Why Are Hurricanes Getting Stronger Only in the Atlantic? ✛

Original: "Basin-Specific Intensification of Tropical Cyclones"
· Ivo Welch
arXiv:2606.22518 · 2026-06-21 · CC BY 4.0 · 1 min
Satellites show that the number of powerful hurricanes has increased in only one ocean, not in others.

A hurricane is a giant vortex of wind that forms over warm ocean water. It needs energy, just as a fire needs fuel. A hurricane draws its energy from temperature differences: the warmer the water and the cooler the air above, the more powerful the storm can become.

Aerosols are tiny particles of dust, smoke, or droplets in the air. They act like an umbrella, blocking sunlight from heating the water.

Previously, scientists assumed that as the planet warms, hurricanes should intensify across all oceans simultaneously. But when they examined each ocean separately, they found otherwise. In the North Atlantic, the number of the most intense hurricanes increased by 7.5 per decade. In contrast, across three parts of the Pacific Ocean, no such increase was observed: in one region the relationship was actually reversed, and in the other two there was none.

This is similar to a situation where one city sees more fires due to heat, while a neighboring city does not, even though the heat is the same everywhere. The reason must lie not only in the heat but also in local conditions: how much dust is in the air, how the winds blow, and how the water circulates. Therefore, hurricane forecasts need to be made for each ocean individually, not for the whole planet at once.

The 1991 eruption of Mount Pinatubo released so many aerosols that it lowered sea surface temperatures for several years and, according to this study, affected the number of cyclones in the North Atlantic.

Scientists
Ludwig BoltzmannRudolf ClausiusJacob BekensteinStephen HawkingJames Clerk MaxwellEdward Witten
Concepts
tropical cyclone El Niño NOAA CPC North Equatorial Countercurrent tropospheric biennial oscillation ENSO Niño 3.4 Atlantic multidecadal oscillation ERSST intertropical convergence zone seasonal cycle monsoon La Niña interannual variability OISST v2.1 TAO/TRITON moorings Walker circulation decadal variability Westerly wind burst climate