A specific area in the equatorial Pacific Ocean used to monitor El Niño-Southern Oscillation sea surface temperature anomalies.The Niño 3.4 region is a rectangular area in the equatorial Pacific Ocean, spanning from 120°W to 170°W longitude and 5°N to 5°S latitude. It is one of several designated 'Niño regions' used by climatologists to track sea surface temperature anomalies that indicate the state of the El Niño–Southern Oscillation (ENSO). When the average temperature in this region deviates from its long-term mean by more than 0.5°C for several months, an El Niño (warm) or La Niña (cool) episode is declared.
The Niño region designations were formalized in the 1980s by the Climate Prediction Center and other research groups, with Niño 3.4 later adopted as the primary index for ENSO monitoring.
The region is chosen because it captures the area where ocean–atmosphere coupling is strongest and where temperature changes are most directly linked to shifts in the Walker circulation. Monitoring involves averaging satellite and buoy measurements of sea surface temperature across the region, then comparing them to a 30-year climatological baseline. The resulting anomaly index, often called the ONI (Oceanic Niño Index), is the standard metric for defining ENSO events.
It is used operationally by meteorological agencies worldwide to issue ENSO alerts and seasonal outlooks, influencing decisions in agriculture, water management, and disaster preparedness.
The Niño 3.4 index is so widely used that a single value from it can trigger global media headlines about an impending El Niño.




