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
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
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
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
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
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
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
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
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
| Level | Aircraft | Cabin |
|---|---|---|
| Light | Momentary slight, erratic changes in altitude and/or attitude. Rhythmic bumpiness without appreciable change is Light Chop | Slight strain against seat belts. Unsecured objects displaced slightly; walking is easy |
| Moderate | Similar to light but greater intensity. Changes occur but the aircraft remains in positive control at all times. Usually varies indicated airspeed | Definite strain against seat belts. Unsecured objects dislodged; walking is difficult |
| Severe | Large, abrupt changes in altitude and/or attitude, usually with large airspeed variations. Aircraft may be momentarily OUT OF CONTROL | Occupants forced violently against seat belts. Objects tossed about; walking impossible |
| Extreme | Aircraft 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.
Key Takeaways
- Clear ice (large supercooled drops / freezing rain) is the most dangerous; structural icing needs visible moisture and roughly -15°C to +2°C.
- Ice can raise stall speed 20–30% WITHOUT a stall warning — if the airplane feels sluggish in ice, act, don't wait for the horn.
- A thunderstorm's mature stage (updrafts + downdrafts) is the most dangerous; stay 20 NM from severe cells, never fly under or between close cells, never top a building storm.
- Microbursts give a headwind-then-tailwind shear on approach — max power, pitch up, go around; advection fog (warm moist air over a cold surface) can persist for days.
Aircraft Icing · ACS K3g–K3h
Types of Structural Icing
- Clear ice: Hard, heavy, transparent — forms from large supercooled droplets that flow back before freezing. Most hazardous — difficult to see and remove
- Rime ice: Rough, milky, opaque — forms from small supercooled droplets that freeze instantly on contact. Easier to remove with deice boots
- Mixed ice: Combination of clear and rime — characteristics of both types. Common in rapidly changing conditions
- Frost: Forms on cold-soaked surfaces when dew point is below freezing. Reduces lift up to 30% — NEVER take off with frost on wings
- SLD (Supercooled Large Droplets): Extremely hazardous — can accumulate behind protected surfaces and in areas boots/TKS can't reach
Icing Conditions & Temperature Envelope
- Structural icing requires TWO ingredients: visible moisture AND temperature at or below 0°C
- Most likely between -15°C and +2°C (supercooled water droplet range)
- Peak icing risk: -10°C to 0°C — where supercooled liquid water content is highest
- Below -15°C: Most moisture is ice crystals that bounce off the airframe (less icing risk)
- Below -40°C: All moisture is ice crystals — no icing risk
- Freezing rain = temperature inversion overhead — warmer air aloft is melting precipitation that refreezes on contact. Climbing MAY find warmer air, but verify with PIREPs
Effects on Aircraft Performance
- Increased weight AND drag — decreased lift coefficient
- Disrupted airflow over wings — effective stall speed increases (stalls at higher airspeed)
- Stall warning may NOT activate — ice changes the airfoil shape before reaching the stall AOA
- Unprotected surfaces (antennas, gear, pitot tube, static ports) accumulate ice rapidly
- Pitot tube blockage → erroneous airspeed (reads low or zero). Turn on pitot heat proactively before entering known moisture
- Propeller icing reduces thrust efficiency — RPM may decrease
- Tailplane icing: Can cause pitch-down moment when flaps are lowered (NASA tailplane icing studies)
Pilot Actions & Regulatory Framework
- 14 CFR §91.527: No person may fly under IFR into known or forecast icing unless equipped for it (applies to large/turbine aircraft)
- For Part 91 small aircraft: No explicit FAR prohibition, but "known icing" is defined by the certification standards — if not certified for flight into known icing (FIKI), don't do it
- Exit icing conditions immediately — change altitude or route. Every minute adds weight
- Use all available anti-ice/deice equipment at the FIRST sign of accumulation
- Increase approach speed 10-20% to account for increased stall speed from residual ice
- Report icing via PIREP: Trace, Light, Moderate, Severe — include altitude, temperature, aircraft type
- Pre-flight: Clean aircraft of ALL frost, ice, and snow before takeoff — no exceptions
Icing PIREPs — Intensity Scale
- The current AIM defines the four intensities by a representative ACCRETION RATE on the unprotected outer wing — see the table below
- Trace and Light both say "consider exiting"; Moderate says "as soon as possible"; Severe is the only one where exit is required by regulation
- Severe is aircraft-dependent — it may occur at ANY accumulation rate when the rate or accumulation exceeds what your aircraft tolerates
- Expect icing in visible moisture between +2 °C and −10 °C
- When reporting: Include type (rime/clear/mixed), intensity, altitude, temperature, and aircraft type — a Cessna 172 accumulates differently than a King Air
| Level | Rate | Means |
|---|---|---|
| Trace | Under ¼ in/hr | Ice becomes noticeable; accumulation slightly exceeds sublimation. Consider exiting before it worsens |
| Light | ¼ to 1 in/hr | Requires occasional cycling of manual deicing systems. Consider exiting |
| Moderate | 1 to 3 in/hr | Requires frequent cycling of manual deicing systems. Consider exiting as soon as possible |
| Severe | Over 3 in/hr | Ice protection systems FAIL to remove it and ice forms where it normally does not. By regulation, immediate exit is required |
Rates are representative accretion on the unprotected part of the outer wing. Severe is aircraft-dependent — it can occur at any rate that exceeds what your airplane tolerates.
Thunderstorms & Convection · ACS K3i–K3j
Three Stages of Thunderstorms
- Cumulus (Developing): Updrafts ONLY — building upward, rain not yet reaching surface. Looks harmless but can intensify rapidly
- Mature: Most dangerous stage — both updrafts AND downdrafts coexist. Heaviest rain, hail, lightning, wind shear, microbursts
- Dissipating: Downdrafts dominate — rain decreasing, anvil top spreading. STILL DANGEROUS — contains turbulence and wind shear
- A single cell lasts 20-90 minutes. Multi-cell clusters and supercells can persist for hours
- Three ingredients for TS development: moisture, instability (lifting mechanism), and a trigger (fronts, terrain, convergence, heating)
Thunderstorm Hazards for IFR Flight
- Severe turbulence: Can exceed structural limits of GA aircraft (exceeds ±25 ft/sec gust loads)
- Hail: Can occur in clear air up to 20 NM from the storm. Hail shafts can be invisible to radar
- Lightning: Temporarily blinds pilots, can damage avionics, magnetize compass, punch holes in skin
- Microbursts: 4,000 ft diameter, winds up to 150 kts — headwind-to-tailwind transition on approach
- Tornadoes: Associated with supercell thunderstorms, extending from cloud to ground
- Heavy precipitation: Obscures visibility, ingestion can cause engine flameout
- Gust front: Leading edge of cold air outflow can extend 15-20 NM ahead of the storm
Microbursts — The Silent Killer
- A microburst is a localized column of sinking air within a thunderstorm — produces damaging divergent winds at the surface
- Size: 1-3 NM diameter. Duration: 5-15 minutes from first contact to dissipation
- Peak intensity reached within 5 minutes of initial outflow — no time to react if on approach
- Headwind-to-tailwind shear: Aircraft initially gains airspeed (pilot reduces power), then rapidly loses airspeed and altitude
- Can produce winds up to 150 kts. Delta-V (total velocity change) can exceed 90 kts
- Dry microbursts: Occur in arid regions — precipitation evaporates before reaching ground. No visual cue!
- Wet microbursts: Occur in moist environments — visible rain shaft can indicate location
- If encountered: Apply MAX power, pitch to 15° nose-up, accept stall warning — priority is arresting descent rate
Thunderstorm Avoidance Rules
- Maintain at least 20 NM from any severe thunderstorm or intense radar echo
- Do NOT attempt to fly under a thunderstorm — turbulence and downdrafts extend to the surface
- Do NOT fly between cells that are less than 40 NM apart — the gap may be filled with severe turbulence
- Circumnavigate the entire area if storms are embedded (cannot identify individual cells)
- Avoid the anvil — severe turbulence and hail extend well above and downwind
- Do NOT rely solely on onboard radar or datalink weather — datalink has 5-20 minute latency!
- At night, embedded thunderstorms are especially dangerous — no visual avoidance cues
- Do NOT attempt to "top" a building thunderstorm — they can build at 6,000 ft/min
Embedded Thunderstorms (Critical IFR Hazard)
- Thunderstorms hidden within widespread stratiform cloud layers — cannot be seen visually
- Most commonly associated with warm fronts and squall lines in moist, unstable air masses
- SIGMET or Convective SIGMET will be issued when embedded thunderstorms are occurring or forecast
- Onboard weather radar is the only real-time tool for detecting embedded TS — request vectors from ATC if not equipped
- Continuous lightning illumination from within a cloud layer at night = embedded TS
- If you inadvertently enter one: Maintain attitude, keep wings level, accept altitude deviations, slow to maneuvering speed (Va), don't chase the instruments
Fog, Visibility & Ground Icing · ACS K3k–K3l
Types of Fog — IFR Pilot's Primary Adversary
- Radiation fog: Clear nights, light winds (<5 kts), moist air — forms in low-lying areas, burns off 1-3 hours after sunrise
- Advection fog: Warm moist air moves over cold surface — can persist for DAYS, common on coasts. Wind 5-15 kts helps maintain it
- Upslope fog: Air forced uphill cools adiabatically to dew point — common in mountains. Can be thick and persistent
- Steam fog (arctic sea smoke): Cold air over warm water — shallow but can be dense. Common over lakes/rivers in fall
- Precipitation-induced fog: Rain from warmer air aloft saturates cooler air below — common ahead of warm fronts
- Freezing fog: Fog with temps below 0°C — deposits ice on aircraft and runway. Extremely hazardous for takeoff and landing
Visibility Considerations for IFR
- Temp/dew point spread ≤3°C: Fog or low clouds likely developing. ≤1°C: almost certain
- Flight visibility vs. ground visibility: §91.175 — YOU must have the required flight visibility to descend below MDA/DA
- Prevailing visibility in METARs is "representative" — actual conditions vary across the airport environment
- LIFR (Low IFR): Ceiling <500 ft AND/OR vis <1 SM — consider whether you're proficient enough to attempt
- RVR (Runway Visual Range): Measured by transmissometers along the runway. Used for precision approaches when vis < 1 SM
- Sector visibility: Some METARs report variable visibility by compass direction — check remarks section
Obstructions to Visibility
- Haze (HZ): Fine particles, visibility typically 3-5 SM — slant range visibility much worse than reported ground vis
- Smoke (FU): From fires, industrial sources — can reduce visibility to near zero. Check NOTAMs for wildfire areas
- Volcanic ash (VA): Extremely hazardous — can cause engine failure (melts in combustion chamber, solidifies on turbine blades)
- Dust/sand (DU/SA): Common in desert regions — haboobs can reduce vis to zero in minutes
- Blowing snow (BLSN): Can produce whiteout conditions on approach and departure
- Mist (BR): Vis 5/8 SM to 6 SM with moisture. Fog (FG): Vis < 5/8 SM. Know the difference for METAR decoding
Frost & Ground Icing
- Frost forms on aircraft surfaces when the skin temperature is at or below 0°C AND the dewpoint — NO visible moisture required
- Even a thin layer of frost disrupts airflow — increases stall speed, reduces lift, reduces climb performance
- 14 CFR §91.527(a): "No pilot may take off when frost, ice, or snow is adhering to wings, control surfaces, or propellers"
- Polished frost: The most deceptive — thin, transparent coating that may appear harmless but still disrupts laminar flow
- Deicing vs. anti-icing: Deicing removes existing contamination; anti-icing prevents new accumulation. Know the holdover times
- Cold-soaked fuel tanks: Fuel in wing tanks can cool wing skin below ambient — frost forms even above 0°C ambient when humidity is high
Key Takeaways
- Flight categories: VFR >3,000 & >5 SM; MVFR 1,000–3,000 and/or 3–5; IFR 500–999 and/or 1–2; LIFR <500 and/or <1 — judged on the WORST of ceiling/vis.
- TAFs cover a 5 SM radius for 24–30 hours; watch FM/BECMG/TEMPO/PROB groups, and TAF/FB winds are TRUE (ATIS/AWOS are magnetic).
- AIRMETs (moderate): Sierra = IFR/mountain obscuration, Tango = turbulence/winds, Zulu = icing; SIGMETs and Convective SIGMETs are severe.
- PIREPs are the ONLY real-time source of actual cloud tops, icing, and turbulence — and datalink (FIS-B/XM) is 5–20 min old, strategic only.
METAR & TAF Decoding · ACS K1–K2
METAR Decoding — Beyond the Basics
- Type: METAR (routine) or SPECI (special — issued when significant weather changes occur between routines)
- Wind: First 3 digits = direction (true north), next 2-3 = speed, G = gusts. VRB = variable direction when speed <6 kts
- Visibility: In statute miles (US). P6SM = "plus 6 SM." RVR reported in feet when vis drops below 1 SM
- Weather: Intensity prefix (- light, moderate (no prefix), + heavy), descriptor (TS, SH, FZ, DR, BL, MI, PR, BC), type (RA, SN, FG, BR, HZ, etc.)
- Clouds: SKC/CLR/FEW/SCT/BKN/OVC + altitude in hundreds of feet AGL. "CB" or "TCU" appended when observed
- Ceiling: The LOWEST broken (BKN) or overcast (OVC) layer. FEW and SCT are NOT ceilings
- Remarks (RMK): Critical info — peak wind, pressure tendency, lightning, variable ceiling/vis, maintenance data
TAF Decoding — The IFR Planning Backbone
- Issued 4x daily for 24 or 30 hours. Covers a 5 SM radius around the airport
- FM (From): Complete change in conditions at the specified time. Previous conditions no longer valid
- TEMPO: Temporary fluctuation expected for <1 hour at a time, covering <50% of the period
- BECMG: Gradual, permanent change expected over the 2-hour period specified
- PROB30/PROB40: 30% or 40% probability of conditions during the period. Not used within first 9 hours of TAF
- AMD: Amended forecast. COR: Corrected. RTD: Delayed. NIL: Missing
- TAF winds are TRUE direction (unlike ATIS/AWOS which report magnetic)
- NSW: No Significant Weather expected — cancels previous weather phenomena
Flight Categories — Know the Thresholds
- VFR: Ceiling >3,000 ft AND visibility >5 SM
- MVFR (Marginal VFR): Ceiling 1,000-3,000 ft AND/OR visibility 3-5 SM
- IFR: Ceiling 500 to less than 1,000 ft AND/OR visibility 1 to less than 3 SM
- LIFR (Low IFR): Ceiling <500 ft AND/OR visibility <1 SM
- These are based on the WORST condition — if ceiling is 600 ft (IFR) but vis is 8 SM (VFR), category is IFR
- On GFA and other charts: VFR = green, MVFR = blue, IFR = red, LIFR = magenta
Advisories, PIREPs & Forecasts · ACS K2
AIRMETs (WA) — Widespread Moderate Hazards
- AIRMET Sierra (S): IFR conditions (ceilings <1,000 ft and/or vis <3 SM over >50% of area) and/or mountain obscuration
- AIRMET Tango (T): Moderate turbulence, sustained surface winds ≥30 kts, low-level wind shear (non-convective)
- AIRMET Zulu (Z): Moderate icing and freezing level information
- Valid for 6 hours, reissued every 6 hours, amended as needed
- Significant to ALL aircraft, but especially light GA aircraft — a "moderate" hazard in an AIRMET is defined for light aircraft
- If you see AIRMET Zulu covering your route: evaluate altitude options to stay above freezing level or below the icing layer
SIGMETs (WS) — Severe Hazards
- SIGMET: Severe icing not associated with thunderstorms, severe or extreme turbulence, dust/sandstorms reducing vis <3 SM, volcanic ash
- Valid for 4 hours (6 hours for volcanic ash)
- Convective SIGMET (WST): Severe thunderstorms (surface winds ≥50 kts, hail ≥¾″, tornadoes)
- Also issued for: Embedded TS, line of TS, area of TS ≥40% of an area
- Convective SIGMETs valid for 2 hours, updated hourly. Issued for Eastern, Central, and Western US
- Any convective SIGMET implies: severe or greater turbulence, severe icing, and low-level wind shear
PIREPs (UA/UUA) — The Only Real-Time Reports
- UA = Routine pilot report. UUA = Urgent pilot report (severe icing, severe turbulence, etc.)
- ONLY real-time source of: actual cloud tops/bases, icing type/intensity, turbulence type/intensity, flight conditions between reporting stations
- Format: /OV (location) /TM (time) /FL (altitude) /TP (aircraft type) /SK (sky condition) /WX (weather) /TA (temperature) /WV (wind) /TB (turbulence) /IC (icing) /RM (remarks)
- ATC may solicit PIREPs — especially during approaches in changing conditions
- YOU should file: When encountering conditions different from forecast, especially icing, turbulence, or cloud tops. Contact FSS (122.0) or ATC
- Absence of PIREPs does NOT mean conditions are good — it may mean nobody is flying there
Winds & Temperatures Aloft Forecast (FB)
- Issued 2x daily, valid at 6, 12, and 24 hours
- Stations at 3,000, 6,000, 9,000, 12,000, 18,000, 24,000, 30,000, 34,000, 39,000 ft MSL
- No wind reported for levels within 1,500 ft of station elevation (too close to surface turbulence)
- Temperature not reported for the 3,000 ft level
- Format: 4-digit wind direction/speed (9900 = light and variable). Above 100 kts: add 50 to direction, subtract 100 from speed
- Negative temperatures indicated by "1" in the first digit of temperature field (e.g., "2722-12" = 270° at 22 kts, -12°C)
- Critical for: flight planning fuel burn, icing avoidance (check temps at planned altitude), wind component calculations
Graphical Forecast for Aviation (GFA) & Convective Outlook
- GFA: Web-based interactive tool at aviationweather.gov — replaced the legacy Area Forecast (FA)
- Provides: clouds, visibility, precipitation, TS, turbulence, icing — observations + forecasts out to 18 hours
- Layers can be toggled: Surface, Low, Mid, High. Click on any grid point for detailed info
- Use GFA alongside METARs and TAFs for the complete picture — GFA fills the gaps between reporting stations
- Convective Outlook (AC): Issued by Storm Prediction Center — shows probability of thunderstorms. Marginal/Slight/Enhanced/Moderate/High risk areas
- If "Moderate" or "High" risk covers your route → plan for significant delays or cancellation
Center Weather Advisories (CWA) & AIRMETS G-AIRMET
- CWA: Issued by ARTCC (Center) weather service units — more localized and time-critical than AIRMETs/SIGMETs
- Valid for 2 hours. Often the FIRST advisory product for rapidly developing conditions
- May be issued before a SIGMET when conditions are developing but criteria not yet fully met
- G-AIRMET: Graphical version of AIRMETs — issued every 6 hours with 3-hour snapshots out to 12 hours
- G-AIRMET is more precise geographically than text AIRMETs — shows exact boundaries of hazard areas
- Both available on aviationweather.gov — check before filing and again right before departure
Key Takeaways
- Start with a Standard briefing; an Outlook briefing (6+ hrs out) is planning-only — get a Standard/Abbreviated before departure.
- Work the go/no-go top-down: big picture → departure → en route (PIREPs / AIRMETs / SIGMETs) → destination → alternate → personal minimums → fuel.
- An alternate is required unless the destination meets the 1-2-3 rule (≥2,000 ft & ≥3 SM, ±1 hr of ETA); standard alternate mins are 600-2 / 800-2.
- Legal minimums are the floor — set higher personal minimums, run IMSAFE and PAVE, and beat get-there-itis.
Briefings, Go/No-Go & Decision Making · ACS R1–R2, S1–S4
Types of Weather Briefings
- Standard Briefing: Request when you have not received a previous briefing. Most complete — covers all elements. Always start here.
- Abbreviated Briefing: When updating a previous briefing, or need only specific information. Tell the briefer what you already know.
- Outlook Briefing: For flight planned 6+ hours in the future. General weather trends — you MUST get a Standard or Abbreviated before departure.
- Sources: 1800wxbrief.com (Leidos), ForeFlight (FAA-approved), aviationweather.gov, or call 1-800-WX-BRIEF
- Always tell the briefer: aircraft type, IFR/VFR, departure point, route, destination, ETD, altitude, duration
- Standard briefing includes: adverse conditions, VFR flight not recommended (if applicable), synopsis, current conditions, en route forecast, destination forecast, winds aloft, NOTAMs, ATC delays
Go/No-Go Decision Framework
- Step 1: Get the big picture — frontal positions, pressure systems, where is the weather moving?
- Step 2: Check departure conditions — METAR, TAF, departure procedure requirements (ODP minimums)
- Step 3: Analyze en route weather — PIREPs (icing? turbulence?), AIRMETs/SIGMETs, GFA cloud/precip layers
- Step 4: Evaluate destination — TAF, approach minimums vs. forecast weather, trends (improving or deteriorating?)
- Step 5: Alternate planning — Required? Does alternate weather meet the 1-2-3 or 600-2 rule? (See regulations module)
- Step 6: Personal minimums check — Am I current? Proficient? Rested? Is this within MY personal minimums, not just legal minimums?
- Step 7: Fuel — Can I get there, attempt the approach, miss, fly to alternate, and have 45 min reserve?
Personal Minimums — Your Safety Buffer
- Legal minimums are the FLOOR, not the target — personal minimums should always be higher
- Consider ceiling, visibility, crosswind, icing, currency/proficiency, aircraft equipment, terrain, and night factors
- New instrument pilot suggestion: Start with minimums well above published (e.g., 1,000 ft ceiling / 3 SM vis) and lower gradually with experience
- Raise your minimums when: Flying an unfamiliar aircraft or approach, night IFR, mountainous terrain, limited recent IFR time
- The IMSAFE checklist for the PILOT: Illness, Medication, Stress, Alcohol, Fatigue, Eating (nutrition)
- The PAVE checklist: Pilot, Aircraft, enVironment, External pressures — evaluate each before every flight
- Document your personal minimums in writing and review them periodically — easier to follow a plan than to make decisions under pressure
Alternate Airport Requirements (§91.169)
- An alternate is required if the destination forecast (1 hour before to 1 hour after ETA) shows: ceiling <2,000 ft above the airport OR visibility <3 SM
- This is the "1-2-3 Rule": 1 hour before/after, 2,000 ft ceiling, 3 SM visibility
- Alternate minimums (standard): Precision approach — 600 ft ceiling / 2 SM vis. Non-precision — 800 ft ceiling / 2 SM vis
- Non-standard alternate minimums: Shown by a triangle with "A" (▲A) on approach plates — check the actual values
- Some airports are "NA" (Not Authorized) as alternates — usually due to lack of weather reporting
- You can file without an alternate if destination has weather reporting AND forecast meets 1-2-3 rule — but always have a backup plan
- Fuel requirement: Enough to fly to destination, attempt approach, fly to alternate, and then fly 45 minutes at normal cruise
In-Flight Weather Updates & Diversion
- HIWAS: Hazardous In-Flight Weather Advisory Service — broadcast on selected VORs. Listen on en route VOR frequencies
- Flight Watch: Discontinued in 2015. Use 122.0 to contact FSS for PIREPs and updates
- ATC: Request current weather at your destination or alternate. Controllers can relay METARs, PIREPs, and SIGMET info
- ADS-B In: If equipped, provides FIS-B (Flight Information Service - Broadcast) with METARs, TAFs, SIGMETs — remember: 5-20 min latency
- Diversion triggers: Weather worse than forecast at destination, icing or turbulence exceeding aircraft/pilot capabilities, fuel remaining below personal minimums
- If diverting: Advise ATC immediately, request amended clearance to your alternate or nearest suitable airport, declare emergency if fuel is critical
- Never let "get-there-itis" override your training — the cemetery is full of pilots who pressed on into weather they shouldn't have
Onboard Weather Equipment — Uses & Limitations
- Airborne weather radar: Active system — shows precipitation intensity in real-time. Best for tactical TS avoidance. Tilt management is critical
- Stormscope/lightning detection: Passive system — plots electrical discharges. Shows where lightning IS, not where rain is. Good supplement to radar
- ADS-B In (FIS-B): Mosaic NEXRAD, METARs, TAFs, SIGMETs, PIREPs displayed on MFD. STRATEGIC use only (5-20 min latency)
- XM/SiriusXM Weather: Similar to FIS-B but subscription-based. Also strategic, not tactical. 5-15 min latency
- CRITICAL: Neither FIS-B nor XM weather is real-time — NEVER use for tactical avoidance (threading between cells)
- Best practice: Use datalink for strategic routing (planning), airborne radar for tactical avoidance (maneuvering)
- Icing detection: Some aircraft have ice detection systems (icing rate probes). Most GA aircraft rely on visual checks and OAT gauge
Training aid only — verify all data against your POH and current FAA publications.