Intraseasonal Variability In South America during the Cold Season

Intraseasonal (IS) variability in South America is analyzed during the cold season using 10-90 day bandpass filtered OLR anomalies (FOLR). IS variability explains a large percentage of variance with maximum values over Paraguay, northeastern Argentina, and southern Brazil. The leading pattern of FOL...

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Published in:Climate Dynamics
Main Authors: Alvarez, Mariano Sebastián, Vera, Carolina Susana, Kiladis, G. N., Liebmann, Brant
Format: Article in Journal/Newspaper
Language:English
Published: Springer
Subjects:
Online Access:http://hdl.handle.net/11336/32171
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author Alvarez, Mariano Sebastián
Vera, Carolina Susana
Kiladis, G. N.
Liebmann, Brant
author_facet Alvarez, Mariano Sebastián
Vera, Carolina Susana
Kiladis, G. N.
Liebmann, Brant
author_sort Alvarez, Mariano Sebastián
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
container_issue 11-12
container_start_page 3253
container_title Climate Dynamics
container_volume 42
description Intraseasonal (IS) variability in South America is analyzed during the cold season using 10-90 day bandpass filtered OLR anomalies (FOLR). IS variability explains a large percentage of variance with maximum values over Paraguay, northeastern Argentina, and southern Brazil. The leading pattern of FOLR, as isolated from an EOF analysis, (Cold Season IS pattern, CSIS), is characterized by a monopole centered over southeastern South America (SESA) with a northwest-southeast orientation. CSIS induces a large modulation on daily precipitation anomalies, especially on both wet spells and daily precipitation extremes, which are favored during positive (wet) CSIS phases. Large-Scale OLR anomalies over the tropical Indian and west Pacific Oceans associated with CSIS exhibit eastward propagation along tropical latitudes. In addition, circulation anomalies in the Southern Hemisphere reveal the presence of an anticyclonic anomaly over Antarctica with opposite-sign anomalies in middle latitudes 10 days before CSIS is maximum as well as evidence of Rossby wave-like patterns. Positive precipitation anomalies in SESA are favored during wet CSIS phases by the intensification of a cyclonic anomaly located further south, which is discernible over the southeastern Pacific for at least 14 days before CSIS peaks. The cyclonic anomaly evolution is accompanied by the intensification of an upstream anticyclonic anomaly, which remains quasi-stationary near the Antarctica Peninsula before the CSIS peak. We speculate that the stationary behavior of the anticyclonic center is favored by a hemispheric circulation anomaly pattern resembling that associated with a negative Southern Annular Mode (SAM) phase and a wavenumber 3-4 pattern at middle latitudes. Fil: Alvarez, Mariano Sebastián. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Centro de Investigaciones del Mar y la Atmosfera. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Centro de ...
format Article in Journal/Newspaper
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
geographic Alvarez
Argentina
Indian
Pacific
geographic_facet Alvarez
Argentina
Indian
Pacific
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op_doi https://doi.org/10.1007/s00382-013-1872-z
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http://hdl.handle.net/11336/32171
Liebmann, Brant; Kiladis, G. N.; Vera, Carolina Susana; Alvarez, Mariano Sebastián; Intraseasonal Variability In South America during the Cold Season; Springer; Climate Dynamics; 42; 11-12; 6-2014; 3253-3269
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spelling ftconicet:oai:ri.conicet.gov.ar:11336/32171 2025-01-16T19:20:48+00:00 Intraseasonal Variability In South America during the Cold Season Alvarez, Mariano Sebastián Vera, Carolina Susana Kiladis, G. N. Liebmann, Brant application/pdf http://hdl.handle.net/11336/32171 eng eng Springer info:eu-repo/semantics/altIdentifier/url/http://link.springer.com/article/10.1007%2Fs00382-013-1872-z info:eu-repo/semantics/altIdentifier/doi/10.1007/s00382-013-1872-z http://hdl.handle.net/11336/32171 Liebmann, Brant; Kiladis, G. N.; Vera, Carolina Susana; Alvarez, Mariano Sebastián; Intraseasonal Variability In South America during the Cold Season; Springer; Climate Dynamics; 42; 11-12; 6-2014; 3253-3269 0930-7575 CONICET Digital CONICET info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ Intraseasonal Variability Winter Outgoing Longwave Radiation South America https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion ftconicet https://doi.org/10.1007/s00382-013-1872-z 2023-09-24T20:07:36Z Intraseasonal (IS) variability in South America is analyzed during the cold season using 10-90 day bandpass filtered OLR anomalies (FOLR). IS variability explains a large percentage of variance with maximum values over Paraguay, northeastern Argentina, and southern Brazil. The leading pattern of FOLR, as isolated from an EOF analysis, (Cold Season IS pattern, CSIS), is characterized by a monopole centered over southeastern South America (SESA) with a northwest-southeast orientation. CSIS induces a large modulation on daily precipitation anomalies, especially on both wet spells and daily precipitation extremes, which are favored during positive (wet) CSIS phases. Large-Scale OLR anomalies over the tropical Indian and west Pacific Oceans associated with CSIS exhibit eastward propagation along tropical latitudes. In addition, circulation anomalies in the Southern Hemisphere reveal the presence of an anticyclonic anomaly over Antarctica with opposite-sign anomalies in middle latitudes 10 days before CSIS is maximum as well as evidence of Rossby wave-like patterns. Positive precipitation anomalies in SESA are favored during wet CSIS phases by the intensification of a cyclonic anomaly located further south, which is discernible over the southeastern Pacific for at least 14 days before CSIS peaks. The cyclonic anomaly evolution is accompanied by the intensification of an upstream anticyclonic anomaly, which remains quasi-stationary near the Antarctica Peninsula before the CSIS peak. We speculate that the stationary behavior of the anticyclonic center is favored by a hemispheric circulation anomaly pattern resembling that associated with a negative Southern Annular Mode (SAM) phase and a wavenumber 3-4 pattern at middle latitudes. Fil: Alvarez, Mariano Sebastián. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Centro de Investigaciones del Mar y la Atmosfera. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Centro de ... Article in Journal/Newspaper Antarc* Antarctica CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Alvarez ENVELOPE(-64.483,-64.483,-65.633,-65.633) Argentina Indian Pacific Climate Dynamics 42 11-12 3253 3269
spellingShingle Intraseasonal Variability
Winter
Outgoing Longwave Radiation
South America
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Alvarez, Mariano Sebastián
Vera, Carolina Susana
Kiladis, G. N.
Liebmann, Brant
Intraseasonal Variability In South America during the Cold Season
title Intraseasonal Variability In South America during the Cold Season
title_full Intraseasonal Variability In South America during the Cold Season
title_fullStr Intraseasonal Variability In South America during the Cold Season
title_full_unstemmed Intraseasonal Variability In South America during the Cold Season
title_short Intraseasonal Variability In South America during the Cold Season
title_sort intraseasonal variability in south america during the cold season
topic Intraseasonal Variability
Winter
Outgoing Longwave Radiation
South America
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
topic_facet Intraseasonal Variability
Winter
Outgoing Longwave Radiation
South America
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
url http://hdl.handle.net/11336/32171