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Enhanced Fujita Scale

Also called: EF scale, EF rating

The Enhanced Fujita (EF) scale rates tornadoes from EF0 to EF5 based on the damage they cause. Surveyors compare the damage to 28 kinds of buildings, structures, and trees against expected levels of damage, then estimate the 3-second wind gust responsible. EF0 means estimated gusts of 65 to 85 mph, and EF5 means over 200 mph.

Why It Matters

The EF rating is the standard shorthand for how strong a tornado was. It is assigned after the storm, from a damage survey, because tornado winds are almost never measured directly. The scale is a set of wind estimates based on damage, not measurements.

The EF scale replaced the original Fujita (F) scale in the United States on 1 February 2007.

Enhanced Fujita Scale and the Original Fujita Scale

Enhanced Fujita Scale and the Original Fujita Scale
RatingEF scale: estimated 3-second gustOriginal F scale: fastest quarter-mile wind
065 to 85 mph40 to 72 mph
186 to 110 mph73 to 112 mph
2111 to 135 mph113 to 157 mph
3136 to 165 mph158 to 207 mph
4166 to 200 mph208 to 260 mph
5Over 200 mph261 to 318 mph

Source: Storm Prediction Center: The Enhanced Fujita Scale

What a Rating Does Not Tell You

  • It is not a forecast. A tornado gets its rating after a damage survey, so the number is unknown while the tornado is on the ground.
  • It is not a measurement. The wind speeds are estimates inferred from damage.
  • It depends on what was hit. The rating comes from damage, so a tornado that crosses open country with little to damage can be rated lower than its true strength.
  • There is no EF6. EF5 has no upper limit.

Frequently Asked Questions

What wind speed is an EF5 tornado?

An EF5 tornado has estimated 3-second gusts over 200 mph. It is the highest rating on the Enhanced Fujita scale, and there is no EF6.

What is the difference between the Fujita scale and the Enhanced Fujita scale?

The original Fujita scale assigned wind speeds, up to 261 to 318 mph for an F5, that were never scientifically verified. The Enhanced Fujita scale, used in the United States since 1 February 2007, estimates 3-second gusts from 28 damage indicators. Its wind speeds for the higher ratings are lower than the old scale's.

Who decides a tornado's EF rating?

National Weather Service survey teams. They examine the damage after the storm, match it to the scale's damage indicators, and assign the rating from the worst damage the tornado caused.

Related Terms

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.

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.

Debris Ball

A radar signature showing a concentrated area of debris lofted by a tornado. Debris balls appear as a circular area of high reflectivity collocated with rotation and confirm a tornado is on the ground causing damage.

Funnel Cloud

A rotating cone-shaped cloud extending downward from the base of a thunderstorm but not reaching the ground. When a funnel cloud touches the ground, it becomes a tornado.

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.

Saffir-Simpson Scale

The Saffir-Simpson Hurricane Wind Scale rates hurricanes from Category 1 to Category 5 by maximum sustained wind speed. Category 1 starts at 74 mph and Category 5 at 157 mph, and Category 3 and higher are called major hurricanes. The scale measures wind only: it does not account for storm surge, rainfall flooding, or tornadoes.

Sources

Explore Other Terms

El Niño and La Niña

El Niño and La Niña are the warm and cool phases of a recurring climate pattern in the tropical Pacific called the El Niño-Southern Oscillation (ENSO). During El Niño, the trade winds weaken and the central and eastern tropical Pacific runs warmer than average. During La Niña, the trade winds strengthen and the same waters run cooler. Both shift weather patterns worldwide.

Kp Index

The Kp index is a 0 to 9 scale of global geomagnetic activity, reported in 3-hour intervals from ground-based magnetometers. A Kp of 5 or higher indicates a geomagnetic storm, and the values map onto NOAA's G-scale from G1 (Kp 5) to G5 (Kp 9). The higher the Kp, the farther from the poles the aurora can be seen.

S-Wave

The secondary or shear wave, which arrives after the P-wave and moves rock perpendicular to its direction of travel. S-waves shake far more strongly than P-waves and cause much of the damage in an earthquake. They cannot travel through liquids, which is how scientists established that Earth's outer core is molten.

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.

Barometric Pressure

The weight of the atmosphere pressing down on a given point, measured in inches of mercury (inHg) or millibars (mb). Rising pressure typically indicates improving weather, while falling pressure suggests approaching storms or precipitation.

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.

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