@Article{CeronKaAnCaCaAl:2021:ChENFe,
author = "Ceron, Wilmar L. and Kayano, Mary Toshie and Andreoli, Rita V. and
Canchala, Teresita and Carvajal-Escobar, Yesid and
Alfonso-Morales, Wilfredo",
affiliation = "{Universidad del Valle} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Universidade do Estado do Amazonas (UEA)}
and {Universidad del Valle} and {Universidad del Valle} and
{Universidad del Valle}",
title = "Rainfall Variability in Southwestern Colombia: Changes in
ENSO-Related Features",
journal = "Pure and Applied Geophysics",
year = "2021",
volume = "178",
pages = "1087--1103",
month = "Feb.",
keywords = "Rainfall, El Nino– Southern Oscillation, correlation analysis,
Southwestern Colombia.",
abstract = "The El Nino-Southern Oscillation (ENSO) is the main phenomenon
causing interannual rainfall variability in many parts of the
globe. Its influence on Southwestern Colombia rainfall was
examined using observational and reanalysis data during the
1983-2016 period. In order to focus on the interannual timescale,
the data were filtered at the 3-6-year scale. The relations
between variables were analyzed with total and partial
correlations. The total correlations show consistent relationships
between the sea surface temperature (SST) anomalies in the
tropical Pacific and the rainfall variations in Colombia such that
the rainfall in the Andean Region (AR) relates to the SST
anomalies in the central Pacific, and the rainfall in the Pacific
Region (PR), or Pacific western plains, relates to the SST
anomalies in the eastern Pacific. Partial correlations, excluding
the Oceanic Nino Index (ONI) influence, show that AR rainfall is
partly modulated by a west-east SST gradient between the eastern
tropical Pacific and the tropical North Atlantic (TNA). The
partial correlation analyses indicate that the rainfall in the PR
is modulated by the SST anomalies in the eastern Pacific; for
example, an anomalous SST pattern with simultaneous warming north
of 10 degrees S and cooling south of 10 degrees S relates to
positive rainfall anomalies in the PR. This SST anomaly dipole in
the eastern Pacific is associated with an asymmetric anomalous
low-level wind pattern about 5 degrees S, with southeasterlies to
the south and southwesterlies to the equator which contribute to
increase moisture transport into most of the western plains of
Colombia and Ecuador and in part of the western Andes mountain
range. Conversely, an opposite-sign SST anomaly pattern in the
eastern Pacific and reversed anomaly wind pattern relate to
negative rainfall anomalies in the PR. These results establish the
foundation for rainfall differential modeling in Southwestern
Colombia based on the Pacific SST variations.",
doi = "10.1007/s00024-021-02673-7",
url = "http://dx.doi.org/10.1007/s00024-021-02673-7",
issn = "0033-4553",
language = "en",
targetfile = "Cer{\'o}n2021_Article_RainfallVariabilityInSouthwest.pdf",
urlaccessdate = "08 maio 2024"
}