Turbulence
Turbulence
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30.Apr.2024
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SKYbrary Aviation Safety. (April 30, 2024). Turbulence.
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Description
Turbulence is caused by the relative movement of disturbed air through which an aircraft is flying. Its origin may be thermal or mechanical and it may occur either within or clear of cloud. The absolute severity of turbulence depends directly upon the rate at which the speed or the direction of airflow (or both) is changing, although perception of the severity of turbulence which has been encountered will be affected by the mass of the aircraft involved.
Significant mechanical turbulence will often result from the passage of strong winds over irregular terrain or obstacles. Less severe low level turbulence can also be the result of convection occasioned by surface heating.
Turbulence may also arise from air movements associated with convective activity, especially in or near a thunderstorm or due to the presence of strong temperature gradients near to a Jet Stream. Jet Stream Turbulence, like turbulence caused by Mountain Waves, which can form downwind of ridges, occurs clear of cloud and in the form of Clear Air Turbulence (CAT) (CAT).
Very localised, but sometimes severe, Wake Vortex Turbulence may be encountered when following or crossing behind another aircraft. This turbulence is due to wing tip trailing vortices generated by the preceding aircraft; however, this phenomena is distinctively transient.
Air moving over or around high ground may create turbulence in the lee of the terrain feature. This may produce violent and, for smaller aircraft, potentially uncontrollable effects resulting in pitch and / or roll to extreme positions.
Relative air movements which involve rapid rates of change in wind velocity are described as wind shear and, when severe, they may be sufficient to displace an aircraft abruptly from its intended flight path such that substantial control input is required to compensate. The consequences of such encounters can be particularly dangerous at low altitude where any loss of control may occur sufficiently close to terrain to make recovery difficult. The extreme down-bursts which occur below the base of cumulonimbus clouds called Microbursts are a classic example of circumstances conducive to Low Level Wind Shear
Severity of Turbulence
For the purpose of reporting and forecasting of air turbulence, it is graded on a relative scale, according to its perceived or potential effect on a 'typical' aircraft, as Light, Moderate, Severe and Extreme.
- Light turbulence is the least severe, with slight, erratic changes in attitude and/or altitude.
- Moderate turbulence is similar to light turbulence, but of greater intensity - variations in speed as well as altitude and attitude may occur but the aircraft remains in control all the time.
- Severe turbulence is characterised by large, abrupt changes in attitude and altitude with large variations in airspeed. There may be brief periods where effective control of the aircraft is impossible. Loose objects may move around the cabin and damage to aircraft structures may occur.
- Extreme turbulence is capable of causing structural damage and resulting directly in prolonged, possibly terminal, loss of control of the aircraft.
In-flight turbulence assessment is essentially subjective. Routine encounters involve light or moderate turbulence, although to inexperienced passengers (or pilots), especially in small aircraft, these conditions may seem to be severe.
The perception of turbulence severity experienced by an aircraft depends not only on the strength of the air disturbance but also on the size of the aircraft - moderate turbulence in a large aircraft may appear severe in a small aircraft. Therefore pilot reports of turbulence should mention the aircraft type to aid assessment of the relevance to other pilots in, or approaching, the same area.
Related Articles
Further Reading
- Bureau d’Enquêtes et d’Analyses (BEA) Incidents in Air Transport No 5 - Wind Gradients and Turbulence
- Preventing Turbulence-Related Injuries in Air Carrier Operations Conducted Under Title 14 Code of Federal Regulations Part 121, NTSB (USA), August 2021
- JTSB Digests: Digest of Aircraft Accident Analyses For Prevention of Accidents due to the Shaking of the Aircraft, JTSB (Japan), January 2015
- Review of Aviation Accidents involving Weather Turbulence in the United States 1992-2001, FAA, August 2004
Categories
What Links Here (105)
- Situational Awareness
- Level Bust
- Wake Vortex Turbulence
- Weather
- Coffin Corner
- Cumulonimbus (Cb)
- Hot Weather Operations
- Normal Operating Speed (maximum) (Vno)
- North Atlantic Operations - Contingency
- Pilot Report (PIREP)
- Pre-flight Preparation
- B735, en-route, SE of Kushimoto Wakayama Japan, 2006
- B741, en-route, Pacific Ocean, 1997
- MD11, Hong Kong China, 1999
- A333, en-route, Kota Kinabalu Malaysia, 2009
- B733, en-route, north of Antalya Turkey, 2009
- AT75, vicinity Cork Ireland, 2014
- A333, Manila Philippines, 2013
- A388, en-route, southeast of Mumbai India, 2014
- E145, en-route, near London ON Canada, 2014
- E170, en-route, Ishioka Japan, 2014
- B773, en-route, east northeast of Anchorage AK USA, 2015
- SF34, en-route, north of Edinburgh UK, 2017
- L410, Isle of Man, 2017
- A332, en-route, mid Atlantic, 2013
- A320, en-route, east of Miyazaki Japan, 2018
- B788, vicinity Amritsar India, 2018
- A346, en-route, northern Turkey, 2019
- A320, en-route, North East Spain 2006
- B773, en-route, Bay of Bengal, 2011
- B773, en-route, South China Sea Vietnam 2011
- A332, en-route, near Dar es Salaam Tanzania, 2012
- Controlled Flight Into Terrain (CFIT)
- Night Visual Approaches
- Loss of Control
- Weather Radar
- High-Altitude Flight Operations
- Recovery from Wake Vortex Encounter
- Wake Vortex Propagation and Decay
- Navigation Aids for VFR Flights
- Flight in Mountainous Terrain
- Flying a Visual Approach
- Runway Availability
- Weather Go/No-Go VFR Flight Checklist
- En-route Wake Vortex Hazard
- Transporting Live Animals By Air
- Parallel Runway Operation
- Urgency Instructions and Clearances
- Airworthiness Function Flights - Guidance for Controllers
- Runway Overrun After Unstabilised Approach (OGHFA SE)
- Loss of Separation During Weather Avoidance
- AIRMET
- ATC Operations in Weather Avoidance Scenarios
- Clear Air Turbulence (CAT)
- Engine Separation After Takeoff (OGHFA SE)
- High Level Ice Crystal Icing: Effects on Engines
- In-flight Seat Belt Requirements
- Landing Distances
- Loss of Control and In-Flight Upset After Loss of Engine Power (OGHFA SE)
- Low Level Wind Shear
- Medical Emergencies - Guidance for Flight Crew
- Mountain Waves
- Operations in Crude Oil Smoke: Guidance for Flight Crews
- Organizational Threat Management (OGHFA BN)
- Pyrocumulus
- SIGMET
- Skill Fade
- Threat Management Training (OGHFA BN)
- VFR Loss of Positional Orientation: Guidance for Controllers
- Waterspout
- Weather Forecast
- Weather Observations at Aerodromes
- Weather Radar: Storm Avoidance
- Working Environment
- Inter Tropical Convergence Zone (ITCZ)
- Jet Stream
- Tropical Revolving Storm
- Tropopause
- Thunderstorm
- Cumulus
- Fire whirl
- Firestorm
- Wind
- Lightning
- Haze
- Tornado
- Polar Stratospheric Cloud (PSC)
- Accident and Serious Incident Reports: WX
- Monsoon
- SE078: Turbulence Procedures for Reducing Cabin Injuries
- Gustnado
- Lightning Detection Network
- Asperitas
- Cloud Classification: Genera and Species
- Kelvin-Helmholtz Waves
- Lenticular Cloud
- Nimbostratus
- Performance shear
- Stabilised Approach
- Autothrottle/Autothrust
- Senior Cabin Crew Member (SCCM)
- B788, en-route, Chengde China, 2019
- Richardson Number
- AT45, en-route, north northwest of Tanegashima Japan, 2019
- GAMET






