A patch of the Pacific between 5°S and 5°N, 170°W to 120°W. The temperature anomaly of its water is the main measure of El Niño.The Niño 3.4 region is a specific rectangle of the equatorial Pacific Ocean, stretching from 5°S to 5°N latitude and 170°W to 120°W longitude. It sits in the central Pacific, roughly halfway between the coast of South America and the international date line. Scientists track the average sea-surface temperature in this box because it serves as the primary indicator for El Niño and La Niña events, the periodic warming and cooling of the tropical Pacific that disrupt weather patterns worldwide.
The index was formalized by the U.S. Climate Prediction Center in the 1990s as a standard for operational El Niño monitoring, building on earlier regional indices like Niño 1, 2, and 3.
The region's temperature anomaly—the difference from its long-term average—is computed from satellite and buoy data. When the anomaly stays above +0.5°C for several months, an El Niño is declared; below -0.5°C signals La Niña. This particular box is chosen because its temperature swings correlate strongly with atmospheric circulation changes, making it a sensitive gauge of the ocean-atmosphere coupling that drives these climate phenomena.
It is the benchmark used by meteorological agencies worldwide to declare El Niño or La Niña conditions and to issue seasonal climate forecasts for agriculture, water management, and disaster preparedness.
A single degree Celsius anomaly in this region can shift rainfall patterns across half the globe, from droughts in Australia to floods in California.






