El Niño and its opposite, La Niña, since 1950

El Niño forms when surface temperatures in the tropical Pacific Ocean are about 0.5°C (0.9°F) warmer than normal for three months. A strong or "super" El Nino has temperatures over 1.5°C (2.5°F) warmer than normal. La Niña is the reverse, with temperatures cooler than normal. The chart shows the three-month rolling average anomaly measured since 1950.