Module MOD-10 · 8 min · ACS PA.I.C
Air Masses, Fronts and Clouds
← Weather Theorydraft — pending CFI review
An air mass adopts the temperature and moisture of the region where it forms, and a front is the boundary where two air masses meet. A cold front, where cold air shoves warm air aside, is usually fast and narrow: expect a compact line of showers or thunderstorms and rapid clearing with cooler, drier air behind it. A warm front, where warm air rides up over cool air, is broad and gentle: expect widespread low clouds, steady precipitation, and lowering ceilings well ahead of it. A stationary front barely moves, and an occluded front forms when a cold front catches up to a warm front. The clouds tell the story too. Cumuliform (heaped) clouds mean rising, unstable air with possible turbulence and showers; stratiform (layered) clouds mean stable air and smoother flying. The lowest broken or overcast layer defines the ceiling, which is often what decides whether a VFR flight is legal and safe.
Key terms
- Air mass
- A large body of air with fairly uniform temperature and moisture.
- Front
- The boundary between two air masses of different characteristics.
- Ceiling
- The height AGL of the lowest broken or overcast cloud layer.
Summary
Cold fronts are fast and stormy with clearing behind; warm fronts are broad, cloudy, and wet. Cumuliform clouds signal instability, stratiform clouds signal stability, and the ceiling is the lowest broken or overcast layer.
Quick check ▾
One question on what you just read.
Question 1 of 1
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What weather is typically associated with the passage of a fast-moving cold front?
Sources
Every claim traces to a source — paraphrased knowledge elements pointing at the governing FAA publication; not yet verified against a retrieved source.
- PHAK Ch. 12 / Aviation Weather Handbook FAA-H-8083-28 — Pilot’s Handbook of Aeronautical Knowledge unverified
- Aviation Weather Handbook FAA-H-8083-28 / PHAK Ch. 12 — Aviation Weather Handbook unverified
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