Meteorology — PPL(A)

Weather theory, pressure systems, fronts, cloud types, icing, and how to read METARs and TAFs for UK VFR decision-making.

Exam Focus

Most Relevant To

  • Meteorology
  • Navigation
  • Operational Procedures

Know This Cold

  • METAR and TAF decode — every group, in order.
  • Frontal characteristics: warm front approach signs vs. cold front approach signs.
  • Pressure: QNH, QFE, QNE — when to use each, and what they reference.
  • Cloud types associated with stable and unstable air.
  • Icing types and conditions that produce them.
  • ISA standard atmosphere values.

The Atmosphere

The troposphere is the layer you fly in — it extends to roughly 36,000 ft in mid-latitudes. Temperature decreases with altitude at the Environmental Lapse Rate (ELR). When ELR exceeds the Dry Adiabatic Lapse Rate (DALR), the atmosphere is unstable; convective cloud and turbulence result.

  • ISA sea level: 15°C, 1013.25 hPa, density 1.225 kg/m³.
  • ISA temperature lapse rate: 2°C per 1,000 ft (troposphere).
  • DALR: 3°C per 1,000 ft (unsaturated air rising).
  • SALR: approximately 1.5°C per 1,000 ft (saturated air rising — varies with temperature).
  • Tropopause: approximately 36,000 ft at mid-latitudes (lower at poles, higher at equator).

Pressure Systems and Wind

In the northern hemisphere, wind circulates anticlockwise around a low (cyclone) and clockwise around a high (anticyclone). Buys Ballot's Law: stand with the wind on your back, low pressure is to your left. Surface friction backs the wind slightly toward the low.

  • Low pressure: ascending air, cloud development, instability, poor weather, strong winds.
  • High pressure: descending air, stable conditions, radiation fog risk, inversions.
  • Isobars close together: strong pressure gradient, strong winds.
  • Isobars far apart: weak gradient, light winds.
  • Veering: wind changing clockwise (S → W). Backing: anti-clockwise (W → S).

Instructor Tip

The exam often asks about wind at altitude vs. surface. Above 2,000 ft, friction disappears and wind backs and strengthens compared to the surface reading — important for drift calculations.

Frontal Weather

A front is the boundary between two air masses of different temperature and humidity. Frontal systems are responsible for the majority of UK weather changes and in-flight hazards.

  • Warm front: shallow angle (~1:150), approaches with Ci → Cs → As → Ns. Persistent rain ahead, low cloud after passage.
  • Cold front: steeper angle (~1:50), approaches quickly. Towering Cb, heavy showers, squalls, rapid clearance after passage.
  • Occluded front: cold front catches warm front. Complex weather; properties depend on warm or cold occlusion.
  • Warm sector: between warm and cold fronts. Stratus, drizzle, poor visibility, stable.

Common Mistake

Students confuse which cloud sequence belongs to warm vs. cold fronts. Warm front clouds develop gradually from high to low — you have time to divert. Cold fronts arrive with little warning and intense convective weather.

Cloud Types

  • Cirrus (Ci): high-level ice, fibrous streaks — first sign of an approaching warm front.
  • Cirrostratus (Cs): high-level sheet — halos around sun or moon.
  • Altostratus (As): mid-level grey sheet — sun appears as through ground glass.
  • Nimbostratus (Ns): thick, dark, continuous rain — instrument conditions.
  • Stratocumulus (Sc): low lumpy layer — common UK cloud, generally benign.
  • Stratus (St): low featureless layer — poor visibility, drizzle, common in warm sector.
  • Cumulus (Cu): vertical development, associated with instability.
  • Cumulonimbus (Cb): severe thunderstorm cloud — icing, turbulence, lightning, windshear. AVOID.

Icing

Airframe icing is a serious hazard. It adds weight, degrades aerofoil shape, blocks pitot/static sources, and can jam controls. Understanding when and where icing occurs is essential for exam and for safe VFR operation.

  • Rime ice: rough, opaque — forms in cloud with small supercooled droplets. Freezing level to −20°C.
  • Clear ice: smooth, dense — forms in large supercooled droplets or freezing rain. Most dangerous. Adds most weight.
  • Hoar frost: crystalline surface frost — forms below 0°C on ground, not in flight.
  • Most icing risk: just above the freezing level in cloud. Temperature −2°C to −20°C.
  • Severe icing: Cb, frontal cloud, freezing rain (warm air over-running cold).

Instructor Tip

The exam often asks: "At which temperature is clear ice most likely to form?" Answer: 0°C to −10°C where large supercooled water droplets are most abundant.

Reading a METAR

A METAR is a routine aerodrome weather observation. Decode left to right: type, ICAO, time, wind, visibility, weather, cloud, temperature/dewpoint, QNH, trends/remarks.

  • METAR EGLL 121250Z — EGLL, 12th at 12:50 UTC.
  • Wind: 24015KT — 240° true at 15 kt. Gusting: 24015G25KT.
  • Visibility: 9999 — 10 km or more. 0600 — 600 m.
  • Weather: -RA (light rain), +TSRA (heavy thunderstorm with rain), BR (mist), FG (fog), RASN (rain and snow).
  • Cloud: FEW018 BKN030 — few at 1,800 ft, broken at 3,000 ft. OVC = overcast.
  • Temperature/Dewpoint: 12/09 — +12°C, dewpoint +9°C.
  • QNH: Q1013 — altimeter setting 1013 hPa.
  • CAVOK: visibility ≥10 km, no cloud below 5,000 ft or MSA, no significant weather.

Reading a TAF

A TAF is an aerodrome forecast, typically 9 or 24 hours. Groups indicate changes: BECMG (gradual change), TEMPO (temporary, less than half the period), PROB30/40 (probability).

  • BECMG 1416: gradual change between 14:00 and 16:00 UTC.
  • TEMPO 1820: temporary condition between 18:00 and 20:00 (each occurrence < 60 min).
  • PROB30 TEMPO: 30% probability of temporary condition — treat as possible, not probable.
  • PROB40: 40% probability. PROB40 TEMPO is more likely and must be planned against.
  • FM1400: from 14:00 UTC — replaces all previous conditions.

Common Mistake

PROB30 groups are often ignored by students. The exam will describe PROB30 conditions and ask if the flight is still legal. You must have an alternate or fuel to cover the possibility.

Key Formulas and Values

ISA temperature at altitude

T = 15 − (alt/1000 × 2)

Altitude in feet, result in °C

Density altitude (simplified)

DA = PA + (ISA dev × 120)

ISA dev = actual temp − ISA temp at PA

DALR

3°C per 1,000 ft

Unsaturated rising air

SALR

~1.5°C per 1,000 ft

Saturated rising air (varies)