📘 How a tornado gets organized
Trace wind shear, rotating updrafts, downdrafts, funnels, and radar signatures.
What you’ll learn
- Ingredients
- Shear
- Updraft
- Supercell
- Inflow
- Downdrafts
- Low-level circulation
- Pressure
- Condensation funnel
- Radar
- Storm motion
- Non-supercell tornadoes
- Lifecycle
- Multiple vortices
- Intensity
- Warning
- Open questions
Questions this course answers
What does wind shear provide for many supercell tornadoes?
Wind changes with height create horizontal vorticity that an updraft can tilt and stretch.
What is a mesocyclone?
Doppler radar uses mesocyclone for a storm-scale rotating updraft.
Why is a condensation funnel not identical to a tornado?
Condensation marks saturated air; ground contact can exist with an incomplete or invisible funnel.
What can a Doppler velocity couplet indicate?
Opposite radial velocities side by side are evidence of rotation relative to the radar.
Why can a downdraft either help or stop a tornado?
A rear-flank downdraft may concentrate low-level rotation, but cold outflow can choke the updraft.
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