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Ch 13 - Icing

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Ch 13 - Icing Ch 13 - Icing Introduction Aircraft icing can have serious negative effects on both the powerplant and the aerodynamic performance of your aircraft As a ... – PowerPoint PPT presentation

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Title: Ch 13 - Icing


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Ch 13 - Icing
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Ch 13 - Icing
  • Introduction
  • Aircraft icing can have serious negative effects
    on both the powerplant and the aerodynamic
    performance of your aircraft
  • As a pilot, your life and the lives of your
    passengers depend on your ability to understand
    icing and to take the proper preflight and
    inflight steps to deal with it safely

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  • In this chapter, you will learn to identify and
    report the various types of icing, understand its
    causes, and become familiar with the
    meteorological conditions under which it is most
    likely to occur
  • When you complete this chapter, you should have a
    basic understanding of the icing threat and the
    knowledge of how to avoid it or at least minimize
    the problem

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  • Section A Aircraft Icing Hazards
  • Induction Icing
  • Structural Icing
  • Ground Icing
  • Section B Observing and Reporting Structural
    Icing
  • Observations of Icing Type and Severity
  • Icing PIREPs

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  • Section C Microscale Icing Processes
  • Temperature
  • Liquid Water Content
  • Droplet Size
  • Section D Icing and Macroscale Weather Patterns
  • Cyclones
  • Influence of Mountains
  • Icing Climatology
  • Section E Minimizing Icing Encounters

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  • Section A Aircraft Icing Hazards
  • Icing refers to any deposit or coating of ice
    on an aircraft.
  • Two types of icing are critical in the operation
    of aircraft induction icing and structural
    icing.

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  • Induction Icing
  • Induction icing a general term which applies to
    all icing that affects the power plant operation.
  • The main effect of induction icing is power loss
    due to ice blocking the air before it enters the
    engine, thereby interfering with the fuel/air
    mixture.
  • Induction icing includes carburetor icing and
    icing on air intakes such as screens and air
    scoops.
  • Carburetor icing occurs when moist air drawn
    into the carburetor is cooled to a temperature
    less than 0 degrees Celsius by adiabatic
    expansion and fuel vaporization.

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  • Structural icing
  • Structural icing Airframe or structural icing
    refers to the accumulation of ice on the exterior
    of the aircraft during flight through clouds or
    liquid precipitation when the skin temperature of
    the aircraft is equal to, or less than 0 degrees
    Celsius.
  • The primary concern over even the slightest
    amount of structural icing is the loss of
    aerodynamic efficiency via an increase in drag
    and a decrease in lift.

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  • Ground icing Another important form of
    structural icing to be considered is that which
    may occur prior to take off.
  • An aircraft that is ice-free is as critical for
    takeoff as it is in other phases of flight, if
    not more so.
  • Causes of ground icing include freezing rain,
    freezing drizzle and wet snow.
  • Also, frost can be a significant hazard.

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  • Test data indicate that ice, snow, or frost
    having a thickness and roughness similar to
    medium or coarse sandpaper on the leading edge
    and upper surface of a wing can reduce lift by as
    much as 30 percent and increase drag by 40 percent

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  • A hard frost can increase the stalling speed
    by as much as 5 or 10 percent.
  • An aircraft carrying a coating of frost is
    particularly vulnerable at low levels if it also
    experiences turbulence or wind shear, especially
    at slow speeds and in turns.
  • Frost may prevent an airplane from becoming
    airborne at normal takeoff speed

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  • Section B Observing and Reporting Structural
    Icing
  • Observations of Icing Type and Severity
  • Rime ice Structural icing occurs when super
    cooled cloud or precipitation droplets freeze on
    contact with an aircraft.
  • The freezing process produces three different
    icing types clear, rime, and mixed ice.

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  • Rime ice is the most common icing type.
  • It forms when water droplets freeze on impact,
    trapping air bubbles in the ice.
  • This type of ice usually forms at temperatures
    below -15 degrees Celsius.
  • Rime ice appears opaque and milky white with a
    rough, porous texture.

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  • Although rime icing has serious effects on the
    aerodynamics of the aircraft wing, it is regarded
    as the least serious type of icing because it is
    lighter, easier to remove, and tends to form on
    the part of the aircraft where, if available,
    anti-icing and/or deicing equipment is located.

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  • Clear ice forms when droplets impacting an
    airplane freeze slowly, spreading over the
    aircraft components.
  • Air temperatures are usually between 0 degrees
    Celsius and 5 degrees Celsius.
  • These conditions create a smooth, glossy surface
    of streaks and bumps of hard ice.
  • Clear ice is less opaque than rime ice.
  • It may actually be clear but often is simply
    translucent (clear ice is also called glaze).

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  • Clear ice is the most dangerous form of
    structural icing because it is heavy and hard
  • it adheres strongly to the aircraft surface
  • it greatly disrupts the airflow over the wing and
    it can spread beyond the location of de-icing or
    anti-icing equipment.

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  • Runback icing when ice spreads beyond the ice
    protection equipment.
  • Mixed ice a combination of rime and clear ice
  • forms at intermediate temperatures (about -5
    degrees Celsius to -15 degrees Celsius) and has
    characteristics of both types.
  • The variation in liquid water content in this
    temperature range causes an aircraft that is
    flying in these conditions to collect layers of
    both less opaque (clear) and more opaque (rime)
    ice.

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  • Icing intensity The severity of icing is
    determined by its operational effect on the
    aircraft.
  • Icing intensity is classified as trace, light,
    moderate and severe and is related to
  • rate of accumulation of ice on the aircraft
  • the effectiveness of available de-icing/anti-icing
    equipment
  • and the actions you must take to combat the
    accumulation of ice.

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  • Icing PIREPs
  • Icing PIREPs Pilot reports of structural icing
    are often the only direct observations of that
    hazard and, as such, are of extreme importance to
    all pilots and aviation forecasters.
  • The critical information that an icing PIREP
    should contain includes location, time, flight
    level, aircraft type, temperature, icing
    intensity, and icing type.
  • Excellent aids to pilots in the diagnosis of
    icing conditions are graphical presentations of
    recent icing PIREPs from the Aviation Digital
    Data Service (ADDS).

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  • Section C Micro scale Icing Processes icing
    occurrence, type, and severity depend on three
    basic parameters
  • Temperature
  • Liquid water content
  • Droplet size

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  • Temperature icing types and critical outside
    air temperatures include
  • Clear (0 to -5 degrees Celsius
  • Clear or mixed (-5 to -10 degrees Celsius)
  • Mixed or rime (-10 to -15 degrees Celsius)
  • Rime (-15 to -20 degrees Celsius)

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  • Liquid Water Content (LWC) simply a measure of
    the liquid water due to all the super cooled
    droplets in that portion of the cloud where your
    aircraft happens to be

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  • Droplet Size
  • Super-cooled large droplets (SLD) associated
    with heavy icing and especially with runback
    icing problems
  • Collision/coalescence small water droplets can
    grow into large super cooled droplets
  • through this process, water droplets are super
    cooled and they initially formed in subfreezing
    surroundings

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  • Warm layer process - small water droplets can
    grow into large super cooled droplets
  • through this process, when snow falls into a warm
    layer (temperature greater than 0 degrees
    Celsius) where ice crystals melt, and then fall
    into a cold layer (temperature less than 0
    degrees Celsius) where the rain droplets become
    super cooled.

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  • The presence of ice pellets (PL) at the
    surface is evidence that there is freezing rain
    at a higher altitude

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  • Section D Icing and Macro scale Weather
    Patterns
  • Cyclones and Fronts extra tropical cyclones
    provide a variety of mechanisms to produce
    widespread, upward motions. These include
    convergence of surface winds, frontal lifting and
    convection.
  • Influence of Mountains mountainous terrain
    should always be considered a source of icing
    hazards when subfreezing clouds are present.
  • Icing Climatology refers to the average
    distribution of icing for a given area

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  • Section E Minimizing Icing Encounters know
    capabilities of your aircraft, decision tree
  • Freezing level analyzed on the freezing level
    chart and appears on some aviation forecast
    charts
  • Freezing level chart solid lines on this chart
    indicate the position of particular freezing
    levels.
  • The dashed lines indicate where the freezing
    level intersects the ground.
  • The open circles indicate the location of
    sounding stations where freezing levels are
    reported in hundreds of feet MSL.

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Ch 13 - Icing
  • Summary
  • Icing can affect an aircraft in many ways,
    including the degradation of aerodynamics, and
    causing difficulties with control surfaces,
    powerplant operation, propeller balance,
    operation of landing gear, communications,
    instrument accuracy, and ground handling

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  • Summary
  • An icing encounter does not leave much room for
    error
  • This is especially true when it is combined with
    the additional complications of turbulence, wind
    shear, and IMC
  • In this chapter, you have learned how induction
    and structural icing can form

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  • Summary
  • You are now aware of the types and severity
    classifications of structural icing, and how
    temperature, liquid water content, and droplet
    size contribute to icing type and severity
  • You now understand that the production of
    supercooled large droplets, such as found in
    freezing precipitation, is of particular
    importance for severe icing

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  • Summary
  • - In addition, your brief examination of an icing
    climatology has demonstrated how extratropical
    cyclones, airmasses, and fronts interact with
    moisture sources and mountains to make some
    geographical areas more conducive to icing events
    than others

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  • Summary
  • Finally, on the basis of icing causes and
    characteristics, a number of practical rules of
    thumb have been established to help you avoid or
    at least minimize icing effects
  • Keep in mind that these are general guidelines
    they have not directly addressed the capabilities
    of your aircraft to handle icing situations

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  • Summary
  • - More details with regard to tools and
    procedures for the general assessment of all
    weather conditions, including icing, in the
    preflight phase of flight will be presented in
    Part IV of this text
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