Why Thunderstorms Cluster in One Place ✛

Original: "Climatological variability of a thunderstorm environment dataset in tropical and temperate regions"
arXiv:2512.14304 · 2025-12-16 · CC BY 4.0 · 1 min
A warm ocean, high-altitude winds, and climate decide where lightning strikes.

A thunderstorm is like an orchestra where warm air rises, high-altitude winds lead the melody, and lightning punctuates the finale. But who decides where this orchestra will play? Scientists gathered 45 years of data and identified the chief conductor: El Niño, a warm current in the Pacific Ocean.

To hear the music of storms, they didn't chase every cloud. Instead, for each point on the planet they calculated two numbers: how much energy is available to lift the air, and how much the wind changes with height. Multiplying them together gave a "thunderstorm environment index." The threshold was tuned so that the number of storm days matched the actual lightning detected by sensors.

In dry deserts, the threshold for a thunderstorm can be tens of times lower than in humid tropics; otherwise, not a single flash would occur.

It turned out that El Niño controls thunderstorm hotspots over a quarter of the entire planet, and over more than half of the tropical oceans. Climate warming also adds storms: roughly 30 thunderstorm days per year for each degree of warming. But for now, this signal drowns in the usual weather variability, as storms fluctuate from year to year on their own.

Previously, it was unclear how strongly ocean currents influence thunderstorms and whether a warming signal could be detected. Now it's clear: El Niño is the chief conductor, while warming is still a quiet soloist. This knowledge could help provide early warnings of thunderstorm threats to farmers, power companies, and emergency services.

The threshold for a thunderstorm environment is unique at each point on the planet: it is tuned so that the number of 'thunderstorm' hours matches the number of recorded lightning strikes. In dry deserts, this threshold can be tens of times lower than in humid tropics.

BTE = CAPE \times WS06
Product of convective available potential energy and wind shear; the higher, the more favorable conditions for thunderstorms
Concepts
interannual variability tropospheric biennial oscillation natural variability El Niño seasonal cycle climate ENSO El Niño-Southern Oscillation monsoon ERA5 spring predictability barrier tropical cyclone temperature anomaly Multivariate ENSO Index ERSST Jin-Timmermann model TAO/TRITON moorings precipitation anomaly La Niña Westerly wind burst