@Article{KayanoCéAnSoAvZuCa:2022:DoElNi,
author = "Kayano, Mary Toshie and C{\'e}ron, Wilmar L. and Andreoli, Rita
V. and Souza, Rodrigo A. F. and Avila-Diaz, Alvaro and Zuluaga,
Cristian Felipe and Carvalho, Leila M. V.",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and
{Universidad del Valle} and {} and {Universidade do Estado do
Amazonas (UEA)} and {Universidad de Ciencias Aplicadas y
Ambientales (UDCA)} and {Universidade Federal de Vi{\c{c}}osa
(UFV)} and {University of California}",
title = "Does the El Niño-Southern Oscillation Affect the Combined Impact
of the Atlantic Multidecadal Oscillation and Pacific Decadal
Oscillation on the Precipitation and Surface Air Temperature
Variability over South America?",
journal = "Atmosphere",
year = "2022",
volume = "13",
number = "2",
pages = "e231",
month = "Feb.",
keywords = "Atlantic Multidecadal Oscillation, Climate variability,
Climatology, Pacific Decadal Oscillation, South America,
Teleconnections.",
abstract = "Previous studies have shown that the Atlantic Multidecadal
Oscillation (AMO) and Pacific Decadal Oscillation (PDO) have
combined effects on the precipitation (PRP) variability over South
America. The combined impacts have been assessed considering four
mean states as the averages of the variable anomalies during
sub-periods overlapping time intervals of the PDO and AMO phases.
Since these sub-periods include years under El Niño-Southern
Oscillation (ENSO) extremes, the extent to which these years
occurrence affects the averaged anomaly patterns during different
mean states is investigated. The analyses are done for the PRP and
surface air temperature (SAT) during the austral winter (June to
August) and summer (December to February) of the 19012014 period
using a composite technique. The nonlinear ENSO response in each
mean state for a variable corresponds to the sum of the anomaly
composites of the El Niño and La Niña events. In each mean state,
the nonlinear PRP and SAT anomalies are not negligible and show
similar patterns of the corresponding mean state, with larger
magnitudes. For both seasons and all mean states, these
similarities are more pronounced for SAT than for PRP. Thus, the
ENSO variability affects the mean states PRP and SAT anomaly
patterns in different ways. As far as we know, analyses of the
nonlinear ENSO response of the South American climate during
distinct mean states were not performed before. Our results also
indicate that the ENSO variability should be considered in the
studies of the low-frequency modes and their effects on the mean
state over South America. The results presented could be relevant
for climate monitoring and modeling studies.",
doi = "10.3390/atmos13020231",
url = "http://dx.doi.org/10.3390/atmos13020231",
issn = "2073-4433",
language = "en",
targetfile = "atmosphere-13-00231.pdf",
urlaccessdate = "03 maio 2024"
}