Thunderstorms
The single most-tested CPL weather topic, and the one most likely to kill you. The PPL standard is recognition; the CPL standard is anticipation — recognizing the conditions for convection from the morning briefing forward, understanding which cells are still building and which are dissipating, and respecting the operational separation distance even when ADS-B says the cell is shrinking. Primary references: FAA-H-8083-28 Aviation Weather Handbook (Ch. 22) and AC 00-24C — Thunderstorms.
Three required ingredients
Every thunderstorm — single-cell pop-up to organized supercell — needs all three:
- Sufficient water vapor — moisture for condensation and latent-heat release
- Unstable air — air that continues rising once disturbed (positive buoyancy through the lower atmosphere)
- Lifting mechanism — something to start the unstable parcel rising
Common lifting mechanisms: converging winds around surface lows and troughs, frontal lift (cold or warm), upslope flow over terrain, drylines, outflow boundaries from prior storms, sea/lake/land breezes, and valley breezes. See AWH Chapter 22 for the full taxonomy.
Life cycle — three stages
- Towering cumulus stage: Continuous updraft, rapid vertical growth (3,000+ fpm). Cloud is building. Precipitation has not yet started. Lasts ~10-20 minutes.
- Mature stage: Both updraft and downdraft present. Precipitation begins reaching the ground. Most dangerous stage — strongest turbulence, lightning, hail, microbursts. Lasts ~10-20 minutes.
- Dissipating stage: Downdrafts dominate. Updraft cuts off because precipitation cools and stabilizes the column. Anvil top spreads downwind on upper-level winds. Storm is dying — but downbursts and hail can still reach the surface from the collapsing cell.
Operational implication: "Dissipating" does not mean "safe to fly under." Strong downbursts often occur right as the cell collapses.
Three thunderstorm types
- Single-cell: Isolated, one updraft / downdraft cycle. Lifespan ~30 minutes. Common over heated terrain on summer afternoons. Easy to circumnavigate visually.
- Multicell (cluster or line): Multiple cells in different life-cycle stages. New cells form on the gust front of the dissipating cell. Can persist for hours. Squall lines are linear multicells — intense, fast-moving, often forming 50–300 NM ahead of strong cold fronts. Penetration is not survivable; the only legal answer is "don't."
- Supercell: One persistent rotating updraft (mesocyclone). The most dangerous form. Persists for hours; produces large hail, damaging straight-line winds, and the majority of strong tornadoes. Recognizable on radar by its hook echo. See SPC convective outlooks in your morning brief — supercell days are flagged in advance.
Hazards
Per AC 00-24C, a single thunderstorm cell carries the following:
- Low ceilings and visibility (precipitation, dust)
- Lightning (can damage avionics and pilot eyesight)
- Adverse winds and rapid wind shifts at the surface
- Downbursts and microbursts — see the wind shear & microbursts page
- Severe to extreme turbulence extending up to 20 NM laterally and 25 NM downwind in some cases
- Icing (especially in the upper portions, mixed and clear)
- Hail — can be encountered in clear air outside the visible cloud
- Rapid altimeter changes from pressure surges along gust fronts
- Static electricity — radio interference and P-static
- Tornadoes
- Engine water ingestion in heavy rain — flame-out risk on turbines
Avoidance — the rules pilots actually follow: circumnavigate by 20 NM minimum; never fly under an overhanging anvil; never try to outclimb a cell. Use ADS-B FIS-B weather as a strategic aid only — its NEXRAD age stamps lag the real cell by 5–20 minutes, which is plenty of time to fly into a building cell that the screen still shows clear.
METAR & TAF coding
From AC 00-45H — Aviation Weather Services:
- TS — thunderstorm without precipitation (dry thunderstorm)
- TSRA — thunderstorm with rain
- VCTS — thunderstorms in the vicinity (5–10 SM of the airport)
- TSB[time]E[time] — thunderstorm began HHmm, ended HHmm. Example: TSB0159E30 = began 0159, ended at :30 of the same hour
- +TSRAGR — heavy thunderstorm, rain, hail (GR ≥ 1/4 inch); GS = small hail/snow pellets
Convective SIGMETs are issued for the CONUS in lieu of regular SIGMETs for thunderstorms — issued every 55 minutes (and as needed) for organized severe convection. Read the current product at aviationweather.gov/sigmet. They cover thunderstorms producing severe surface wind, hail ≥ 3/4", embedded TSs, lines of TSs, or any tornado.
The pre-flight question
Before launching on a day with any chance of convection:
- Have you read the latest SPC convective outlook? "Slight risk" or worse means cells are likely.
- Are there active Convective SIGMETs on your route?
- Where will building cells most likely form along your route — over heated terrain, along a frontal line, on the upslope?
- What is your turn-around point? Brief it out loud.
- Is there a fuel-stop alternate that keeps you 20+ NM from any forecast cell?
Pilots who answer those five questions before launching almost never get caught.