",
editor = "Matovic, Darko",
pages = "337--408",
address = "Rijeka",
keywords = "biomass, production, Geology, Geophysics.",
abstract = "The Andes Mountains barrier and the interaction with the easterly
trade winds, and the flow associated to the South Atlantic
Subtropical High (SASH) are responsible of a key feature of the
low-level atmospheric circulation and climate: the so called South
American Low Level Jet (SALLJ). The SALLJ is a wind maximum
immersed in a pole-ward and moist current with a cross stream mean
dimension in the mesoscale, which has been identified as an
efficient dynamical mechanism to transport heat and humidity from
tropical to subtropical latitudes. The SALLJEX (South American Low
Level Jet Experiment) field campaign provided a unique data set
for the study and better understanding of the SALLJ (Vera et al.,
2006). The SALLJ feeds and controls the life cycle of the
mesoscale convective systems over an area that includes the Del
Plata basin, and accounts for an important fraction of the
precipitation in southern South America, thus influencing the
water balance in the region (Nicolini et al., 2002; Saulo et al.,
2000). The SALLJ has also being pointed as an important agent to
transport and mix other biogeochemical components (Paegle, 1998).
The orographic control of the Andes favouring the poleward flow
causes the persistency of the SALLJ all year round, being only
episodically interrupted by mid-latitude transient systems
arriving in the subtropical South America (SA) (James \&
Anderson, 1984; Nogues- Paegle et al., 1998). While during the
summer this flow has a net poleward component, in the winter it
has an eastward tendency up in the mid-latitudes, with an outflow
toward the South Atlantic Ocean broadly ranging from 20º S to 40º
S, strongly depending on the position of the SASH. Nogues-Paegle
\& Mo (1997) found an intraseasonal meridional seesaw of dry and
wet conditions over tropical and subtropical South America during
austral summer in which the South Atlantic Convergence Zone (SACZ)
and the low-level stream intensify alternatively. Over the central
and north bands of SA during the winter, the climate is strongly
influenced by the northward motion of the Inter-tropical
Convergence Zone (ITCZ) and the westward displacement of SASH,
composing a scenario of a low levels high pressure system over the
continent, with light winds and most of the convection being
shifted to the northern part of the Amazon and very little
precipitation.",
affiliation = "Instituto Nacional de Pesquisas Espaciais (INPE), 1Departamento de
Ciencias de la Atm{\'o}sfera y los Oc{\'e}anos, Facultad de
Ciencias Exactas y Naturales, Universidad de Buenos Aires, Buenos
Aires and {Instituto Nacional de Pesquisas Espaciais (INPE)} and
{Instituto Nacional de Pesquisas Espaciais (INPE)}",
isbn = "978-953-307-492-4",
label = "lattes: 9873289111461387 3 UlkeLongFrei:2011:TrPaAn",
language = "en",
targetfile = "
InTech-Biomass_burning_in_south_america_transport_patterns_and_impacts.pdf",
url = "http://www.intechopen.com/articles/show/title/biomass-burning-in-south-america-transport-patterns-and-impacts",
volume = "cap. 9",
urlaccessdate = "17 maio 2024"
}