@Article{EscobarReboSouz:2019:ClSuBa,
author = "Escobar, Gustavo Carlos Juan and Reboita, Michelle Sim{\~o}es and
Souza, Amanda",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and
{Universidade Federal de Itajub{\'a} (UNIFEI)} and {Universidade
Federal de Itajub{\'a} (UNIFEI)}",
title = "Climatology of surface baroclinic zones in the coast of Brazil",
journal = "Atmosfera",
year = "2019",
volume = "32",
number = "2",
pages = "129--141",
keywords = "Classical cold fronts, subtropical fronts, baroclinic troughs.",
abstract = "This study presents the main differences between classical cold
fronts, subtropical fronts and baroclinic troughs, as well as a
climatology of these systems along the coast of Brazil. Regarding
the seasonality of these systems, classical cold fronts are more
frequent in winter followed by spring, subtropical fronts in
spring, and baroclinic troughs in spring and summer. In
southeastern Brazil, these three kinds of systems are responsible
for about 40% (60%) of the total precipitation during the rainy
(dry) season. RESUMEN: Este trabajo presenta las diferencias entre
frentes fr{\'{\i}}os cl{\'a}sicos, frentes subtropicales y
vaguadas barocl{\'{\i}}nicas mediante el uso de cartas
sin{\'o}pticas, as{\'{\i}} como una climatolog{\'{\i}}a de
estos sistemas en la costa este de Brasil. En lo que se refiere a
la estacionalidad de los sistemas analizados, los frentes
fr{\'{\i}}os cl{\'a}sicos son m{\'a}s frecuentes en invierno,
seguido por la primavera, mientras que los frentes subtropicales
ocurren preferentemente en primavera y las vaguadas
barocl{\'{\i}}nicas en primavera y verano. En el sudeste de
Brasil, estos tres tipos de sistemas barocl{\'{\i}}nicos son
responsables del 40% (60%) de la precipitaci{\'o}n total durante
la estaci{\'o}n lluviosa (seca).",
doi = "10.20937/ATM.2019.32.02.04",
url = "http://dx.doi.org/10.20937/ATM.2019.32.02.04",
issn = "0187-6236",
language = "en",
targetfile = "52594-150460-1-PB.pdf",
urlaccessdate = "19 abr. 2024"
}