FREEZING CONTAMINATION : AIRCRAFT ICING

Similar documents
Meteorology. Review Extreme Weather a. cold front. b. warm front. What type of weather is associated with a:

FREEZING CONTAMINATION : AIRCRAFT ICING

Aircraft Icing Icing Physics

The Ice Crystal Weather Threat to Engines

FREEZING CONTAMINATION : AIRCRAFT ICING

GENERAL AVIATION SAFETY SENSE

Aircraft Icing FAR/CS-25, Appendix O and P charts

Airplane Icing. Accidents That Shaped Our Safety Regulations. Federal Aviation Administration

Chapter 7 Precipitation Processes

Guidance to Instructors on Subject Delivery PILOT NAVIGATION. This is a suggested programme for the delivery of this subject.

Subject No 8 - PPL Meteorology

ANALYSIS OF CAUSES OF ICING CONDITIONS WHICH CONTRIBUTED TO THE CRASH OF CONTINENTAL FLIGHT 3407

1. describe the two methods by which cloud droplets can grow to produce precipitation (pp );

Thermal modelling of the Wing Anti Ice System in modern aircrafts

Collision and Coalescence 3/3/2010. ATS 351 Lab 7 Precipitation. Droplet Growth by Collision and Coalescence. March 7, 2006

Effect of Mixed Icing Conditions on Thermal Ice Protection Systems

U.S. DEPARTMENT OF TRANSPORTATION FEDERAL AVIATION ADMINISTRATION. National Policy

AIRCRAFT ICING Capt. M.P. Pappy Papadakis JD 1992 OUT DATED MATERIAL

COLD WEATHER PROTECTION GENERAL

Preventing Runway Excursions. Landing on wet / Contaminated Runways

Preventing Runway Excursions. Landing on wet / Contaminated Runways

A Description of Convective Weather Containing Ice Crystals Associated with Engine Powerloss and Damage

Why Should You Consider a Freezing Point Depressant Ice Protection System? Icing Certification Present and Future. CAV Aerospace Limited

METEOROLOGY PANEL (METP) WORKING GROUP- METEOROLOGICAL OPERATION GROUP (MOG) FIRST MEETING

SAMPLE ASSESSMENT TASKS AVIATION ATAR YEAR 12

Federal Aviation Administration

STUDY UNIT SEVENTEEN GRAPHICAL AIRMAN S METEOROLOGICAL ADVISORY (G-AIRMET)

Deputy Director for Science NCAR Aviation Applications Program

ADL110B ADL120 ADL130 ADL140 How to use radar and strike images. Version

ROYAL CANADIAN AIR CADETS PROFICIENCY LEVEL THREE INSTRUCTIONAL GUIDE SECTION 4 EO M EXPLAIN THE EFFECTS OF HUMIDITY AND TEMPERATURE ON WEATHER

Water in the Atmosphere

Thursday, June 5, Chapter 5: Condensation & Precipitation

Analysis of Causes of Icing Conditions Which Contributed to the Crash of Continental Flight 3407

Traffic and Weather. Soaring Safety Foundation. Tom Johnson CFIG

ELEMENTARY SCIENCE PROGRAM MATH, SCIENCE & TECHNOLOGY EDUCATION. A Collection of Learning Experiences WEATHER Weather Student Activity Book

Chapter 5: Weather. Only Section 1: What is Weather?

Most types of clouds are found in the troposphere, and almost all weather occurs within this

WAFS_Word. 2. Menu. 2.1 Untitled Slide

Planed treatment recommendations

RESEARCH ON AIRWORTHINESS REQUIREMENTS OF SUPERCOOLED LARGE DROP ICING PROTECTION FOR AIRCRAFT ( )

24.2 Cloud Formation 2/3/2014. Orographic Lifting. Processes That Lift Air Frontal Wedging. Convergence and Localized Convective Lifting

In-Flight Mixed Phase Ice Accretion Prediction on Finite Wings with TAICE-3D

ISSUED BY KENDRIYA VIDYALAYA - DOWNLOADED FROM

WO2 ROZSA-HRABINSKI METEOROLOGY 1

Syllabus details and associated Learning Objectives (A) and EIR METEOROLOGY

Helicopter-triggered lightning strike forecasting

Network Severe Weather Programme

Advances in weather and climate science

The Ice Crystal Icing Hazard & Risk Mitigation: Delta Air Lines Perspective

Weather - is the state of the atmosphere at a specific time & place

Cloud Formation and Classification

Weather & Atmospheric Variables Review

Chapter 5 - Atmospheric Moisture

Answer Key. Page 1 of 5

Chapter 7: Precipitation Processes. ESS5 Prof. Jin-Yi Yu

INITIAL VERIFICATION OF A 3D MORPHOGENETIC MODEL OF IN-FLIGHT ICING ON A CYLINDER

Wind Resource Assessment in Icing Environments

EARTH SCIENCE. Prentice Hall Water in the Atmosphere Water in the Atmosphere Water in the Atmosphere.

Pd: Date: Page # Describing Weather -- Lesson 1 Study Guide

MINISTRY OF DEFENCE MILITARY AIRCRAFT ACCIDENT SUMMARY

Return periods of prolonged fog events in Canada

FLIGHT IN ICING CONDITIONS

Lecture 07 February 10, 2010 Water in the Atmosphere: Part 1

FLIGHT INSTRUMENTS. This manual is dedicated only for IVAO Network activities. This document must not be used in real aviation or in others networks.

Weather, Atmosphere and Meteorology

Pilot briefing ENTC - Tromsø airport, Langnes

Aerodynamics and Flight Mechanics

Learning. Goals. Page 1 of 6. Document : V1.1

9/22/14. Chapter 5: Forms of Condensation and Precipitation. The Atmosphere: An Introduction to Meteorology, 12 th.

78% : component of atmosphere! 21% : 1% : Changes depending on origin of air: - originated over - originated over Ozone = O 3 Definition:

In-flight Ice Accretion Prediction Code

Unit 4 Lesson 2 Clouds and Cloud Formation. Copyright Houghton Mifflin Harcourt Publishing Company

Introduction. Aerospace Industries Assoiation AIA/EIWG Subcommittee on Engine Ground Operations During Heavy Snow. August 2014

Precipitation. AT350: Ahrens Chapter 8

INSTRUMENTATION OF AN ICING WIND TUNNEL BASED ON SAE STANDARDS

Aero-Propulsive-Elastic Modeling Using OpenVSP

surrounds Earth and protects it somewhat from solar radiation. Like all other matter, air has weight,

Chapter 8 - Precipitation. Rain Drops, Cloud Droplets, and CCN

Flight Dispatcher Aviation Meteorology Required Knowledge

Weather Technology in the Cockpit (WTIC) Shortfall Analysis of Weather Information in Remote Airspace Friends and Partners of Aviation Weather Summer

Subject No 20 - CPL Meteorology

Aircraft Icing. FAR 25, Appendix C charts. Prof. Dr. Serkan ÖZGEN. Dept. Aerospace Engineering, METU Fall 2015

Precipitations. Terminal Velocity. Chapter 7: Precipitation Processes. Growth of Cloud Droplet Forms of Precipitations Cloud Seeding

RISK FACTORS FOR FATAL GENERAL AVIATION ACCIDENTS IN DEGRADED VISUAL CONDITIONS

1. Base your answer to the following question on the weather map below, which shows a weather system that is affecting part of the United States.

Sensors and Programs for Inflight Icing. Dr. Darrel Baumgardner Droplet Measurement Technologies Boulder, CO

Aviation Hazards: Thunderstorms and Deep Convection

By A. W. BREWER, M.Sc.

Accident Prevention Program

Forecasting and modelling ice layer formation on the snowpack due to freezing precipitation in the Pyrenees

So what makes clouds cover a perfectly fine beautiful airplane with ice?

Explain in plain language the coded or pictorial information contained in:

Proficiency Level Three Combined Aviation Assessment Study Guide

Weather. Describing Weather

according to and water. High atmospheric pressure - Cold dry air is other air so it remains close to the earth, giving weather.

JAA Administrative & Guidance Material Section Five: Licensing, Part Two: Procedures

Moisture, Clouds, and Precipitation Earth Science, 13e Chapter 17

Verification and performance measures of Meteorological Services to Air Traffic Management (MSTA)

COLLINS WXR-2100 MULTISCAN RADAR FULLY AUTOMATIC WEATHER RADAR. Presented by: Rockwell Collins Cedar Rapids, Iowa 52498

What do you think of when someone says weather?

Transcription:

FREEZING CONTAMINATION : AIRCRAFT ICING EFFECTS ON AIRCRAFT Different types of accretion Intensity of ice accretion Consequences of accretion Vulnerability factors examples Specific vulnerabilities Detection in flight Removal of accretion : De-icing Prevention of icing : Anti-icing Certification and icing conditions Marginal weather conditions 1

Source NASA-Lewis Research Center 2

Different types of accretion (1) hoar frost source Transport Canada Aspect : Crystalline in the form of scales, needles or feathers. Formation conditions : Sublimation of water vapour into ice. This deposit can occur without clouds. Effects : Even if the amount of deposited material is low, it can be significant under certain conditions. 3

Different types of accretion (2) rime ice Source Météo France Aspect : Opaque and white, but rather fragile and brittle. Formation conditions : On a cold surface in a homogeneous cloud environment (T<<0 C). The supercooled cloud droplets rapidly freeze resulting in entrapped bubbles of air. Effects : Forms on leading edges. Rime ice is always significant and needs to be removed. 4

Different types of accretion (3) clear ice Source NASA-Lewis Research Centre Aspect : Transparent, homogeneous and smooth, very compact. Its specific mass is close to the one of pure ice. Formation conditions : On a cold surface in a homogeneous cloud environment with a temperature close to 0 C. The supercooled cloud droplets are present in large quantities and spread out before they slowly freeze. Effects : Develops in cones on the leading edges and is very significant. Should be prevented from forming. 5

Different types of accretion (4) mixed ice Image source: NASA-Lewis Research Centre Aspect : Mix of clear ice, hoar frost and rime ice. Whitish and brittle. Formation conditions : On a cold surface in a heterogeneous cloud environment where the temperature and cloud drops sizes fluctuate (*). Effects : Similar to rime ice. 6

Intensity of ice accretion (1) light : > 1g/cm²/hour moderate : > 6g/cm²/hour severe : > 12g/cm²/hour 7

Intensity of ice accretion (2) Light Icing : does not pose any specific restraints on the behaviour of the aircraft Moderate icing : icing conditions may cause the crew to change heading or altitude Severe icing : icing conditions which force the crew to immediately change heading or altitude 8

Consequences of accretion (1) The accumulation of ice represents an increase in mass and leads to the modification of the longitudinal equilibrium of the aircraft. The effect is relatively small on larger aircraft. Icing on tubes and antennas disturbs their operation and can lead to the rupture of elements. Icing on the windshield reduces the visibility. Means of propulsion (motors, propellers, fans, rotors) are also vulnerable to ice accretion. Their efficiency is reduced and they can stop functioning altogether. 9

Consequences of accretion (2) The aerodynamic consequences: a major impact. clean with contamination Lift force (*) reduces considerably (20% - 30%) when modern wings get contaminated. Moreover, forms of light icing have a similar effect to forms of severe icing. source NASA 10

A vulnerability factor: the aerodynamic profile (1) The aerodynamic flux (flow of air along the surfaces of an aircraft) is modified by the shape of its profile. Also the collection efficiency, for a fixed size of cloud droplets, of a wing profile depends upon its form and thickness. Aerodynamic flux PROFILE Drop trajectory Collection zone In the same icing conditions, the resulting accretion and the effect on aerodynamics vary largely from one type of aircraft to another. 11

t in C Another vulnerability factor : Aerodynamic speed (2) 27 8 1 Aerodynamic speed in knots Difference in air temperature and temperature of the point of impact ( t) in the lower layers of the atmosphere. Fast aircraft are less vulnerable to ice accretion. 12

Specific vulnerability of the turbo reactor : ingestion of ice during flight A turbo reactor in operation can shut down or be destroyed by ingestion of a mass of ice. Images source: Pratt and Whitney Two possible scenarios: Accumulation on the landing gear while taxiing-out in an area contaminated with frozen snow. The ice lumps will become projectiles on the initial acceleration of the aircraft. Late use of de-icing or anti-icing equipment flight during severe icing conditions. The ice that breaks off can fly straight into the engine. 13

Specific vulnerability for light aviation: Formation of ice in a carburettor The carburettors in light aircraft are prone to formation of ice. This icing occurs in the part of the carburettor where the pressure decreases (temperature drops) and where the fuel vaporises (temperature decreases even further). When the icing is important enough, the engine stalls. This is a diagram which source Royal Australian Air Force allows us to determine the risk for carburettor icing in function of the temperature and dew point (*). The risk is at a maximum in saturated air with temperatures between +5 and +15 C. 14

Specific vulnerability for light aviation: flight in clouds under Instrument Flight Rules (IFR). Light aircraft flying IFR and which are not equipped with effective de-icing equipment are particularly vulnerable in icing conditions. It is therefore very useful for the pilot to know the lowest flight level (altitude or pressure) where the temperature is below 0 C. (*) If this sheet of stratocumulus has a temperature below freezing, it would not be a good idea to level out at this level! Frank Jansen photography 15

Detection in flight Visual indications for ice accretion (*) Source ATR Electronic ice detector (**) Source ATR 16

Removal of accretion: de-icing De-icing is the process whereby a system removes ice after it has formed on the aircraft. If the type of icing is not too solid and the intensity of the phenomena is moderate, the pilot can remove the icing by mechanical means. The advantage of these systems is that they use little energy. This is why they are mounted on light aircraft and turboprops. Black surface can be deformed by pneumatic systems Source ATR The downside is that these systems can be ineffective in exceptional icing conditions. 17

Prevention of icing: anti-icing Anti-icing is a system which prevents icing to form. The most widely used technique is to heat the elements or surfaces prone to icing. Advantage: the aircraft will be well protected in almost all icing conditions if they are anticipated. Source I.A.E Disadvantage: these systems are high energy consumers. Their use will imply cost penalties. 18

Certification in icing conditions measured liquid water content Aeronautical authorities impose exploitation rules during icing conditions. More particularly, certain standards haven been defined to certify an aircraft, for example the properties of a de-icing system will be defined. accretion severe 12 g/cm²/hour moderate 6 g/cm²/hour light 1 g/cm²/hour icing potential These standards have been defined on a basis of special studies conducted in the real atmosphere (here CASP II in Canada in 1992). Very extreme situations (red circle), which are rarely encountered are not taken into account. median volume diameter The conditions which cause the extreme observations have to be specified. 19

Marginal weather conditions Experience shows that atmospheric conditions bordering icing conditions have not been evaluated enough. Actually, these situations correspond to an intense phenomena that is easy to observe or detect and which warrants an immediate and effective reaction from the aeronautical actor. When the atmospheric parameters oscillate around icing conditions or when the conditions are out of the regional or seasonal mean, traps ( real atmospheric ambushes) will develop. Early detection can easily be done by an aeronautical meteorologist. 20

Conclusion of the first part : a list with meteorological objectives on icing. 1) Deliver accurate forecasts within aeronautical range ( 24 hours), adapted to the local and seasonal context. Determine the first freezing level and obtain good scores in forecasting the presence or absence of potential icing conditions on a certain level. These points are operationally important. 2) Arrive to a good detection of extreme conditions corresponding to case of observed severe icing. This is an important point for certain categories of public transport aircraft. (commuters) 3) Underline the marginal situations (ambushes) which are bordering on the limit of unpredictable, in order to create a permanent state of vigilance amongst the aeronautical operators. This point is important for air safety in general. 4) Deepen theoretical knowledge about the subject in extreme case through experiments. This in order to refine the current standards. 5) Develop training for the aeronautical actors on the subject: To allow him to correctly interpret the information To familiarize him with the methods and classic scenarios we use. To create awareness about the need of feedback. 21

Forward to: prognostic variables in the atmosphere Notes for teachers 22