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

• Published in: Atmosphere Vol. 12; no. 9; p. 1094
• Main Authors: Kayano, Mary T., Andreoli, Rita V., Cerón, Wilmar L., Souza, Rodrigo A. F.
• Format: Journal Article
• Language: English
• Published: Basel MDPI AG 01-09-2021
• Subjects: Annual variations; Anticyclones; Atmospheric circulation; Atmospheric models; Cells; Circulation pattern anomalies; Circulation patterns; Climate; Climate models; Climate monitoring; climate variability; Datasets; El Nino; El Nino phenomena; El Nino-Southern Oscillation event; El Nino-Southern Oscillation event-rainfall relationships; Equator; Hadley cells; Interannual oscillation; Interannual variations; La Nina; Ocean basins; Oceans; Oscillation modes; Rain; Rainfall; Rainfall variability; Rossby wave train; Seasons; South America; Southern Oscillation; Summer; teleconnections; Time series; Trends; Tropical climate; tropical Indian ocean; Wind; South America; Brazil; Indian Ocean; Africa
• ISSN: 2073-4433; 2073-4433
• DOI: 10.3390/atmos12091094

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.