The El Nino Southern Oscillation (ENSO) is generally thought to be the main reason for inter-annual warming or cooling.
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La Nina is the cold cousin of El Nino - the two collectively making up the El Nino Southern Oscillation (ENSO).
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Much of the variability in global TC ACE is explained by the concomitant changes or evolution in the character of the El Nino Southern Oscillation (ENSO) and Pacific Decadal Oscillation (PDO).
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