Weather Ch.4 Flashcards
LIST the classifications of turbulence used in Pilot Reports (PIREPs)
- Mechanical
- Thermal
- Wind Shear
- Frontal
LIST the intensities of turbulence used in Pilot Reports (PIREPs)
- Light
- Moderate
- Severe
- Extreme

DEFINE the terms used to report turbulence with respect to time
- Occasional: Less than 1/3 of the time
- Intermittent: 1/3 to 2/3 of the time
- Continuous: More than 2/3 of the time
DESCRIBE how thermal turbulence develops
- Also called Convective turbulence
- Result of heating from below
- Solar heating
- Cold Air moving over warmer surface
- Strength depends on type of surface
DESCRIBE how mechanical turbulence develops
- casued by passage of wind over obstructions
- Buildings
- Irregular terrain/mountains
- Strength and magnitude dependent on
- wind speed
- roughness of terrain
- stability of the air
DESCRIBE the cloud formations associated with mountain wave turbulence
- Rotor Clouds
- Form downwind from and parallel to mountain range
- Cylindrical shape
- downward flow has been known to reach the gorund
- Cap Clouds
- Cover top of mountatin
- Remain stationary
- Lenticular Clouds
- Form on leeward side of mountain from standing waves
DESCRIBE techniques for flight in the vicinity of mountain waves
- Approach mountain at 45 degree angle, so it is easy to turn back
- Circumnavigate if possible
- fly 50% higher than peak
- Avoid rotor, cap, and lenticualr clouds
- Avoid strong downdrafts on leeward side of mountain
- Pressure changes affect pitot-static instruments
- Fly reccomended turbulent air penetration speed
DESCRIBE how frontal lifting creates turbulence
- Turbulence is caused by warm air being lifted by the cold front
- abrupt wind shift between air masses
- strong vertical currents when warm air is moist and unstable
- most severe in fast-moving front
- no turbulence in warm front due to little or no lifting
DESCRIBE how temperature inversions are examples of wind shear turbulence
- Extreme wind shear may be formed when strong inversion exists near the ground
- conditions near ground are stable
- Strong wind has to exist in upper warmer air
- wind shear is then produced at layer boundry
- Sudden change in wind direction/velocity causes loss of airpseed and lift
DESCRIBE how jet streams are examples of wind shear turbulence
- The change in wind speed in short distance can create a significant amount of wind shear
- vertical shear is more significant than horizontal shear
- exit by turning south or changing alttitude
- jet stream could have winds that reach 250 knots
DESCRIBE the recommended procedures for flying through turbulence
- Maintain PCL setting consistent with desired turnbulent air penetration speed
- trim aircraft for level flight
- do not chase airspeed deviations with power corrections
- severe turbulence causes large rapid variations
- Allow altitude to vary, do not chase altimeter
- Vertical gusts cause significant altitude deviations
- Maintain pitch and bank by reference to attitude indicator
DESCRIBE structural icing, in a classroom
- forms on external surfaces of the aircraft
- 4 types of icing:
- Clear
- Rime
- Mixed
- Frost
STATE the requirements for the formation of structural icing
- there must be visible moisture that super-cooled (liquid water that is below freezing); mainly in clouds
- The free air temp and aircraft’s surface temp are below freezing
STATE the temperature range most conducive to structural icing
- -20 C to 0 C
DESCRIBE icing conditions associated with fronts
- Warm fronts
- stratiform clouds
- rime icing
- low rate of accumulation
- widespread area of icing
- Cold Fronts
- cumuliform clouds
- clear icing
- high rate of accumulation
- limited area of icing
- Occluded Fronts
- Mixed clouds
- Stratus and cumulus
- mixed icing
- rime, clear, and mixed
- rapid and heavy accumulation
- very widespread area of icing
IDENTIFY the hazards of aircraft icing
- Most hazardous: Alters the shape of airfoil changing the stall angle of attack
- Decreases lift, thrust, and range
- Increases drag, weight, fuel consumption, and stall speed
- faulty indications from pitot-static system
- inhibits control surface movement and antenna transmission
DESCRIBE the types of engine icing, in a classroom
- Induction Icing
- AKA inlet icing
- happens in clear skies and above freezing temps
- taxi and departure
- reduced pressure in intake system lowers temp, causing condensation and ice formation
- High probability with air temps 10 C or less and high relative humidity
- Compressor Icing
- forms on compressor inlet blades
- restricts airflow to engine could casue FOD
- causing a flame-out, loss of thrust, rise of Exhaust gas temp, fuel to air ratio to increase
DESCRIBE ground icing hazards
- Frost
- usually found first thing in the morning
- must remove prior to flight
- deicing fluid if highly corrosive and should not be sprayed down intakes or other openings
- Taxiing through mud, slush, or water
- splashed on aircraft surfaces
- can freeze later at higher altitudes and colder temps
- Runway breaking conditions
- hazardous to control during braking of aircraft
IDENTIFY the procedures to minimize or avoid the effects of icing
- Avoid known icing conditions
- visible moisture (clouds)
- 0 to -20 C
- low altitudes or mountainous terrain
- When encountered
- Climb or descend
- Climb: out of visible moisture, to colder temps (frozen moisture not a hazrd), to watmer temps (if below warm front or temp inversion )
- Descend: out of visible moisture, below freezing level, if visible moisture or freezing level on surface you can’t descend
- Climb or descend
- Anti-Ice or De-Ice
- Anti prevents icing
- De removes existing ice
- Do not fly perpindicular to a front in icing conditions
- Maximizes exposure time
- Minimze bank angle and high AOA
- Increased stall speed
- Use common sense
- Remove ice or frost prior to takeoff
LIST the intensities of icing used in Pilot Reports (PIREPs)
- Trace
- ice perceptible but not hazardous
- Light
- accumulaton maybe a problem if over an hour, ocassional us of anti or de-icing, not a problem if equioment is used
- Moderate
- rate of accumulation potentially hazardous, even for short encounters, de-ice/anti-ice equipment or diversion necessary
- Severe
- Rate of accumulation extreme, de-ice/anti-ice equipment fails to reduce or control, immediate diversion necessary, emergency
LIST the types of icing used in Pilot Reports (PIREPs)
- Rime Ice: Rough, milky opaque ice formed by the instantaneous freezing of small super-cooled water droplets
- Clear Ice: glossy, clear or translucent ice formed by the relatively slow freezing of large super-cooled water droplets
- Mixed Ice: A combination of rime and clear ice
DEFINE the types of visibility
- Flight Visibility
- average forward horizontal distance, measured in statute miles from the cockpit of an aircraft in flight
- pilot can see and identify prominent unlighted objects by day and prominent lighted objects at night
- in statute miles
- Prevailing Visibility
- used on METARS
- greatest horizontal visibility
- equaled or exceeded throughout over half horizon circle AKA must be at least 180°
- Slant Range Visibility
- distance on final approach at which runway environment in sight
- May be reported via PIREP
- can be estimated by meteoroligists
- Runway Visual Range (RVR)
- horizontal distance seen by looking down runway from approach end
- reported in meters or hundreds of feet
- horizontal distance seen by looking down runway from approach end
DEFINE obscuring phenomena
- any collection of particles that reduce horizontal visibility to less than six miles
- surface based or aloft
- Ex. fog, haze, smoke, volcanic ash, and blowing spray
- vis can vary greatly in same location with different points of view
DESCRIBE the sky coverage terms that define a ceiling
- A ceiling is the height above the ground (AGL) ascribed to the lowest broken or overcast layer; or the vertical visibility into an obscuring phenomenon (total obscuration)
- Vertical visibility is the distance that can be seen directly upward from the ground into a surface based obscuring phenomenon
- Broken= sky cover is 5/8 to 7/8
- Overcast= sky cover is 8/8
DESCRIBE the parameters that define fog
- visible layer of condensed moisture (must meet all 3)
- Base at or within 50 ft of surface
- greater than 20 ft thick
- reduces visibility to less than 5/8 of a mile
- 2 types
- Advection
- Raditation
STATE the requirements for fog formation
- condensation nuclei
- high moisture content
- small temp/dew point spread
- near equal (saturation)
- light surface winds
- 1-10 knots
DESCRIBE the two main types of fog
- Advection
- warm, moist air moves over cool surface
- at or near saturation
- cool surface reduces temp/dew point spread
- Usually forms over water
- brough inland by winds
- winds can be stronger
- Very thick
- doesn’t dissipate with sunshine
- only wind shift can dissipate
- persistent
- warm, moist air moves over cool surface
- Radiation
- caused by nocturnal radiation cooling
- what you see in the morning
- Rate depends on:
- surface composition
- vegetation
- cloud coverage
- ceiling
- Light winds
- dissiption begins as sun warms surface
DESCRIBE the aviation hazards of ash clouds
- Volcanic ash clouds create an extreme hazard to aircraft operating near (especially downwind) of active volcanoes. Aircraft flying through volcanic ash clouds have experienced a significant loss of engine thrust and/or multiple engine flameouts along with wing leading edges and windshields being sandblasted.
- multiple engine malfunctions
- flameout
- all engines affected on mulit-engine aircraft
- pitted windscreens
- affects cockpit vis
- sandblasting of external surfaces
- Make 180° turn to escape, fly 20 NM upwind of eruption