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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
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- 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 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
- What is the El Niño–Southern Oscillation (ENSO) in a nutshell?
ENSO is one of the most important climate phenomena on Earth due to its ability to change the global atmospheric circulation, which in turn, influences temperature and precipitation across the globe
- 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
- What is ENSO? The El Niño Southern Oscillation - World Climate Service
ENSO is an acronym for the El Niño Southern Oscillation, a phenomenon of tropical Pacific Ocean sea surface temperature variations that drive global climate variability
- 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
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