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The research distinguishes between East and Central ENSO types, finding that they produce different precipitation patterns in South America. East El Niño (EEN) is associated with positive precipitation anomalies in southern Brazil, while Central El Niño (CEN) is linked to negative anomalies in eastern Brazil. Generally, anomalies are more extensive and stronger during East ENSO events than Central ones, though southern Brazil in austral spring is an exception. The frequency of extreme precipitation events generally aligns with these seasonal anomalies, though the areas of increased extreme event frequency are often more extensive than those with increased seasonal precipitation.