Research news on El Nino-Southern Oscillation

El Niño–Southern Oscillation (ENSO) is a coupled ocean–atmosphere phenomenon centered in the tropical Pacific, characterized by quasi-periodic fluctuations between warm (El Niño), cold (La Niña), and neutral phases. It arises from interactions between equatorial Pacific sea surface temperature anomalies, changes in thermocline depth, and variations in trade winds and the Walker circulation. ENSO modulates global atmospheric circulation, influencing precipitation patterns, temperature anomalies, and extreme weather frequency worldwide. It is a primary source of interannual climate variability and is represented and predicted in climate models using indices such as Niño 3.4 and the Southern Oscillation Index, with substantial implications for seasonal forecasting and climate impact assessments.

March smashes heat records for continental US

March's persistent unseasonable heat was so intense that the continental United States registered its most abnormally hot month in 132 years of records, according to federal weather data. And the next year or so looks to ...

Planet trapped record heat in 2025: UN

The amount of heat trapped by Earth reached record levels in 2025, with the consequences of such warming feared to last for thousands of years, the UN warned Monday.

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