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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 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
Ch 13 - Icing
• 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
Ch 13 - Icing
• 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
Ch 13 - Icing
• 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
Ch 13 - Icing
• 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.
Ch 13 - Icing
• 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.
Ch 13 - Icing
• 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.
Ch 13 - Icing
– 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.
Ch 13 - Icing
• ***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
Ch 13 - Icing
• ***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
Ch 13 - Icing
• 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.
Ch 13 - Icing
– 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.
Ch 13 - Icing
– 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.
Ch 13 - Icing
• 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”).
Ch 13 - Icing
– 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.
Ch 13 - Icing
• 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.
Ch 13 - Icing
• 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.
Ch 13 - Icing
• 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).
Ch 13 - Icing
• Section C: Micro scale Icing Processes – icing
occurrence, type, and severity depend on three basic
parameters:
– Temperature
– Liquid water content
– Droplet size
Ch 13 - Icing
– 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)
Ch 13 - Icing
– 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
Ch 13 - Icing
– 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
Ch 13 - Icing
• 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.
Ch 13 - Icing
• ***The presence of ice pellets (PL) at the

surface is evidence that there is freezing rain at
a higher altitude
Ch 13 - Icing
• 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
Ch 13 - Icing
• 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.
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
Ch 13 - Icing
• 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
Ch 13 - Icing
• 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
Ch 13 - Icing
• 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
Ch 13 - Icing
• 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
Ch 13 - Icing
• 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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Ch 13 (1)

  • 1.
  • 2. Ch 13 - Icing
  • 3. 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
  • 4. Ch 13 - Icing • 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
  • 5. Ch 13 - Icing • 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
  • 6. Ch 13 - Icing • 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
  • 7. Ch 13 - Icing • 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.
  • 8. Ch 13 - Icing • 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.
  • 9. Ch 13 - Icing • 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.
  • 10. Ch 13 - Icing – 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.
  • 11. Ch 13 - Icing • ***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
  • 12. Ch 13 - Icing • ***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
  • 13. Ch 13 - Icing • 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.
  • 14.
  • 15. Ch 13 - Icing – 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.
  • 16. Ch 13 - Icing – 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.
  • 17. Ch 13 - Icing • 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”).
  • 18.
  • 19. Ch 13 - Icing – 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.
  • 20. Ch 13 - Icing • 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.
  • 21.
  • 22. Ch 13 - Icing • 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.
  • 23.
  • 24. Ch 13 - Icing • 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).
  • 25. Ch 13 - Icing • Section C: Micro scale Icing Processes – icing occurrence, type, and severity depend on three basic parameters: – Temperature – Liquid water content – Droplet size
  • 26. Ch 13 - Icing – 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)
  • 27. Ch 13 - Icing – 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
  • 28. Ch 13 - Icing – 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
  • 29. Ch 13 - Icing • 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.
  • 30.
  • 31. Ch 13 - Icing • ***The presence of ice pellets (PL) at the surface is evidence that there is freezing rain at a higher altitude
  • 32. Ch 13 - Icing • 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
  • 33.
  • 34. Ch 13 - Icing • 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.
  • 35.
  • 36. 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
  • 37. Ch 13 - Icing • 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
  • 38. Ch 13 - Icing • 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
  • 39. Ch 13 - Icing • 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
  • 40. Ch 13 - Icing • 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
  • 41. Ch 13 - Icing • 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