Page 5: 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.

Europe climate report signals rising extremes

Europe endured a historic heatwave across Nordic countries, shrinking glaciers and record sea temperatures in 2025 as the fast-warming continent faces more frequent climate extremes, a new report showed Wednesday.

El Niño season predicted to start as early as next month

An El Niño event is expected to develop from mid-2026, impacting global temperature and rainfall patterns, according to the World Meteorological Organization (WMO). The latest monthly Global Seasonal Climate Update from WMO ...

Warming El Nino set to return in mid-2026: UN

The El Niño weather phenomenon, which pushed global temperatures to record highs the last time around, is expected to return in mid-2026, the UN said Friday.

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