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La Niña

oceanic phenomenon

News •

Scientists trace record Arctic sea ice loss to an unexpected ocean • Oct. 29, 2026, 3:44 PM ET (Earth.com)

La Niña, the cool phase of El Niño and the Southern Oscillation (ENSO), characterized primarily by colder-than-normal surface waters of the Pacific Ocean along the western coast of South America, stronger-than-normal trade winds that drive warmer toward equatorial parts of Asia and northern Australia, and amplified nutrient upwelling along the South American coast (see also marine ecosystem: upwelling). While its local and regional effects on weather and climate are generally the opposite of those associated with El Niño, its global effects can be more complex. La Niña events often follow El Niño events, which occur at irregular intervals of about two to seven years.

The Oceanic Niño Index (ONI), a measure of the departure from normal sea surface temperature in the east-central Pacific Ocean, is the standard means by which each La Niña episode is determined, gauged, and forecast. La Niña episodes are indicated by sea surface temperature decreases of more than 0.5 °C (0.9 °F) for at least five successive overlapping three-month seasons.

The Editors of Encyclopaedia BritannicaThis article was most recently revised and updated by Rick Livingston.