IFR Weather

IFR Weather

AWH / AIM 7 • Theory & Fronts, Icing & Storms, Products, Briefings

Weather is the #1 Cause of Fatal GA Accidents

This module covers ACS IR.I.B knowledge areas K1–K4 and risk management R1–R2. References: Aviation Weather Handbook (FAA-H-8083-28A), Instrument Flying Handbook (FAA-H-8083-15B), AIM Chapter 7, AC 00-6B, AC 91-74B.

Key Takeaways

  • Stable air → stratiform clouds, steady precip, poor visibility, smooth air (classic IFR); unstable air → cumuliform, showers, turbulence, good vis between.
  • Standard lapse rate is 2°C/1,000 ft; a steep lapse rate destabilizes (convection), an inversion is extremely stable and traps moisture into low IFR.
  • A warm front is the classic extended-IFR maker — a 200+ NM band of stratus with gradually lowering ceilings; cold fronts are narrow but violent.
  • The worst icing sits just above the freezing level in stratiform cloud ahead of a warm front; wind shear and mountain-wave are the big wind hazards.

Atmospheric Stability & Fronts · ACS K3a–K3f

Atmospheric Stability & the IFR Pilot

  • Stable air resists vertical motion — produces stratiform clouds, steady precipitation, poor visibility, smooth air
  • Unstable air promotes vertical motion — produces cumuliform clouds, showery precipitation, good visibility (outside precip), turbulence
  • Temperature inversions = extremely stable — trap moisture, haze, pollution below the inversion
  • Surface-based inversions are the #1 cause of morning low IFR (LIFR) conditions
  • Conditionally unstable: stable until lifted to saturation, then becomes unstable — classic setup for embedded thunderstorms
DPE Tip
DPEs love asking: "What kind of weather would you expect in stable vs. unstable air?" Stable = stratus, poor vis, smooth. Unstable = cumulus, turbulence, good vis between showers.
FAA-H-8083-28A Ch. 4

Lapse Rates & Stability Indicators

  • Standard lapse rate: 2°C per 1,000 ft (3.5°F/1,000 ft)
  • If ambient lapse rate > 3°C/1,000 ft → absolutely unstable (expect strong thermals, CB development)
  • If ambient lapse rate < moist adiabatic (~1.5°C/1,000 ft) → absolutely stable
  • Increasing lapse rate (surface heating) → destabilization → afternoon convection
  • Decreasing lapse rate (radiational cooling) → stabilization → nighttime fog and low stratus
DPE Tip
Know the difference between dry adiabatic (~3°C/1,000 ft) and moist/saturated adiabatic (~1.5-2°C/1,000 ft). The moist rate is less because condensation releases latent heat.
FAA-H-8083-28A Ch. 4

Air Masses & Their Weather

  • cP (continental Polar): Cold, dry, stable — brings clear skies but bitter cold in winter. Can become unstable over warm water (lake-effect snow)
  • mP (maritime Polar): Cool, moist — Pacific mP brings low stratus and rain to the West Coast; Atlantic mP brings fog and drizzle to the Northeast
  • mT (maritime Tropical): Warm, moist, unstable — Gulf of Mexico mT is the primary moisture source for thunderstorms east of the Rockies
  • cT (continental Tropical): Hot, dry, unstable at low levels — forms over deserts, causes extreme turbulence and dust devils
  • Source region determines initial properties; modification occurs as the air mass moves over different surfaces
FAA-H-8083-28A Ch. 5

Frontal Systems — IFR Weather Generators

  • Warm front: Warm air rides up over cold air — wide band (200+ NM) of stratiform clouds, steady precip, gradual lowering ceilings, poor visibility — classic IFR setup
  • Cold front: Cold air undercuts warm — narrow band (50 NM) of cumuliform clouds, heavy rain, turbulence, rapid clearing behind
  • Stationary front: Neither air mass advancing — prolonged poor weather, low ceilings, fog for days
  • Occluded front: Cold front overtakes warm front — combines hazards of both; wide area of clouds and precip
  • Cold-type occlusion: Cold front lifts warm front — most severe weather at the surface
DPE Tip
A warm front is the most likely to produce extended IFR conditions. DPEs will present a scenario where ceilings are gradually lowering — that screams warm front approach.
FAA-H-8083-28A Ch. 5

Frontal Weather Sequences

  • Approaching warm front: Cirrus → cirrostratus → altostratus → nimbostratus → stratus/fog. Pressure falling, wind shifting
  • Warm front passage: Temperature rises, pressure levels, visibility may improve, wind shifts clockwise (veers)
  • Approaching cold front: Altocumulus → cumulonimbus. Pressure falling, temp steady/warm
  • Cold front passage: Temperature drops, pressure rises sharply, wind shifts clockwise (veers), visibility improves after front passes
  • Worst icing: Just above the freezing level in stratiform clouds ahead of a warm front — extensive areas of freezing rain
FAA-H-8083-28A Ch. 5

Clouds as Stability Indicators

  • Stratiform (stratus, nimbostratus, altostratus): Stable air — continuous, layered, smooth, steady precip
  • Cumuliform (cumulus, cumulonimbus, towering Cu): Unstable air — vertical development, turbulence, showery precip
  • High clouds (cirrus family, >20,000 ft): Ice crystals — indicate upper-level moisture, approaching warm front
  • Lenticular clouds: Mountain wave indicator — smooth appearance but severe turbulence nearby
  • Standing lenticular clouds (ACSL) in PIREPs = mountain wave turbulence — stay well above or avoid
DPE Tip
If a DPE shows you a METAR with "SCT025 OVC080" and asks what it implies — scattered low layer (stable boundary layer) with overcast above (approaching front or moist layer aloft).
FAA-H-8083-28A Ch. 3

Wind Hazards & Turbulence · ACS K3d–K3e

Wind Shear — The Invisible Threat

  • Wind shear: Any rapid change in wind speed or direction over a short distance — horizontal or vertical
  • Low-level wind shear (LLWS): Most dangerous within 2,000 ft AGL, especially on approach
  • Associated with: fronts, thunderstorms, temperature inversions, jet streams, sea/land breezes
  • Microburst-induced shear: Headwind → tailwind transition can cause loss of 40-80 ft/min climb performance in seconds
  • LLWAS (Low-Level Windshear Alert System) at many airports — ATC will advise but coverage has gaps
  • If you encounter wind shear on approach: GO AROUND immediately. Apply max power, pitch for Vref + wind additive
DPE Tip
Classic checkride scenario: "You're on an ILS approach and tower reports LLWAS alert, wind shear on final. What do you do?" — Missed approach. No hesitation.
FAA-H-8083-28A Ch. 7; AIM 7-1-27

Mountain Wave Turbulence

  • Caused by strong winds (25+ kts) blowing perpendicular to a mountain ridge
  • Turbulence extends well above ridge height — can reach into the stratosphere
  • Rotor zone (below ridge height, downwind side): Most severe turbulence — can exceed structural limits
  • Cap cloud on peak, lenticular clouds downwind = visual indicators of mountain wave
  • PIREP mountain wave reports use "MWAVE" — always check these when crossing terrain
  • Rule of thumb: Fly at least 50% above ridge height, or avoid entirely if moderate+ wave reported
FAA-H-8083-28A Ch. 7

Turbulence Categories & Reporting

  • Light: Slight, erratic changes in altitude/attitude — occupants may feel a slight strain against seatbelts
  • Moderate: Changes in altitude/attitude, but aircraft remains in positive control — occupants feel definite strain; unsecured objects dislodged
  • Severe: Large, abrupt changes — aircraft may be momentarily out of control; occupants forced violently against seatbelts
  • Extreme: Aircraft practically impossible to control — may cause structural damage. IMMEDIATE heading/altitude change required
  • Report turbulence location, intensity, type (chop/CAT/MWAVE), altitude, aircraft type — PIREPs are the ONLY real-time turbulence data
LevelAircraftCabin
LightMomentary slight, erratic changes in altitude and/or attitude. Rhythmic bumpiness without appreciable change is Light ChopSlight strain against seat belts. Unsecured objects displaced slightly; walking is easy
ModerateSimilar to light but greater intensity. Changes occur but the aircraft remains in positive control at all times. Usually varies indicated airspeedDefinite strain against seat belts. Unsecured objects dislodged; walking is difficult
SevereLarge, abrupt changes in altitude and/or attitude, usually with large airspeed variations. Aircraft may be momentarily OUT OF CONTROLOccupants forced violently against seat belts. Objects tossed about; walking impossible
ExtremeAircraft violently tossed about and practically impossible to control. May cause structural damage

Duration is reported separately: Occasional is less than 1/3 of the time, Intermittent 1/3 to 2/3, Continuous more than 2/3.

DPE Tip
Don't conflate the scales: ICING is Trace / Light / Moderate / Severe, but TURBULENCE is Light / Moderate / Severe / Extreme — no "Trace," and it adds "Extreme."
AIM 7-1-21
Go Deeper
Question about icing envelopes, reading a TAF, or an IFR go/no-go call? Ask Kit for a CFI-level explanation.
Walk me through a go/no-go weather decision for an IFR cross-country

Training aid only — verify all data against your POH and current FAA publications.