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- El Niño La Niña (El Niño-Southern Oscillation) | NOAA . . .
El Niño and La Niña are the warm and cool phases of a natural climate pattern across the tropical Pacific known as the El Niño-Southern Oscillation, or “ENSO” for short
- El Niño–Southern Oscillation - Wikipedia
El Niño–Southern Oscillation (ENSO) is a global climate phenomenon that emerges from variation in winds and sea surface temperatures over the tropical Pacific Ocean Those variations have an irregular pattern but do have some semblance of cycles The occurrence of ENSO is not predictable
- What is ENSO? - National Weather Service
The El Niño-Southern Oscillation (ENSO) is a recurring climate pattern involving changes in the temperature of waters in the central and eastern tropical Pacific Ocean
- Climate Prediction Center: ENSO Diagnostic Discussion
Synopsis: ENSO-Neutral is likely in the Northern Hemisphere summer 2025 (82% chance in June-August) and may continue into winter 2025-26, though confidence is lower (48% chance of Neutral and 41% chance of La Niña in November-January)
- ENSO Information: NOAA Physical Sciences Laboratory
The term El Niño Southern Oscillation (ENSO) basically refers to both the El Niño and La Niña phenomena together See this page for a more detailed explanation of what happens in the ocean and atmosphere during ENSO
- El Niño Southern Oscillation (ENSO)
El Niño Southern Oscillation (ENSO) is a naturally occurring large-scale climatic phenomenon involving fluctuating ocean temperatures in the central and eastern equatorial Pacific, coupled with changes in the overlying atmosphere
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