@Article{LopesAnSoCeKaCaMo:2022:MuNiEf,
author = "Lopes, Aixa Braga and Andreoli, Rita V. and Souza, Rodrigo A. F.
and Ceron, Wilmar L. and Kayano, Mary Toshie and Canchala,
Teresita and Moraes, Djanir Sales",
affiliation = "{Instituto Nacional de Pesquisas da Amaz{\^o}nia (INPA)} and
{Universidade do Estado do Amazonas (UEA)} and {Universidade do
Estado do Amazonas (UEA)} and {Instituto Nacional de Pesquisas da
Amaz{\^o}nia (INPA)} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Universidad del Valle} and {Instituto
Nacional de Pesquisas da Amaz{\^o}nia (INPA)}",
title = "Multiyear La Nina effects on the precipitation in South America",
journal = "International Journal of Climatology",
year = "2022",
volume = "42",
number = "16",
pages = "9567--9582",
month = "Dec.",
keywords = "multiyear La Niņa, precipitation, South America.",
abstract = "The effect of multiyear La Niņa (LN) events on precipitation in
South America (SA) was assessed considering 10 persistent LN
events over two successive years, referred to as Y1 and Y2 for the
19012012 period. Y1 spans from the austral winter of the first
year to autumn of the second year, and Y2 spans from the austral
winter of the second year to autumn of the third year. Comparisons
were performed season by season of the Y1 and Y2. Composites
revealed that the teleconnections related to a multiyear LN event
during its Y1 and Y2 years, responsible for distinct seasonal
precipitation anomaly patterns in SA, were associated with
different tropical ocean conditions. In spring, the negative sea
surface temperature (SST) dipole in the Indian Ocean during the Y2
was not observed during Y1. Different LN-related SST anomaly
patterns in the tropical Atlantic between Y1 and Y2 occurred in
the other seasons. Over northern/northeastern SA, the positive
precipitation anomalies became weaker (stronger) during austral
summer and autumn (winter and spring) of the Y2 than Y1 and were
associated with changes in the Walker cells. During austral spring
and summer, southeastern presented drier conditions during the Y2
than Y1. In the spring of Y2, two Rossby wave trains, one
associated with the LN-related anomalous cooling in the equatorial
Pacific and another triggered by the upper-level anticyclone in
the tropical Indian Ocean, characterized the circulation pattern
over SA which explains the difference in precipitation anomalies
between the Y2 and Y1. These drier (wetter) conditions during
austral spring and summer (winter and spring), particularly over
southern and southeastern Brazil (Colombia) in the Y2, might have
more severe effects on the regional hydrological cycle than those
in the Y1. The results here indicate that accurate prediction of
LN duration is crucial in a climate-monitoring context.",
doi = "10.1002/joc.7847",
url = "http://dx.doi.org/10.1002/joc.7847",
issn = "0899-8418",
language = "en",
targetfile = "Intl Journal of Climatology - 2022 - Lopes - Multiyear La Ni a
effects on the precipitation in South America.pdf",
urlaccessdate = "03 maio 2024"
}