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Supercell

A supercell is a thunderstorm with a deep, persistently rotating updraft called a mesocyclone. Supercells are the most dangerous type of thunderstorm: they produce nearly all significant tornadoes in the United States and most hail larger than golf balls, along with damaging winds and flash flooding.

Why It Matters

An ordinary thunderstorm has one updraft and one downdraft and a short life. A supercell is a single cell that can persist for many hours, with updrafts that can exceed 100 mph and outflow winds just as strong.

Supercells form when the wind changes direction and speed with height, for example southerly winds at the surface and westerly winds at about 15,000 feet. That wind shear is what sets the updraft rotating.

The Three Types of Supercell

The Three Types of Supercell
TypePrecipitationWhat to expect
ClassicHeavy precipitation falls next to the updraftLarge hail is likely, and strong, long-lived tornadoes are possible. Most supercells are this type.
Low precipitation (LP)Sparse, often transparentLarge hail that is hard to see, and no hook echo on radar.
High precipitation (HP)Nearly surrounds the updraftTornadoes may be wrapped in rain, with extremely heavy rain and flash flooding likely.

Source: NOAA JetStream: Types of Thunderstorms

Frequently Asked Questions

Do all supercells produce tornadoes?

No. Supercells produce the most destructive and deadly tornadoes, but many supercells never produce one. A supercell without a tornado can still bring large hail, damaging winds, and flash flooding.

How is a supercell different from an ordinary thunderstorm?

Rotation and lifespan. An ordinary single-cell storm has one updraft and one downdraft and dies out quickly. A supercell has a rotating updraft, called a mesocyclone, and can last for many hours while producing large hail, damaging winds, and tornadoes.

What does a supercell look like on radar?

A classic supercell often shows a hook echo, a hook-shaped extension on the storm's right rear side where precipitation wraps around the mesocyclone. Velocity data shows the rotation itself. Low precipitation supercells may show no hook at all.

Related Terms

Mesocyclone

A rotating vortex of air within a supercell thunderstorm, typically 2-6 miles in diameter. Mesocyclones are detected by Doppler radar and indicate the potential for tornado development.

Tornado

A tornado is a violently rotating column of air in contact with the ground, extending from a thunderstorm. Tornadoes are rated from EF0 to EF5 on the Enhanced Fujita scale by the damage they cause. Most last less than 10 minutes, but the strongest can stay on the ground for more than an hour.

Hook Echo

A distinctive hook-shaped radar signature on the right rear of a supercell thunderstorm, indicating rotation and high tornado probability. Hook echoes form as precipitation wraps around the mesocyclone.

Wall Cloud

An isolated lowering of a rain-free cloud base, typically found on the south or southwest side of a supercell. Wall clouds often rotate and may produce a funnel cloud or tornado. They usually precede tornado formation by 10-20 minutes.

Wind Shear

A change in wind speed or direction over a short distance, either horizontally or vertically. Strong wind shear is essential for supercell and tornado development but is also a significant hazard to aircraft during takeoff and landing.

Hail

Balls or irregular lumps of ice produced in severe thunderstorms. Hailstones form when updrafts carry raindrops into extremely cold areas of the atmosphere where they freeze. Repeated cycles through the updraft can create hailstones larger than softballs.

CAPE

CAPE (Convective Available Potential Energy) is the amount of energy a rising parcel of air can draw from the atmosphere, measured in joules per kilogram (J/kg). The higher the CAPE, the faster a storm's updraft can rise, and the stronger thunderstorms can become once something sets them off.

Sources

Explore Other Terms

Aftershock

A smaller earthquake following a mainshock in the same area, caused by the crust adjusting to redistributed stress. Aftershocks are most frequent in the first hours and days and taper off over time, but can continue for months or years after a large event. If one turns out to be larger than the original earthquake, it is reclassified as the mainshock.

Thundersnow

A rare phenomenon where thunder and lightning occur during a snowstorm. Thundersnow typically happens in intense winter storms and is often associated with heavy snowfall rates of 2-4 inches per hour.

Wet-Bulb Temperature

Wet-bulb temperature is the lowest temperature air can reach by evaporating water into it. It is always at or below the air temperature, and the drier the air, the larger the gap between the two. Forecasters use it to judge heat stress and how much falling rain or snow can cool the air.

MRMS

Multi-Radar Multi-Sensor, an advanced system that combines data from multiple radars, satellites, and surface observations to create a seamless, high-resolution national weather picture updated every 2 minutes.

Watch vs. Warning

A watch means the risk of hazardous weather has risen but its timing, location, or occurrence is still uncertain: be prepared. A warning means hazardous weather is occurring, imminent, or likely and threatens life or property: take action now. An advisory covers events that are occurring or likely but less serious than a warning.

IFR

Instrument Flight Rules govern flights conducted under instrument procedures and can be used in clear weather too. Separately, the IFR weather category means a ceiling from 500 to less than 1,000 feet and/or visibility from 1 to less than 3 statute miles, with lower values classified as LIFR. Legal operating requirements depend on airspace, regulations, equipment, and pilot qualifications.

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