Hazards Flashcards
Fog
Visible moisture with base below 50’ and no visible downward motion
–Fog (FG): visibility less than 5/8 SM
–Mist (BR): visibility greater to or equal to ≥ 5/8 SM
Fog
Formation Factors
Small temperature/dew point spread
Abundant condensation nuclei
Light surface wind
Cooling land surfaces, warm air above
Fog
Cooling Actions
Radiation
Adiabatic
Conduction
Fog
Dissipation Factors
Heating
Strong wind
Greenhouse effect/overcast sky
- prevents fog.
- slows fog dissipation
Fog
Types
Radiation fog
Advection fog
Precipitation-Induced fog
Upslope fog
Freezing fog
•Ice Fog
Radiation Fog
Results from radiation cooling on clear, calm nights
- Relatively shallow
- Light winds
- Midnight to sunrise
Advection Fog
Results from surface cooling
- Warm, moist air flowing over a cooler surface
- Deepens with winds 3-9 KTS
- Can be deep, persistent
Precipitation-Induced Fog
Results from precipitation falling through cool, unsaturated air
- Ahead of warm front/behind cold front
- Can be quite dense, extend over large areas, and be long-lived
Upslope Fog
Results from moist, stable air being lifted by sloping terrain
- Cools adiabatically
- Winds >10 KTS
- May cause cap clouds
Freezing Fog
Results when supercooled droplets contact freezing surface
- Supercooled droplets remain liquid until contacting freezing surface
- Sub-freezing temps
Ice Fog
Results from extremely cold temperatures and deposition
- Tiny ice crystals suspended in air
- Temps ≤-30°C
- Often seen in Arctic/Polar air
Fog
Flight Planning
Consider fog formation at destination.
–Do I have a moisture source?
–Do I have lifting action nearby?
–Is the wind strong enough to dissipate current fog?
Check weather reports.
Pick an alternate airfield.
Ask questions.
Icing
Types
Rime Ice
Clear Ice
Mixed Ice
Frost
Rime Ice
Forms from small supercooled water droplets
Easy to break loose.
Clear Icing
Forms from large supercooled water droplets
Clear, hard and glossy solid ice.
(d) Smooth or rough.
Mixed Ice
(a) Combination of rime and clear ice.
(b) Forms rapidly.
(c) Most common from -10° to -15°C.
Frost
Ice crystals formed by deposition of water vapor contacting a cold surface
Freezing Rain
Freezing rain forms when rain droplets are supercooled by passage through a layer of air which has a sub-zero temperature.
Most dangerous icing condition outside of a thunderstorm
Most common with warm fronts
Where would be a likely frontal location to find freezing rain?
Warm fronts
Thunderstorms
Development Factors
Unstable or conditionally unstable air
High moisture content
Lifting action
Thunderstorms
Types
- Air mass
- Orographic
- Frontal
Air Mass
Caused by surface heating
Orographic
Caused by terrain effects