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Tornado formation laboratory

Build a rotating supercell and explore how instability, wind shear and a powerful updraught can produce a tornado.

STORM STAGEDeveloping storm
WIND SHEAR20 m/s
TORNADO WIND0 km/h
CENTRAL PRESSURE1008 hPa
PROBE24 °C · 70%

How tornado formation works

Warm, humid surface air supplies buoyancy while colder air aloft increases instability. Changing wind speed with height creates horizontal rotation. A strong thunderstorm updraught can tilt and stretch that rotation into a vertical mesocyclone. If circulation tightens beneath the cloud base, pressure falls and a condensation funnel may descend. It becomes a tornado only when the circulation reaches the ground.

B ∝ g(Tₚ − Tₑ)/Tₑ   ·   wind shear = Δv/Δz   ·   vθ ∝ 1/r

Educational reduced-order visualisation. Tornado development is considerably more complex, and the displayed intensity is not an official Enhanced Fujita rating or weather forecast.