El Niño events are typically measured using the Niño 3.4 index, which tracks the sea surface temperature anomalies in the eastern Pacific Ocean. A positive anomaly indicates that the ocean temperature is warmer than usual, while a negative anomaly indicates cooler temperatures.
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In recent years, El Niño events have become more frequent and intense, leading to severe weather conditions such as droughts, floods, and heatwaves around the world. One of the most significant El Niño events in recent history was the 2015-2016 event, which was considered one of the strongest on record.
