@Article{SouzaAKVCMFS:2021:SePrVa,
author = "Souza, Itamara Parente de and Andreoli, Rita Val{\'e}ria and
Kayano, Mary Toshie and Vargas, Franci Flores and Cer{\'o}n,
Wilmar L. and Martins, Jorge Alberto and Freitas, Edmilson and
Souza, Rodrigo Augusto Ferreira de",
affiliation = "{Instituto Nacional de Pesquisas da Amaz{\^o}nia (INPA)} and
{Universidade do Estado do Amazonas (UEA)} and {Instituto Nacional
de Pesquisas Espaciais (INPE)} and {Instituto Nacional de
Pesquisas da Amaz{\^o}nia (INPA)} and {Universidad del Valle
Calle} and {} and {Universidade de S{\~a}o Paulo (USP)} and
{Universidade do Estado do Amazonas (UEA)}",
title = "Seasonal precipitation variability modes over South America
associated to El Niño-Southern Oscillation (ENSO) and non-ENSO
components during the 1951–2016 period",
journal = "International Journal of Climatology",
year = "2021",
volume = "41",
pages = "4321--4338",
month = "Mar.",
keywords = "ENSO, Indian Ocean, precipitation, South America, SST, Tropical
Atlantic.",
abstract = "Anomalous seasonal patterns of precipitation variability over
South America (SA) associated with El Niño-Southern Oscillation
(ENSO) and non-ENSO (residual) conditions were assessed during
19512016. Patterns were obtained from empirical orthogonal
functions analysis of total and residual precipitation seasonal
anomalies. In austral spring and summer, precipitation variability
is dominated by a dipolar anomaly mode with a centre extending
from northwestern to northeastern SA and another in
central-eastern Brazil and part of southeastern SA (SESA) during
spring, and a centre in northwestern SA and another extending from
northeastern SA to central and eastern Brazil and central SESA,
during summer. These modes are associated with ENSO to a greater
extent during spring than summer. In summer, there is a strong
association of the dipolar precipitation pattern with sea surface
temperature (SST) anomalies on the east coast of Brazil, which
indicates local influence. In austral fall, SST anomalies in the
tropical South Atlantic relate to precipitation anomalies in
northeast SA, and those in the tropical north Atlantic (TNA) to
precipitation anomalies in northwestern SA, through the
intertropical convergence zone anomalous position modulated by SST
anomalies. In this same condition, the ENSO acts only to intensify
or weaken the dominant precipitation pattern, depending on its
phase, mainly over SESA. In contrast, the second variability mode
in fall is characterized by positive SST anomalies in the Indian
Ocean and equatorial and southern Atlantic Ocean and negative in
the TNA. The importance of ENSO and the Indian Ocean in the
characterization of the SST dipole in the tropical Atlantic
explains the main changes in precipitation patterns over
northeastern Brazil not been discussed in previous studies.",
doi = "10.1002/joc.7075",
url = "http://dx.doi.org/10.1002/joc.7075",
issn = "0899-8418",
language = "en",
targetfile = "souza_seasonal.pdf",
urlaccessdate = "03 maio 2024"
}