Weather Theory for Pilots: Fronts, Stability, Clouds and Hazards
What you'll learn: why weather happens and which hazards matter for small airplanes. Source: FAA Aviation Weather Handbook, PHAK Ch. 12–13.
Pressure and wind
Air flows from high to low pressure, turned by the Coriolis effect: clockwise around highs and counterclockwise around lows in the northern hemisphere.
Stable vs unstable air
| Stable | Unstable |
|---|---|
| Stratiform clouds, smooth air, poor visibility (haze, fog) | Cumuliform clouds, turbulence, good visibility outside showers |
Fronts
- Cold front: fast-moving, often narrow band of storms and gusty winds, then clearing.
- Warm front: slower, wide area of low clouds, rain and poor visibility.
- Look for a wind shift and pressure change when a front passes.
Thunderstorms
Need moisture, unstable air and a lifting action. Stages: cumulus (updrafts), mature (rain begins, worst turbulence), dissipating (downdrafts). Avoid by at least 20 nm when severe.
Icing and fog
- Structural icing needs visible moisture and temperatures near or below freezing.
- Radiation fog: clear, calm nights. Advection fog: moist air moving over a cooler surface.
Products
- METAR (observation; see how to read a METAR) and TAF (forecast, ~5 sm radius).
- AIRMET (Sierra: IFR/mountain obscuration, Tango: turbulence, Zulu: icing) and SIGMET/Convective SIGMET.
- PIREPs: real reports from pilots.
Check yourself
2 questions. Pick an answer to see why it's right or wrong.
Sources, review & change history
- Published
- Oct 16, 2026
- Last source review
- Not yet re-checked against primary sources
- Reviewer
- No independent reviewer yet. Written by Jackson, a student pilot, not a CFI.
- Scope
- Weather theory for VFR pilots in the U.S.
Primary sources
Changes
- Oct 17, 2026: First published.
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