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Mesocyclone

A mesocyclone is the rotating updraft inside a supercell thunderstorm - a broad column of air, typically 2 to 6 miles wide, spinning at 30-60 mph. Mesocyclones produce virtually all violent (EF3+) tornadoes. If a storm has a mesocyclone, meteorologists watch it very closely.

What a Mesocyclone Is

A mesocyclone is:

• The rotating updraft inside a supercell thunderstorm
• Typically 2 to 6 miles in diameter
• Rotating at 30-60 mph
• Extending vertically from about 5,000 to 40,000+ feet
• The parent structure that produces wall clouds, funnel clouds, and tornadoes

How a Mesocyclone Forms

The process is called tilting and stretching:

1. Wind shear near the ground creates a horizontal tube of rotating air (like a rolling log)
2. An updraft develops as warm moist air rises rapidly into the growing thunderstorm
3. The updraft tilts the horizontal tube vertical, creating a rotating column of air
4. Stretching increases the rotation speed - like a figure skater pulling in her arms during a spin
5. A rotating column of air 2-6 miles wide is now embedded in the storm - the mesocyclone

Detection on Radar

Mesocyclones are detected by NEXRAD Doppler radar via a signature called rotation or couplet: an area where the radar sees strong outflow and inflow winds side by side (indicating rotation).

Modern radar automatically flags mesocyclones with algorithms. When a mesocyclone signature intensifies rapidly, or gets close to the ground, NWS forecasters issue Tornado Warnings even before an actual tornado forms.

Mesocyclone Types

Classic Mesocyclone

Well-organized, roughly cylindrical, 4-6 miles wide, extends deep into the storm. Produces the classic Great Plains tornadoes.

Mini Mesocyclone

Smaller, 1-2 miles wide, often associated with mini-supercells. Can still produce significant tornadoes.

Low-Precipitation (LP) Mesocyclone

Highly visible, minimal rain, spectacular structure. Common in West Texas and Colorado. Photogenic but not always highly productive of tornadoes.

High-Precipitation (HP) Mesocyclone

Wrapped in heavy rain. Extremely dangerous because tornadoes are often obscured. Common in Dixie Alley.

Mesocyclone to Tornado

Not every mesocyclone produces a tornado. Approximately 25% of mesocyclones produce a tornado during their lifetime. Meteorologists have identified factors that increase tornado probability:

• Rapid intensification of rotation
• Rotation extending closer to the ground
• Presence of a well-defined wall cloud
• High relative humidity in the low levels of the atmosphere
• Rear-flank downdraft (RFD) that wraps around the mesocyclone

When all these factors align, the mesocyclone typically produces a tornado within 5-20 minutes. This is the window when Tornado Warnings are issued.

Mesocyclone-Free Tornadoes

Not all tornadoes come from mesocyclones. A small fraction (maybe 10-15% of all tornadoes) form via non-supercell mechanisms - landspouts, waterspouts, gustnadoes. These are typically weak (EF0-EF1) and short-lived.

Every EF4 or EF5 tornado in the US since 1950 has been produced by a mesocyclone.

Size Comparison

• Supercell: 20-50 miles wide
• Mesocyclone: 2-6 miles wide (inside the supercell)
• Wall cloud: 1-4 miles wide (a lowering of the mesocyclone base)
• Tornado: 100 yards to 2.6 miles wide (descending from the wall cloud)

The tornado is the concentrated, ground-touching evolution of what started as the broader mesocyclonic rotation.

Sensing a Mesocyclone Nearby

Visual clues that a mesocyclone may be overhead:

• A large area of the sky is dominated by a single towering thunderstorm
• The cloud base appears to be rotating slowly - visible from a distance
• Rain-free area under one side of the storm with heavy rain on the other side
• Wall cloud lowering with visible rotation

Only trained storm spotters should be visually tracking mesocyclones. For most people: seek shelter when a Tornado Warning is issued, regardless of whether you can see the mesocyclone.

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