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What are some common obstructions to visibility in the atmosphere?

FAA-H-8083-28
Weather Meteorology

Answer:

  1. Fog:
    • Forms when air temperature and dew point are nearly equal, reducing visibility to less than 5/8 SM.
  2. Mist:
    • Similar to fog but with higher visibility (5/8 to 6 SM) and smaller water droplets.
  3. Haze:
    • Caused by suspended dry particles such as dust, salt, or smoke, reducing visibility in stable air.
  4. Smoke:
    • Produced by fires or industrial activity and can reduce visibility significantly, especially in light winds.
  5. Precipitation:
    • Rain, snow, or drizzle can reduce visibility, especially heavy rain or snow showers.
  6. Blowing Snow:
    • Snow lifted by the wind, reducing visibility and creating whiteout conditions.
  7. Dust Storm:
    • Strong winds lift large amounts of dust, severely reducing visibility and creating hazardous flight conditions.
  8. Sandstorm:
    • Similar to a dust storm but with fine sand particles, mainly in desert regions.
  9. Volcanic Ash:
    • Extremely hazardous to aviation; can cause engine failure, obscure visibility, and damage aircraft surfaces.

 

Is frost hazardous to flight? Why or why not?

FAA-H-8083-28
Weather Meteorology

Answer:

Yes, frost is hazardous to flight because it affects aerodynamic performance by:

  • Disrupting smooth airflow over the wings, leading to early airflow separation.
  • Reducing lift and increasing stall speed.
  • Potentially preventing takeoff at normal speeds, even with a small amount of frost.
  • Decreasing stall margin in flight, making the aircraft more susceptible to stalling in turns or turbulence.

What is frost, and under what conditions does it form?

FAA-H-8083-25
Weather Meteorology

Answer:

  • Definition:
    • Frost consists of ice crystal deposits that form through sublimation when both temperature and dew point are below freezing.
  • Formation Conditions:
    • Occurs on clear nights when moisture is present in the air.
    • Radiational cooling causes the aircraft’s skin temperature to drop below freezing, allowing moisture to freeze directly onto the surface.

What are the different types of fog?

FAA-H-8083-28
Weather Meteorology

Answer:

  1. Radiation Fog:
    • Forms at night or near daybreak under clear skies, little or no wind, and high humidity.
    • Caused by ground cooling, which lowers air temperature to the dew point.
  2. Advection Fog:
    • Develops when moist air moves over colder ground or water.
    • Common in coastal areas but can form inland.
    • Can occur day or night and with wind present.
  3. Upslope Fog:
    • Forms when moist, stable air is lifted up a slope or terrain and cools adiabatically.
    • Dissipates when upslope winds stop.
  4. Frontal Fog (Precipitation-Induced Fog):
    • Forms when warm, moist air is lifted over a front, producing clouds and precipitation.
    • If cold air below is near the dew point, evaporation from precipitation can saturate the air and create fog.
  5. Steam Fog:
    • Occurs when very cold air moves over warmer water.
    • Moisture evaporates, rises, and immediately re-condenses, forming fog that rises like steam.
  6. Freezing Fog:
    • Forms when supercooled fog droplets freeze upon contact with surfaces.
    • Occurs when air temperature is at or below 0°C (32°F).
    • Can cause dangerous icing on aircraft and runways.

 

What causes fog to form?

FAA-H-8083-28
Weather Meteorology

Answer:

  • Fog Formation:
    • Occurs when air temperature and dew point become equal (or nearly so).
    • Can happen in two ways:
      1. Cooling the air below its dew point (radiation fog, advection fog, or upslope fog).
      2. Adding moisture to raise the dew point (frontal fog or steam fog).

 

What is a temperature inversion?

FAA-H-8083-28
Weather Meteorology

Answer:

  • Definition:
    • A temperature inversion occurs when temperature increases with altitude, reversing the normal lapse rate.
  • Types and Effects:
    • Inversion Aloft:
      • Allows warm rain to fall through colder air below, which can lead to freezing rain and icing hazards.
    • Ground-Based Inversion:
      • Traps fog, smoke, and pollutants, leading to poor visibility.
      • Creates stable air conditions with little to no turbulence.

 

What should a pilot do if they unexpectedly encounter icing conditions?

FAA-H-8083-15
Weather Meteorology

Answer:

  • Exit the Icing Conditions:
    • Leave the area of precipitation to avoid further ice accumulation.
    • Change altitude to reach warmer air above freezing.
  • If Unable to Exit:
    • Consider an immediate landing at the nearest suitable airport.
  • Additional Considerations:
    • If the aircraft has anti-ice or de-ice systems, activate them.
    • Monitor airspeed, control responsiveness, and climb performance.
    • Communicate with ATC for assistance in finding a safer route or altitude.

 

What is the freezing level, and how can a pilot determine its location?

FAA-H-8083-28
Weather Meteorology

Answer:

  • Definition:
    • The freezing level is the lowest altitude where the air temperature reaches 0°C.
    • Multiple freezing levels can exist due to temperature inversions.
  • Determining the Freezing Level:
    • Current Icing Products (CIP) and Forecast Icing Products (FIP).
    • Freezing Level Graphics Chart – Provides a visual representation of freezing altitudes.
    • Graphical Forecasts for Aviation (GFAs) – Displays freezing levels across a flight region.
    • PIREPs – Pilot reports on in-flight icing conditions.
    • AIRMETs and SIGMETs – Identify areas of known or forecast icing hazards.
    • Surface Analysis Charts – Help locate cold air masses.
    • Low-Level Significant Weather Charts – Show freezing levels in the lower atmosphere.
    • Winds and Temperatures Aloft Forecasts – Indicate air temperatures at various altitudes.

 

What are the three types of structural ice that can form on an aircraft in flight?

FAA-H-8083-28
Weather Meteorology

Answer:

  1. Clear Ice (Glaze Ice):
    • Glossy, transparent, or translucent ice that forms slowly as large, supercooled water droplets freeze gradually.
    • More common in warmer temperatures (closer to freezing), high liquid water content, and large droplets.
    • Can be hard to detect and difficult to remove, increasing aircraft weight and disrupting aerodynamics.
  2. Rime Ice:
    • Rough, opaque, and milky ice that forms instantly when small, supercooled water droplets freeze on impact.
    • Occurs in colder temperatures with lower liquid water content and smaller droplets.
    • More common and easier to remove than clear ice but still disrupts airflow over the aircraft.
  3. Mixed Ice:
    • A combination of clear and rime ice, forming uneven and rough ice layers.
    • Occurs in variable temperature and moisture conditions, where both large and small droplets exist.
    • Can create aerodynamic and control issues due to its irregular shape and weight buildup.
  • General Temperature Ranges for Icing Types:
    • Rime ice: Colder than -15°C.
    • Clear ice: Warmer than -10°C.
    • Mixed ice: Between -15°C and -10°C.

 

What are the three main types of icing that can affect an aircraft?

FAA-H-8083-28
Weather Meteorology

Answer:

  1. Structural Icing:
    • Forms on the airframe, wings, propeller, and control surfaces.
    • Disrupts aerodynamic flow, reducing lift and increasing drag.
  2. Induction System Icing:
    • Occurs in the engine’s air intake, restricting airflow.
    • Includes carburetor icing, which can cause engine power loss or failure.
  3. Instrument Icing:
    • Forms on pitot tubes, static ports, and antennas.
    • Can lead to incorrect instrument readings, affecting airspeed, altitude, and climb/descent indications.