Why the Wind Goes Haywire Before a Big El Niño ✛

Original: "An improved noise model for representing westerly wind bursts in the recharge oscillator model of ENSO"
arXiv:2512.22710 · 2025-12-27 · CC BY 4.0 · 1 min
The warm ocean itself triggers new wind bursts, explaining why strong El Niños arrive in a series of pushes.

The Pacific Ocean works like a seesaw: water warms up near one coast, then the other. When it gets unusually warm off South America, that's El Niño—a year of weird weather across the planet. Wind rocks this seesaw. Short bursts of westerly wind, lasting just one to two weeks, are especially important. A single burst hits the water like a palm on a taut sheet, sending a wave racing across the entire ocean.

Scientists used to describe these bursts as steady background noise, as if the wind always blew the same way. But before a major El Niño, bursts come in series, like someone tossing stone after stone into a pond. The new model says: while the water is cold, the wind stays calm. But once the ocean warms about one and a half degrees above normal, it starts triggering new bursts on its own. Warm water changes the air above it, and that air breaks into short, powerful jolts.

One and a half degrees is the threshold beyond which an El Niño is considered strong. Right at that point, the wind switches to bursts in series.

Testing against 153 years of data confirmed that this model correctly shows more bursts before a strong El Niño than before a weak one. That helps better predict dangerous warm years. Now the ocean's seesaw is less of a mystery: you can see where the hand that pushes it comes from.

Westerly wind bursts last only one to two weeks, but they can trigger a chain of oceanic Kelvin waves that, over several months, warm the eastern Pacific by several degrees.

Scientists
Rainer Sachs
Concepts
Westerly wind burst ENSO recharge oscillator model Multivariate ENSO Index El Niño-Southern Oscillation zebiak cane model Warm water volume La Niña El Niño ERSST Southern Oscillation spring predictability barrier equatorial wave propagation NOAA CPC natural variability Bjerknes feedback Indian Ocean capacitor effect relative ONI TAO/TRITON moorings wind