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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 Southern Oscillation (ENSO) | National Centers for . . . El Niño and the Southern Oscillation, also known as ENSO is a periodic fluctuation (i e , every 2–7 years) in sea surface temperature (El Niño) and the air pressure of the overlying atmosphere (Southern Oscillation) across 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
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
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