Evolution of Extreme Madden-Julian Oscillation Events and their Impact on South America

Autores
Minjares, Mónica; Barreiro, Marcelo; Corral, Álvaro
Año de publicación
2025
Idioma
inglés
Tipo de recurso
documento de conferencia
Estado
versión publicada
Descripción
The Madden-Julian Oscillation is the leading mode of intraseasonal variability in the tropics, having large influence on the tropical circulation and precipitation within the time band of 30-60 days (Wheeler and Hendon, 2004; Kiladis et al., 2014) and is the most important source of predictability on subseasonal time scales (Ling et al., 2019). The influence of MJO is not limited to the tropics, it also impacts the extratropics through atmospheric teleconnection patterns. During austral summer the MJO influences the South American Dipole (SAD), a rainfall pattern characterized by opposite rainfall anomalies in the South Atlantic Convergence Zone (SACZ) and southeastern South America (SESA). ENSO is the most important source of interannual climate variability, is originated in the equatorial Pacific but has a strong influence around the globe. In particular in South America during austral summer the El Niño phase influences the rainy season in the coast of Peru, northeastern Brazil, southeastern Brazil, Uruguay, Argentina and Chile (e.g. Ambrizzi et al. 2004; Barreiro 2010, Barreiro 2024). Both, MJO and ENSO are known to influence the SAD through different mechanisms. In a recent work (Corral et al. 2023), we studied the statistics of the size and duration of MJO events and found that there is increased probability of extinction after about 27 days, roughly half the characteristic period. Moreover, this analysis allows us to distinguish between weak MJO and extreme MJO events, which would be expected to have different impacts worldwide and particularly over South America. Hence in this study we focus characterizing the evolution of extreme MJO events and their impact in tropical and extratropical South America depending on the initiation phase. Following our previous work (Corral et al. 2023), MJO events are considered extremes when they exceed a certain threshold, based on the distribution of events. We further analyze whether ENSO influences MJO and its impacts over South America.
Facultad de Ciencias Astronómicas y Geofísicas
Materia
Meteorología
Madden-Julian Oscillation
Extreme events
Nivel de accesibilidad
acceso abierto
Condiciones de uso
http://creativecommons.org/licenses/by-nc-sa/4.0/
Repositorio
SEDICI (UNLP)
Institución
Universidad Nacional de La Plata
OAI Identificador
oai:sedici.unlp.edu.ar:10915/193597

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spelling Evolution of Extreme Madden-Julian Oscillation Events and their Impact on South AmericaMinjares, MónicaBarreiro, MarceloCorral, ÁlvaroMeteorologíaMadden-Julian OscillationExtreme eventsThe Madden-Julian Oscillation is the leading mode of intraseasonal variability in the tropics, having large influence on the tropical circulation and precipitation within the time band of 30-60 days (Wheeler and Hendon, 2004; Kiladis et al., 2014) and is the most important source of predictability on subseasonal time scales (Ling et al., 2019). The influence of MJO is not limited to the tropics, it also impacts the extratropics through atmospheric teleconnection patterns. During austral summer the MJO influences the South American Dipole (SAD), a rainfall pattern characterized by opposite rainfall anomalies in the South Atlantic Convergence Zone (SACZ) and southeastern South America (SESA). ENSO is the most important source of interannual climate variability, is originated in the equatorial Pacific but has a strong influence around the globe. In particular in South America during austral summer the El Niño phase influences the rainy season in the coast of Peru, northeastern Brazil, southeastern Brazil, Uruguay, Argentina and Chile (e.g. Ambrizzi et al. 2004; Barreiro 2010, Barreiro 2024). Both, MJO and ENSO are known to influence the SAD through different mechanisms. In a recent work (Corral et al. 2023), we studied the statistics of the size and duration of MJO events and found that there is increased probability of extinction after about 27 days, roughly half the characteristic period. Moreover, this analysis allows us to distinguish between weak MJO and extreme MJO events, which would be expected to have different impacts worldwide and particularly over South America. Hence in this study we focus characterizing the evolution of extreme MJO events and their impact in tropical and extratropical South America depending on the initiation phase. Following our previous work (Corral et al. 2023), MJO events are considered extremes when they exceed a certain threshold, based on the distribution of events. We further analyze whether ENSO influences MJO and its impacts over South America.Facultad de Ciencias Astronómicas y Geofísicas2025info:eu-repo/semantics/conferenceObjectinfo:eu-repo/semantics/publishedVersionObjeto de conferenciahttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdfhttp://sedici.unlp.edu.ar/handle/10915/193597enginfo:eu-repo/semantics/altIdentifier/isbn/978-950-34-2665-4info:eu-repo/semantics/altIdentifier/url/https://cenamet.org.ar/congremet/wp-content/uploads/2025/11/A3_T068.pdfinfo:eu-repo/semantics/reference/hdl/10915/193317info:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by-nc-sa/4.0/Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)reponame:SEDICI (UNLP)instname:Universidad Nacional de La Platainstacron:UNLP2026-05-06T13:00:43Zoai:sedici.unlp.edu.ar:10915/193597Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292026-05-06 13:00:44.269SEDICI (UNLP) - Universidad Nacional de La Platafalse
dc.title.none.fl_str_mv Evolution of Extreme Madden-Julian Oscillation Events and their Impact on South America
title Evolution of Extreme Madden-Julian Oscillation Events and their Impact on South America
spellingShingle Evolution of Extreme Madden-Julian Oscillation Events and their Impact on South America
Minjares, Mónica
Meteorología
Madden-Julian Oscillation
Extreme events
title_short Evolution of Extreme Madden-Julian Oscillation Events and their Impact on South America
title_full Evolution of Extreme Madden-Julian Oscillation Events and their Impact on South America
title_fullStr Evolution of Extreme Madden-Julian Oscillation Events and their Impact on South America
title_full_unstemmed Evolution of Extreme Madden-Julian Oscillation Events and their Impact on South America
title_sort Evolution of Extreme Madden-Julian Oscillation Events and their Impact on South America
dc.creator.none.fl_str_mv Minjares, Mónica
Barreiro, Marcelo
Corral, Álvaro
author Minjares, Mónica
author_facet Minjares, Mónica
Barreiro, Marcelo
Corral, Álvaro
author_role author
author2 Barreiro, Marcelo
Corral, Álvaro
author2_role author
author
dc.subject.none.fl_str_mv Meteorología
Madden-Julian Oscillation
Extreme events
topic Meteorología
Madden-Julian Oscillation
Extreme events
dc.description.none.fl_txt_mv The Madden-Julian Oscillation is the leading mode of intraseasonal variability in the tropics, having large influence on the tropical circulation and precipitation within the time band of 30-60 days (Wheeler and Hendon, 2004; Kiladis et al., 2014) and is the most important source of predictability on subseasonal time scales (Ling et al., 2019). The influence of MJO is not limited to the tropics, it also impacts the extratropics through atmospheric teleconnection patterns. During austral summer the MJO influences the South American Dipole (SAD), a rainfall pattern characterized by opposite rainfall anomalies in the South Atlantic Convergence Zone (SACZ) and southeastern South America (SESA). ENSO is the most important source of interannual climate variability, is originated in the equatorial Pacific but has a strong influence around the globe. In particular in South America during austral summer the El Niño phase influences the rainy season in the coast of Peru, northeastern Brazil, southeastern Brazil, Uruguay, Argentina and Chile (e.g. Ambrizzi et al. 2004; Barreiro 2010, Barreiro 2024). Both, MJO and ENSO are known to influence the SAD through different mechanisms. In a recent work (Corral et al. 2023), we studied the statistics of the size and duration of MJO events and found that there is increased probability of extinction after about 27 days, roughly half the characteristic period. Moreover, this analysis allows us to distinguish between weak MJO and extreme MJO events, which would be expected to have different impacts worldwide and particularly over South America. Hence in this study we focus characterizing the evolution of extreme MJO events and their impact in tropical and extratropical South America depending on the initiation phase. Following our previous work (Corral et al. 2023), MJO events are considered extremes when they exceed a certain threshold, based on the distribution of events. We further analyze whether ENSO influences MJO and its impacts over South America.
Facultad de Ciencias Astronómicas y Geofísicas
description The Madden-Julian Oscillation is the leading mode of intraseasonal variability in the tropics, having large influence on the tropical circulation and precipitation within the time band of 30-60 days (Wheeler and Hendon, 2004; Kiladis et al., 2014) and is the most important source of predictability on subseasonal time scales (Ling et al., 2019). The influence of MJO is not limited to the tropics, it also impacts the extratropics through atmospheric teleconnection patterns. During austral summer the MJO influences the South American Dipole (SAD), a rainfall pattern characterized by opposite rainfall anomalies in the South Atlantic Convergence Zone (SACZ) and southeastern South America (SESA). ENSO is the most important source of interannual climate variability, is originated in the equatorial Pacific but has a strong influence around the globe. In particular in South America during austral summer the El Niño phase influences the rainy season in the coast of Peru, northeastern Brazil, southeastern Brazil, Uruguay, Argentina and Chile (e.g. Ambrizzi et al. 2004; Barreiro 2010, Barreiro 2024). Both, MJO and ENSO are known to influence the SAD through different mechanisms. In a recent work (Corral et al. 2023), we studied the statistics of the size and duration of MJO events and found that there is increased probability of extinction after about 27 days, roughly half the characteristic period. Moreover, this analysis allows us to distinguish between weak MJO and extreme MJO events, which would be expected to have different impacts worldwide and particularly over South America. Hence in this study we focus characterizing the evolution of extreme MJO events and their impact in tropical and extratropical South America depending on the initiation phase. Following our previous work (Corral et al. 2023), MJO events are considered extremes when they exceed a certain threshold, based on the distribution of events. We further analyze whether ENSO influences MJO and its impacts over South America.
publishDate 2025
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