El Nino may return in 2026 and make planet even hotter
The warming El Niño weather phenomenon could form later this year, potentially pushing global temperatures to record heights.
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.
The warming El Niño weather phenomenon could form later this year, potentially pushing global temperatures to record heights.
Environment
Mar 2, 2026
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Environment
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Earth Sciences
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Earth Sciences
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Earth Sciences
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