Turbulence Intensity Categories

Turbulence is classified into four internationally recognised intensity categories. These definitions, used in PIREPs and weather advisories, describe both the effect on aircraft and on occupants.

Intensity PIREP Code Occupant Effect Aircraft Effect
Light LGT Slight strain against seat belts. Unsecured items may move. Food/drink service may be difficult. Slight erratic changes in altitude or attitude. Report as: slight/erratic variations in airspeed.
Moderate MOD Hard strain against seat belts. Unsecured items dislodged. Walking extremely difficult. Changes in altitude/attitude, IAS variations. Aircraft remains in positive control at all times.
Severe SVR Violent movement against seat belts. Impossible to walk. Possible injuries to unsecured occupants. Large, abrupt changes in altitude/attitude. Momentary loss of aircraft control. Large IAS variations.
Extreme EXTRM Impossible to remain seated. Significant risk of injuries. Aircraft practically impossible to control. Risk of structural damage. Report immediately to ATC.

Note on "Chop": PIREPs may also report LGT CHOP or MOD CHOP — this refers to rhythmic bumps without abrupt changes, typically caused by light mechanical turbulence. Less disruptive than the equivalent-intensity standard turbulence.

Types of Turbulence

Turbulence arises from several distinct atmospheric mechanisms. Understanding the cause of each type allows pilots to anticipate where and when it is likely, and how to avoid or escape it.

Convective / Thermal

Convective (Thermal) Turbulence

Caused by differential surface heating creating rising columns of air (thermals). Surfaces with high heat absorption — cities, dark ploughed fields, tarmac runways, and rocky terrain — generate stronger thermals than surrounding areas. Thermals vary in strength from gentle bubbles to powerful columns reaching cloud base.

When
Afternoon; sunny, low-humidity days
Location
Below and within Cu/TCu/Cb; boundary layer
Severity
Light–Moderate; Severe near TCu/Cb

Avoidance strategies:

  • Fly early morning before surface heating develops
  • Fly above the convective layer / cloud tops when possible
  • Increase cruise speed to Va (manoeuvring speed) in moderate or worse turbulence
  • Avoid flight below TCu or Cb cloud base
  • In hot conditions, plan routes over water or high terrain where thermals are weaker
Mechanical

Mechanical Turbulence

Created when wind flows over surface obstacles — hills, ridges, mountains, forests, buildings, and even other aircraft. The airflow separates and creates eddies and vortices downwind of the obstruction. Severity increases with wind speed and the size/sharpness of the obstacle.

When
Any time; worse with wind >15 kt near terrain
Location
Downwind of obstacles; low level near terrain
Severity
Light to Severe; Extreme in rotor zones

Mountain Wave

At a larger scale, strong winds flowing over mountain ridges can generate standing waves extending for hundreds of miles downwind and up to the stratosphere. These waves have three components:

  • Cap cloud / Banner cloud: cloud over the mountain peak; wave clouds (lenticular) are lens-shaped, stationary clouds forming in wave crests
  • Rotor zone: violent turbulent area below the wave crest on the lee side — can be Extreme intensity; lenticular cloud at rotor level may appear smooth but flight within is extremely hazardous
  • Wave train: series of updraught/downdraught cycles downwind; can cause significant altitude deviations

Avoidance: Cross ridges at right angles; avoid the lee side in strong wind; give wide vertical clearance above ridge height; do not fly below lenticular clouds. Increase to Va.

Clear Air Turbulence

Clear Air Turbulence (CAT)

CAT occurs in clear air without any cloud or visual indication — making it essentially impossible to detect or avoid visually. It is primarily associated with the strong wind shear zones around the jet stream, where speed and/or direction changes rapidly over a short distance.

Altitude
Typically FL250–FL400
Associated with
Jet stream >80 kt; tropopause edges
Detection
PIREPs only; no visual clue
Severity
Moderate to Severe; occasionally Extreme

Location indicators:

  • Edges of the jet stream — particularly the equatorward (warm) side where wind shear is greatest
  • Areas where the tropopause height changes sharply (jet stream entrance and exit regions)
  • Lee side of mountains at high altitude (mountain wave CAT)
  • Near active thunderstorm systems — turbulence can extend many miles laterally in clear air

Detection and avoidance:

  • PIREPs (pilot reports) from preceding aircraft are the most reliable current source
  • Winds aloft charts and jet stream forecasts aid planning
  • Some modern long-range radar systems and LIDAR can detect CAT; most aircraft cannot
  • If jet stream core winds are forecast above 80 kt, expect potential CAT near the edges

Response to unexpected CAT: Slow to Va, maintain attitude (do not chase altitude), inform ATC, request level change if possible, file PIREP on exit.

Wake Turbulence

Wake Turbulence

All aircraft generating lift produce two counter-rotating vortices trailing from the wingtips. These vortices are generated from the moment of rotation on takeoff until touchdown on landing. They represent one of the most dangerous hazards in the terminal area, capable of rolling a smaller aircraft beyond its ability to recover.

Sink rate
300–500 ft/min
Persistence
Up to 3 minutes in calm air
Drift
With the crosswind component
Worst conditions
Heavy, slow, clean configuration

ICAO Wake Turbulence Categories (WTC):

CategoryMTOWExamples
Super (J)>560,000 kgA380
Heavy (H)>136,000 kgB747, B777, A330
Upper Medium (UM)15,000–136,000 kgA320, B737
Medium (M)7,000–136,000 kgATR-72, Dash 8
Light (L)<7,000 kgC172, PA-28

Key rules for avoiding wake turbulence:

  • ATC provides mandatory separation based on WTC categories — do not waive this without understanding the risk
  • On approach: stay at or above the preceding aircraft's glidepath; land beyond the preceding aircraft's touchdown point
  • On departure: rotate before the preceding aircraft's rotation point; turn early to avoid the flight path
  • Vortices drift with crosswind — on a right crosswind, the upwind vortex may remain over the runway; on a left crosswind, it drifts away from the runway
  • In calm wind conditions, vortices may remain on the runway for up to 3 minutes — use caution with low-wind operations behind heavy aircraft
  • Request additional separation from ATC if needed; it is always the PIC's responsibility to ensure safe separation

PIREP Turbulence Encoding

Turbulence encounters must be reported as Pilot Reports (PIREPs). Accurate PIREPs are the most valuable real-time weather information available to other pilots and forecasters. The standard format for a turbulence PIREP:

// Standard PIREP turbulence group
/TB [intensity] [type] [altitude or altitude range]

// Examples:
/TB LGT // Light turbulence
/TB MOD-SVR // Moderate to Severe
/TB LGT CHOP // Light Chop (rhythmic)
/TB NEG // Negative (no turbulence encountered)
/TB EXTRM // Extreme — report immediately to ATC

Example complete PIREP decoded:

UA /OV EGCC /TM 1430 /FL095 /TP C172 /SK BKN070 /TB MOD /RM PIREP

UA = Routine PIREP
OV = Over EGCC (Manchester Airport)
TM = Time 1430Z
FL = Flight Level 095 (9,500 ft)
TP = Aircraft type C172
SK = Sky: Broken at 7,000 ft
TB = Turbulence: Moderate
RM = Remarks: PIREP (routine)

Filing a PIREP: Report to ATC as soon as practicable after encountering unexpected turbulence. Include: position (overhead or between two points), time, altitude, aircraft type, and intensity/type. In the UK, PIREPs are forwarded to the Met Office. In many jurisdictions, failing to report encountered phenomena is considered a duty of care issue.

Pilot Response to Turbulence

Unexpected Turbulence Encounter

When to Divert

Seat belts: Passengers should be instructed to keep seat belts fastened whenever seated. The majority of turbulence injuries occur to unsecured passengers and cabin crew during unexpected moderate or severe turbulence encounters in cruise flight at high altitude — often in VMC with no apparent weather.