Page 3: Research news on el nino southern oscillation

El Niño–Southern Oscillation (ENSO) is a coupled ocean–atmosphere phenomenon in the tropical Pacific characterized by quasi-periodic fluctuations between warm (El Niño), cold (La Niña), and neutral phases. It arises from interactions among equatorial Pacific sea-surface temperatures, trade winds, and the Walker circulation, producing large-scale anomalies in convection, thermocline depth, and surface pressure, notably the Southern Oscillation index. ENSO modulates global atmospheric circulation, altering precipitation, temperature, and storm tracks on interannual timescales, and serves as a key source of seasonal-to-interannual climate variability and predictability in climate diagnostics and modeling.

La Niña's new twist: Ground movement threatens Aussie homes

Australia's changing climate is shaking things up, literally. New research from the University of South Australia (UniSA) warns that increasingly intense La Niña weather cycles are posing fresh challenges for homeowners, ...

Ancient El Niño patterns hint at future climate trends

A Monash University-led study is prompting scientists to rethink how the El Niño-Southern Oscillation (ENSO) system evolved and how it might behave in the future as our climate continues to change.

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