Page 4: 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.

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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