Page 2: 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.

A subtle return of La Niña

A weak La Niña emerged in the equatorial Pacific in late 2025, and scientists are watching how it may help shape weather and climate in the months ahead.

WMO predicts weak La Niña climate pattern over the summer

There is a 55% chance of a weak La Niña impacting weather and climate patterns during the next three months, according to the latest update from the World Meteorological Organization (WMO). Even though La Niña has a temporary ...

Study of extreme Indian rainfall upends conventional wisdom

A new study published in the journal Science, led by scientists at the City College of New York (CCNY) and Columbia University, challenges long-held beliefs about how El Niño events influence rainfall during the Indian summer ...

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