@Article{CavalcantiMareAlveCost:2017:ObMoSi,
author = "Cavalcanti, Iracema Fonseca de Albuquerque and Marengo, Jos{\'e}
Antonio and Alves, Lincoln Muniz and Costa, Duarte Filipe",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Centro
Nacional de Monitoramento e Alertas de Desastres Naturais
(CEMADEN)} and {Instituto Nacional de Pesquisas Espaciais (INPE)}
and {University of Exeter}",
title = "On the opposite relation between extreme precipitation over west
Amazon and southeastern Brazil: observations and model
simulations",
journal = "International Journal of Climatology",
year = "2017",
volume = "37",
number = "9",
pages = "3606--3618",
month = "July",
keywords = "extreme precipitation, South America, AGCM, climate simulation,
PULSE.",
abstract = "During the austral summer of 2014 and 2015, a severe drought
occurred in southeastern Brazil at the same time when flooding
conditions were registered in the state of Acre in the western
Amazonia of Brazil. This study aimed the identification of the
atmospheric and oceanic large-scale characteristics and regional
features associated with these conditions, and verification of the
Center of Weather Forecasting and Climate Studies/National
Institute of Space Research (CPTEC/INPE) atmospheric global
circulation model ability in reproducing the observed features.
The state of Acre was chosen as a pilot area of the PULSE-Brazil
project - a web platform tool that contains climate, ecological
and health data for Brazil. The observational data and model
results were analysed for the climatological period of 1981-2010.
Correlation analyses between precipitation over west Amazon and
atmospheric and oceanic variables indicated the main patterns in
both data sets. Extreme wet and dry Januaries over west Amazon
were selected to explore the regional and large-scale associated
features. The general results of climate analyses indicated an
opposite relation of precipitation between western Amazon and
southeastern Brazil, in January, besides the typical precipitation
dipole between the south Atlantic convergence zone and
southeastern South America. This configuration is related to
anomalous humidity flux at low levels and associated anomalous sea
level pressure over southeastern South America induced by
subsidence. The role of convection anomalies over the Pacific
Ocean on South America anomalies is discussed. The wet and dry
cases in Acre region display opposite atmospheric anomalies over
South America that are linked to wavetrains over the Pacific
Ocean, likely related to the opposite conditions of
Indonesia-Pacific tropical convection. Similar patterns of the dry
cases were observed during January of 2014 and 2015. The model
reproduced some observed atmospheric patterns related to
precipitation extremes and the results are discussed in terms of
regional and large-scale climate variability.",
doi = "10.1002/joc.4942",
url = "http://dx.doi.org/10.1002/joc.4942",
issn = "0899-8418",
language = "en",
targetfile = "cavalcanti_on the.pdf",
urlaccessdate = "24 jan. 2021"
}