The Role of the Indian Ocean Basin-Wide and El Niño–Southern Oscillation Modes in Interannual Rainfall Variability over South America during Austral Summer

This paper examines the relative role of the Indian Ocean basin-wide (IOBW) mode and El Niño–Southern Oscillation (ENSO) in the atmospheric circulation and rainfall interannual variations over South America (SA) during southern summer of the 1951‒2016 period. The effects of the warm IOBW and El Niño...

Full description

Bibliographic Details
Main Authors: Mary T. Kayano, Rita V. Andreoli, Wilmar L. Cerón, Rodrigo A. F. Souza
Format: Article
Language:English
Published: MDPI AG 2021-08-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/12/9/1094
_version_ 1797520254627217408
author Mary T. Kayano
Rita V. Andreoli
Wilmar L. Cerón
Rodrigo A. F. Souza
author_facet Mary T. Kayano
Rita V. Andreoli
Wilmar L. Cerón
Rodrigo A. F. Souza
author_sort Mary T. Kayano
collection DOAJ
description This paper examines the relative role of the Indian Ocean basin-wide (IOBW) mode and El Niño–Southern Oscillation (ENSO) in the atmospheric circulation and rainfall interannual variations over South America (SA) during southern summer of the 1951‒2016 period. The effects of the warm IOBW and El Niño (EN) events, and of the cold IOBW and La Niña (LN) events are examined using partial correlations. The ENSO and IOBW modes, through the associated large-scale and regional anomalous circulation patterns, induce contrasting effects on the rainfall in northeastern SA. The EN without the warm IOBW effect induces anomalously dry conditions over eastern Amazon and part of northeastern Brazil (NEB) through anomalous sinking motions of the EN-related anomalous Walker and Hadley cells and strong moisture divergence associated with a vigorous anticyclone over tropical South Atlantic (TSA) and SA. The warm IOBW without the EN effect induces anomalously wet conditions in NEB, which is marginally related to the anomalous Walker and Hadley cells but is modulated by an anticyclone over SA between the equator and 20° S, and a cyclone in the southwestern Atlantic between 20° S and 40° S. The results here might be relevant for climate monitoring and modeling studies.
first_indexed 2024-03-10T07:54:10Z
format Article
id doaj.art-6744d8e750044b4faa7c0526e5b27c8c
institution Directory Open Access Journal
issn 2073-4433
language English
last_indexed 2024-03-10T07:54:10Z
publishDate 2021-08-01
publisher MDPI AG
record_format Article
series Atmosphere
spelling doaj.art-6744d8e750044b4faa7c0526e5b27c8c2023-11-22T11:59:10ZengMDPI AGAtmosphere2073-44332021-08-01129109410.3390/atmos12091094The Role of the Indian Ocean Basin-Wide and El Niño–Southern Oscillation Modes in Interannual Rainfall Variability over South America during Austral SummerMary T. Kayano0Rita V. Andreoli1Wilmar L. Cerón2Rodrigo A. F. Souza3Coordenação Geral de Ciências da Terra, Instituto Nacional de Pesquisas Espaciais, Avenida dos Astronautas, 1758, São José dos Campos 12227-010, SP, BrazilEscola Superior de Tecnologia, Universidade do Estado do Amazonas, Av. Darcy Vargas, 1200, Parque 10 de Novembro, Manaus 69065-020, AM, BrazilDepartment of Geography, Faculty of Humanities, Universidad del Valle, Calle 13 # 100-00, Cali P.O. Box 25360, ColombiaEscola Superior de Tecnologia, Universidade do Estado do Amazonas, Av. Darcy Vargas, 1200, Parque 10 de Novembro, Manaus 69065-020, AM, BrazilThis paper examines the relative role of the Indian Ocean basin-wide (IOBW) mode and El Niño–Southern Oscillation (ENSO) in the atmospheric circulation and rainfall interannual variations over South America (SA) during southern summer of the 1951‒2016 period. The effects of the warm IOBW and El Niño (EN) events, and of the cold IOBW and La Niña (LN) events are examined using partial correlations. The ENSO and IOBW modes, through the associated large-scale and regional anomalous circulation patterns, induce contrasting effects on the rainfall in northeastern SA. The EN without the warm IOBW effect induces anomalously dry conditions over eastern Amazon and part of northeastern Brazil (NEB) through anomalous sinking motions of the EN-related anomalous Walker and Hadley cells and strong moisture divergence associated with a vigorous anticyclone over tropical South Atlantic (TSA) and SA. The warm IOBW without the EN effect induces anomalously wet conditions in NEB, which is marginally related to the anomalous Walker and Hadley cells but is modulated by an anticyclone over SA between the equator and 20° S, and a cyclone in the southwestern Atlantic between 20° S and 40° S. The results here might be relevant for climate monitoring and modeling studies.https://www.mdpi.com/2073-4433/12/9/1094climate variabilitySouth Americarainfallteleconnectionstropical Indian oceanRossby wave train
spellingShingle Mary T. Kayano
Rita V. Andreoli
Wilmar L. Cerón
Rodrigo A. F. Souza
The Role of the Indian Ocean Basin-Wide and El Niño–Southern Oscillation Modes in Interannual Rainfall Variability over South America during Austral Summer
Atmosphere
climate variability
South America
rainfall
teleconnections
tropical Indian ocean
Rossby wave train
title The Role of the Indian Ocean Basin-Wide and El Niño–Southern Oscillation Modes in Interannual Rainfall Variability over South America during Austral Summer
title_full The Role of the Indian Ocean Basin-Wide and El Niño–Southern Oscillation Modes in Interannual Rainfall Variability over South America during Austral Summer
title_fullStr The Role of the Indian Ocean Basin-Wide and El Niño–Southern Oscillation Modes in Interannual Rainfall Variability over South America during Austral Summer
title_full_unstemmed The Role of the Indian Ocean Basin-Wide and El Niño–Southern Oscillation Modes in Interannual Rainfall Variability over South America during Austral Summer
title_short The Role of the Indian Ocean Basin-Wide and El Niño–Southern Oscillation Modes in Interannual Rainfall Variability over South America during Austral Summer
title_sort role of the indian ocean basin wide and el nino southern oscillation modes in interannual rainfall variability over south america during austral summer
topic climate variability
South America
rainfall
teleconnections
tropical Indian ocean
Rossby wave train
url https://www.mdpi.com/2073-4433/12/9/1094
work_keys_str_mv AT marytkayano theroleoftheindianoceanbasinwideandelninosouthernoscillationmodesininterannualrainfallvariabilityoversouthamericaduringaustralsummer
AT ritavandreoli theroleoftheindianoceanbasinwideandelninosouthernoscillationmodesininterannualrainfallvariabilityoversouthamericaduringaustralsummer
AT wilmarlceron theroleoftheindianoceanbasinwideandelninosouthernoscillationmodesininterannualrainfallvariabilityoversouthamericaduringaustralsummer
AT rodrigoafsouza theroleoftheindianoceanbasinwideandelninosouthernoscillationmodesininterannualrainfallvariabilityoversouthamericaduringaustralsummer
AT marytkayano roleoftheindianoceanbasinwideandelninosouthernoscillationmodesininterannualrainfallvariabilityoversouthamericaduringaustralsummer
AT ritavandreoli roleoftheindianoceanbasinwideandelninosouthernoscillationmodesininterannualrainfallvariabilityoversouthamericaduringaustralsummer
AT wilmarlceron roleoftheindianoceanbasinwideandelninosouthernoscillationmodesininterannualrainfallvariabilityoversouthamericaduringaustralsummer
AT rodrigoafsouza roleoftheindianoceanbasinwideandelninosouthernoscillationmodesininterannualrainfallvariabilityoversouthamericaduringaustralsummer