El Niño is a recurring climate phenomenon caused by unusually warm ocean waters in the tropical Pacific. That warming alters atmospheric circulation patterns, influencing rainfall, temperatures and storm systems across the globe.
Why it matters now: Scientists say the event is forming against a backdrop of already elevated global temperatures driven by climate change. That means even a moderate El Niño could produce outsized and less predictable impacts.The phenomenon is linked to heatwaves, droughts and wildfire risks in some regions, while others may face flooding and intense rainfall. It can also temporarily raise global temperatures further, increasing the chances that 2026 or 2027 become the hottest years on record.
What’s driving the shift: Forecasters point to a large reservoir of warm subsurface water in the central and eastern Pacific that is expected to rise and sustain the event. Weakening equatorial winds and other atmospheric changes could further amplify warming if ocean-atmosphere feedback loops fully align.
The big picture: Past El Niño events have disrupted agriculture, strained water supplies and complicated energy planning worldwide. Scientists caution there is still uncertainty over whether this episode reaches “Super” status, but even a strong El Niño could significantly disrupt monsoons, hurricane activity and seasonal weather patterns across Asia, Africa and the Americas.

