@Article{FossChouSelu:2017:ClAn,
author = "Foss, Marilei and Chou, Sin Chan and Seluchi, Marcelo Enrique",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Centro Nacional de
Monitoramento e Alertas de Desastres Naturais (CEMADEN)}",
title = "Interaction of cold fronts with the Brazilian Plateau: a
climatological analysis",
journal = "International Journal of Climatology",
year = "2017",
volume = "37",
number = "9",
pages = "3644--3659",
month = "July",
keywords = "cold fronts, climatology, orography, Brazilian Plateau.",
abstract = "Complex orography of elevated terrain and numerous peaks can act
as an important physical barrier to the atmospheric flow and can
generate a range of meteorological phenomena. The objective of
this study is to investigate the effect of the Brazilian Plateau
on the spatial distribution of cold fronts and their climatology
for the period between 1979 and 2010 using Climate Forecast System
Reanalysis data. The cold fronts are detected and divided into
three groups, according to their frequency and trajectory over
South America: the continental fronts are referred to as the AN
group; the fronts that pass over the coastal region of Sao Paulo
are referred to as the SP group; and the fronts that pass over the
two areas are referred to as the ANSP group. Composites of means
and anomalies of atmospheric variables are constructed for each
group. The investigation focuses on the orographic effects of the
Brazilian Plateau on the climatology of the cold fronts. The
Brazilian Plateau affects the spatial distribution ofmaximum and
minimum frontal frequency. The number of cold fronts over the
elevated regions of the Brazilian Plateau is significantly lower
than in the surrounding regions. The maximum frontal frequency is
found to the east of the Andes and a secondary maximum is found
along the Southeast coast of Brazil. The main effect of the
Brazilian Plateau on the mean and anomaly fields of meteorological
variables is to block the dry and cool post-frontal air at lower
atmospheric levels. The most significant anomalies are found in
the ANSP group of cold fronts, which are more intense and move
more rapidly eastward. On the other hand, the AN cold front group
is the most frequent, but the weakest and easily affected by the
Brazilian Plateau orography.",
doi = "10.1002/joc.4945",
url = "http://dx.doi.org/10.1002/joc.4945",
issn = "0899-8418",
language = "en",
targetfile = "foss_interaction.pdf",
urlaccessdate = "27 abr. 2024"
}