Low-level turbulence can occur and icing can become hazardous in which type of fog?
Steam fog.
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Steam fog forms in winter when cold, dry air passes over comparatively warm water. The result is low level turbulence and icing.
The Terminal Aerodrome Forecast (TAF) is:
Specific to an airport.
A TAF is a report established for the five statute mile radius around an airport.
Cold front shape on charts
pointed barbs
warm front shape on charts
rounded barbs
Upon encountering severe turbulence, which flight condition should the pilot attempt to maintain?
Level flight attitude.
Maintain a constant attitude, let the aircraft “ride the waves”.
What information is contained in a CONVECTIVE SIGMET?
Tornadoes, embedded thunderstorms, and hail 3/4 inch or greater in diameter.
A Convective SIGMET contains data regarding severe thunderstorms including, tornadoes, and large hail, ¾” or more in diameter. Embedded thunderstorms are also forecast on Convective SIGMETs.
Which weather conditions should be expected beneath a low-level temperature inversion layer when the relative humidity is high?
Smooth air, poor visibility, fog, haze, or low clouds.
A ground based inversion favors poor visibility by trapping fog, smoke, and other restrictions into low levels of the atmosphere. An inversion is a stable air mass and would have smooth air.
Minimum practical visibility VFR
3 miles
VFR minimum ceiling hieght
1000 feet AGL
Types of clouds (general)
layered (stratus)
cumulus
Smooth or bumpy flight expected with layered (stratus) clouds
smooth
stable atmospheric conditions
Visibility with layered (stratus) clouds
Fair - poor
fog is a type of layered cloud
Cumulus clouds are associated with
unstable air with vertical development
Cumulus cloud flight is (bumpy/smooth) and visibility is:
bumpy flight with high visibility
Troposhere extends to (height in feet)
40,000 feet
What is a temperature inversion
Temperature increases with altitude (usually decreases with altitude)
Stable layer of atmosphere
poor visibility
Why poor visibility in inversions
Pollutants trapped lower - less vertical air movement
Relative humidity
Ratio of current water vapor to the max possible at that temp and pressure
Dew point
Temperature at which air becomes saturated (100% relative humidity)
Describe radiation fog
-Forms on clear nights over flat land
-Caused by ground cooling the air to the dew point
-Light winds deepen fog
-usually dissipates by noon
-rarely over water bodies
Describe advection fog
-When warm, moist air moves over a colder surface
-common along coasts and large lakes
-Can occur day or night
- Light to moderate winds deepen fog
Describe upslope fog
-Formed by moist, stable air being forced uphill
-Common on eastern slopes of mountains
-Dense and persists until upslope wind ceases
Describe precipitation-induced fog
-Caused by evaporation or drizzle
-occurs with frontal activities and non-frontal precipitation
-can form rapidly over large areas and persist
Precipitation-induced fog, also called frontal fog, forms when warm rain falls through cooler, drier air. As the rain evaporates into the colder air, it increases the air’s moisture content until it reaches (100\%) humidity, causing the water vapor to condense into fog
Conditions favorable for fog formation
-Small temperature-dew point spread
-calm or light winds
-Precipitation adding moisture to the air
-Abundance of condensation nuclei
-Cooling processes