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This is an awareness of Super El Niño is an extremely strong climate phenomenon in which sea surface temperatures in the central and eastern tropical Pacific Ocean become much warmer than normal. It occurs when the trade winds weaken, allowing warm ocean water to spread eastward toward the western coast of South America. A very strong El Niño is generally associated with sea surface temperatures at least 2°C above the long-term average in the Niño 3.4 region.