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    TET1 aircraft icing- 12/2005- V1 1+WMO

    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

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    TET1 aircraft icing- 12/2005- V1 2+WMO

    Source NASA-Lewis Research Center

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    Different types of accretion (1)

    Aspect : Crystalline in the form of scales, needles or feathers.

    Formation conditions : Sublimation of water vapour into ice. This deposit canoccur without clouds.

    Effects : Even if the amount of deposited material is low, it can be significant

    under certain conditions.

    hoar frost

    source Transport Canada

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    Different types of accretion (2)

    Aspect : Opaque and white, but rather fragile and brittle.

    Formation conditions : On a cold surface in a homogeneous cloud environment

    (T

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    Different types of accretion (3)

    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 environmentwith a temperature close to 0C. 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.

    clear ice

    Source NASA-Lewis Research Centre

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    TET1 aircraft icing- 12/2005- V1 6+WMO

    Different types of accretion (4)

    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.

    mixed ice

    Image source: NASA-Lewis Research Centre

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    TET1 aircraft icing- 12/2005- V1 7+WMO

    Intensity of ice accretion (1)

    light :

    > 1g/cm/hour

    moderate :

    > 6g/cm/hour

    severe :

    > 12g/cm/hour

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    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 changeheading or altitude

    Severe icing : icing conditions which force the crew to immediately

    change heading or altitude

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    TET1 aircraft icing- 12/2005- V1 9+WMO

    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 ruptureof 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.

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    Consequences of accretion (2)

    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.

    clean

    with contamination

    The aerodynamic consequences:

    a major impact.

    source NASA

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    PROFILE

    A vulnerability factor: the aerodynamic profile (1)

    In the same icing conditions, the resulting accretion and the effect on

    aerodynamics vary largely from one type of aircraft to another.

    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.

    Drop trajectory

    Aerodynamic flux

    Collection zone

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    TET1 aircraft icing- 12/2005- V1 12+WMO

    Aerodynamic speed in knots

    tin

    C

    Another vulnerability factor : Aerodynamic speed (2)

    1

    8

    27

    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.

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    TET1 aircraft icing- 12/2005- V1 13+WMO

    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.

    Two possible scenarios:

    Accumulation on the landing gear while taxiing-out in an area contaminatedwith 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.

    Images source: Pratt and Whitney

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    TET1 aircraft icing- 12/2005- V1 14+WMO

    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.

    The risk is at a

    maximum in saturatedair with temperatures

    between +5 and +15C.

    This is a diagram which

    allows us to determine

    the risk for carburettor

    icing in function of the

    temperature and dewpoint (*).

    source Royal Australian Air Force

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    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 0C. (*)

    If this sheet of stratocumulus

    has a temperature belowfreezing, it would not be a

    good idea to level out at this

    level!Frank Jansen photography

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    TET1 aircraft icing- 12/2005- V1 16+WMO

    Detection in flight

    Visual indications for ice accretion (*)

    Source ATR

    Electronic ice detector (**)

    Source ATR

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    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.

    The downside is that these systems can be ineffective in exceptional icing

    conditions.

    Black surface can bedeformed by pneumatic

    systems

    Source ATR

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    TET1 aircraft icing- 12/2005- V1 18+WMO

    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.

    Disadvantage: these systems are high energy consumers. Their use will imply

    cost penalties.

    Source I.A.E

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    TET1 aircraft icing- 12/2005- V1 19+WMO

    Certification in icing conditions

    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.

    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 (redcircle), which are rarely

    encountered are not taken into

    account.

    measuredliquidwatercontent

    median volume diameter

    accretion

    severe12 g/cm/hour

    moderate6 g/cm/hour

    light1 g/cm/hour

    icing potential

    The conditions which cause the

    extreme observations have to

    be specified.

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    TET1 aircraft icing- 12/2005- V1 20+WMO

    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.

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    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 limitof 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.

    Conclusion of the first part : a list with meteorological objectives on icing.

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    Forward to: prognostic variables in the atmosphere

    Notes for teachers

    http://www.caem.wmo.int/_pdf/icing/icing_03_prognostic_variables.pdfhttp://www.caem.wmo.int/_pdf/icing/icing_02_teacher_notes.pdfhttp://www.caem.wmo.int/_pdf/icing/icing_02_teacher_notes.pdfhttp://www.caem.wmo.int/_pdf/icing/icing_03_prognostic_variables.pdf