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- El Niño La Niña (El Niño-Southern Oscillation) - NOAA Climate. gov
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
- ENSO Information: NOAA Physical Sciences Laboratory
El Niño and La Niña, together called the El Niño Southern Oscillation (ENSO), are episodic departures from expected sea surface temperatures (SSTs) in the equatorial Pacific Ocean
- El Niño and La Niña - National Oceanic and Atmospheric Administration
For more than 30 years, climate researchers have been puzzling about how human-forced climate change affects the El Niño Southern Oscillation (ENSO), the warm phase of which we refer to as El Niño and the cold phase as La Niña
- ENSO: Definition and Characteristics | Climatic Patterns - Geography
ENSO or El Niño is defined by prolonged differences in Pacific-Ocean surface temperatures when compared with the average value The accepted definition is a warming or cooling of at least 0 5°C (0 9°F) averaged over the east-central tropical Pacific Ocean
- El Nino Southern Oscillation (ENSO) | NASA Earthdata
El Niño and La Niña are two opposing climate patterns that break these normal conditions Scientists call these phenomena the El Niño-Southern Oscillation (ENSO) cycle During El Niño, trade winds weaken Warm water is pushed back east, toward the west coast of the Americas
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