@Article{SouzaAnKaCeSoRo:2023:ReInOc,
author = "Souza, Itamara P. P. and Andreoli, Rita Val{\'e}ria and Kayano,
Mary Toshie and Ceron, Wilmar Loiza and Souza, Rodrigo A. F. and
Roy, Indrani",
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 {Universidade do Estado do
Amazonas (UEA)} and UCL",
title = "Interdecadal Pacific Oscillation modulation of ENSO
teleconnections in its decaying stages: Relations with Indian
Ocean basin-wide mode and South American precipitation",
journal = "International Journal of Climatology",
year = "2023",
volume = "43",
number = "7",
pages = "3264--3283",
month = "June",
keywords = "ENSO, Indian Ocean, interdecadal modulation, precipitation, South
America.",
abstract = "This study examines the Interdecadal Pacific Oscillation (IPO)
modulation of the El Nino-Southern Oscillation (ENSO)
teleconnections in its decaying stages with the tropical ocean by
focusing on the Indian Ocean Basin-Wide (IOBW) mode and the
precipitation over South America (SA) in the 1901-2012 period.
Composite analyses revealed that the ENSO teleconnections are
IPO-modulated due to the differential ENSO decaying speed, which
is slower during the positive than negative IPO phase, for both El
Nino (EN) and La Nina (LN) cases. Negative precipitation anomalies
related to EN persist over northeastern SA until austral winter
for the positive IPO phase (POS IPO), while significant opposite
sign anomalies occur in this region for the negative IPO phase
(NEG IPO). These results are associated with the Walker
circulation's reversal during NEG IPO which is, in turn,
accompanied by negative IOBW. During the POS IPO, the positive
IOBW causes upward movements over there and, by continuity,
downward movements over SA. In the NEG IPO, for LN events the wave
train originating in the north of Australia propagates toward
subtropical SA, which, coupled with the surface circulation,
causes dryness in this region. In addition, the rapid decay of LN
in the NEG IPO, followed by the emergence of EN, caused changes in
the Walker circulation, such that enhanced upward movements
occurred over the Pacific and SA region, and downward movements
over the Indian Ocean until austral winter. In turn, the slower
decay of the LN in the POS IPO maintains strong subsidence over
the central Pacific and weak upward motions over western SA. So,
the EN (LN) and positive (negative) IOBW during the POS (NEG) IPO
prolong the scarcity of precipitation over equatorial
(subtropical) SA. Persistent dry periods over these regions during
the ENSO decaying stage might have important implications for the
seasonal forecasts.",
doi = "10.1002/joc.8028",
url = "http://dx.doi.org/10.1002/joc.8028",
issn = "0899-8418",
language = "en",
targetfile = "Intl Journal of Climatology - 2023 - Souza - Interdecadal Pacific
Oscillation modulation of ENSO teleconnections in its.pdf",
urlaccessdate = "06 maio 2024"
}