On the influences of the El Niño, La niña and Atlantic Dipole Paterni on the Amazonian Rainfall during 1960-1998

• Main Authors: SOUZA,Everaldo B de, KAYANO,Mary T, TOTA,Julio, PEZZI,Luciano, FISCH,Gilberto, NOBRE,Carlos
• Format: Article in Journal/Newspaper
• Language: English
• Published: Instituto Nacional de Pesquisas da Amazônia 2000
• Subjects: Seasonal rainfall; ENSO; Amazon; SST anomalous north-south dipole in the Atlantic; Chuva sazonal; ENOS; Amazônia; Dipolo norte-sul de anomalias de TSM; Austral; Pacific; North Atlantic
• Online Access: http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0044-59672000000200305

The influence of the large-scale climatic variability dominant modes in the Pacific and in the Atlantic on Amazonian rainfall is investigated. The composite technique of the Amazon precipitation anomalies is used in this work. The basis years for these composites arc those in the period 1960-1998 with occurrences of extremes in the Southern Oscillation (El Niño or La Niña) and the north/south warm (or cold) sea surface temperature (SST) anomalies dipole pattern in the tropical Atlantic. Warm (cold) dipole means positive (negative) anomalies in the tropical North Atlantic and negative (positive) anomalies in the tropical South Atlantic. Austral summer and autumn composites for extremes in the Southern Oscillation (El Niño or La Niña) and independently for north/south dipole pattern (warm or cold) of the SST anomalies in the tropical Atlantic present values (magnitude and sign) consistent with those found in previous works on the relationship between Amazon rainfall variations and the SST anomalies in the tropical Pacific and Atlantic. However, austral summer and autumn composites for the years with simultaneous occurrences of El Niño and warm north/south dipole of the SST anomalies in the tropical Atlantic show negative precipitation anomalies extending eastward over the center-eastern Amazon. This result indicates the important role played by the tropical Atlantic in the Amazon anomalous rainfall distribution.