Influence of the Antarctic Oscillation on the South Atlantic Convergence Zone

The South Atlantic convergence zone (SACZ) is the main summer-typical atmospheric phenomenon occurring in South America, and it is of great interest because it regulates the rainy season in the most populated regions of Brazil. Frequency variability, persistence, and geographical position of the SAC...

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Published in:Atmosphere
Main Authors: Flávia Venturini Rosso, Nathalie Tissot Boiaski, Simone Erotildes Teleginski Ferraz, Tiago Capello Robles
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2018
Subjects:
Online Access:https://doi.org/10.3390/atmos9110431
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author Flávia Venturini Rosso
Nathalie Tissot Boiaski
Simone Erotildes Teleginski Ferraz
Tiago Capello Robles
author_facet Flávia Venturini Rosso
Nathalie Tissot Boiaski
Simone Erotildes Teleginski Ferraz
Tiago Capello Robles
author_sort Flávia Venturini Rosso
collection MDPI Open Access Publishing
container_issue 11
container_start_page 431
container_title Atmosphere
container_volume 9
description The South Atlantic convergence zone (SACZ) is the main summer-typical atmospheric phenomenon occurring in South America, and it is of great interest because it regulates the rainy season in the most populated regions of Brazil. Frequency variability, persistence, and geographical position of the SACZ and its relationship with intraseasonal variability is well described in the literature. However, the influence of extratropical forcing on the SACZ is not well understood. Consequently, the aim of this study is to evaluate the role of the Antarctic Oscillation (AAO) in SACZ events. The persistence and frequencies of SACZ events, mean, standard deviation of total precipitation per event, lag composite of daily precipitation and geopotential height anomalies were obtained for each phase of the AAO. Therefore, frequency, persistence and total precipitation of SACZ events were higher in positive AAO (AAO+) than negative AAO (AAO−). A teleconnection mechanism between the extratropics and the SACZ region is evident in AAO+, through intensification of the polar and subtropical jets, in the days preceding SACZ. The same was not observed in the AAO−, where the anomalies were confined in the subtropical region and displaced to the South Atlantic Ocean.
format Text
genre Antarc*
Antarctic
South Atlantic Ocean
genre_facet Antarc*
Antarctic
South Atlantic Ocean
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
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op_coverage agris
op_doi https://doi.org/10.3390/atmos9110431
op_relation Climatology
https://dx.doi.org/10.3390/atmos9110431
op_rights https://creativecommons.org/licenses/by/4.0/
op_source Atmosphere; Volume 9; Issue 11; Pages: 431
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spelling ftmdpi:oai:mdpi.com:/2073-4433/9/11/431/ 2025-01-16T19:15:16+00:00 Influence of the Antarctic Oscillation on the South Atlantic Convergence Zone Flávia Venturini Rosso Nathalie Tissot Boiaski Simone Erotildes Teleginski Ferraz Tiago Capello Robles agris 2018-11-07 application/pdf https://doi.org/10.3390/atmos9110431 EN eng Multidisciplinary Digital Publishing Institute Climatology https://dx.doi.org/10.3390/atmos9110431 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 9; Issue 11; Pages: 431 South Atlantic convergence zone Antarctic Oscillation Southern Annular Mode precipitation variability tropical-extratropical interaction Brazil precipitation anomalies Text 2018 ftmdpi https://doi.org/10.3390/atmos9110431 2023-07-31T21:49:38Z The South Atlantic convergence zone (SACZ) is the main summer-typical atmospheric phenomenon occurring in South America, and it is of great interest because it regulates the rainy season in the most populated regions of Brazil. Frequency variability, persistence, and geographical position of the SACZ and its relationship with intraseasonal variability is well described in the literature. However, the influence of extratropical forcing on the SACZ is not well understood. Consequently, the aim of this study is to evaluate the role of the Antarctic Oscillation (AAO) in SACZ events. The persistence and frequencies of SACZ events, mean, standard deviation of total precipitation per event, lag composite of daily precipitation and geopotential height anomalies were obtained for each phase of the AAO. Therefore, frequency, persistence and total precipitation of SACZ events were higher in positive AAO (AAO+) than negative AAO (AAO−). A teleconnection mechanism between the extratropics and the SACZ region is evident in AAO+, through intensification of the polar and subtropical jets, in the days preceding SACZ. The same was not observed in the AAO−, where the anomalies were confined in the subtropical region and displaced to the South Atlantic Ocean. Text Antarc* Antarctic South Atlantic Ocean MDPI Open Access Publishing Antarctic The Antarctic Atmosphere 9 11 431
spellingShingle South Atlantic convergence zone
Antarctic Oscillation
Southern Annular Mode
precipitation variability
tropical-extratropical interaction
Brazil
precipitation anomalies
Flávia Venturini Rosso
Nathalie Tissot Boiaski
Simone Erotildes Teleginski Ferraz
Tiago Capello Robles
Influence of the Antarctic Oscillation on the South Atlantic Convergence Zone
title Influence of the Antarctic Oscillation on the South Atlantic Convergence Zone
title_full Influence of the Antarctic Oscillation on the South Atlantic Convergence Zone
title_fullStr Influence of the Antarctic Oscillation on the South Atlantic Convergence Zone
title_full_unstemmed Influence of the Antarctic Oscillation on the South Atlantic Convergence Zone
title_short Influence of the Antarctic Oscillation on the South Atlantic Convergence Zone
title_sort influence of the antarctic oscillation on the south atlantic convergence zone
topic South Atlantic convergence zone
Antarctic Oscillation
Southern Annular Mode
precipitation variability
tropical-extratropical interaction
Brazil
precipitation anomalies
topic_facet South Atlantic convergence zone
Antarctic Oscillation
Southern Annular Mode
precipitation variability
tropical-extratropical interaction
Brazil
precipitation anomalies
url https://doi.org/10.3390/atmos9110431