Ch 6 Weather Flashcards
Unstable air
- cloud, rain, turbulence, visibility
more vertical development, moist and warm
- cumulus clouds
- shower rains
- rough turbulence
- good visibility
Wake Turbulence
1. when departing after lg aircraft landed
2. landing behind lg aircraft
3. taking off behind lg aircraft
4. lg aircraft just taken off & you approach to land
- lift off beyond their touchdown
- land beyond their touchdown
- lift off before the lg aircraft rotation pt.
- touchdown before the lg aircraft’s liftoff point.
- Rime ice
- Clear ice
- Mixed
- can be found in stratus clouds, instant icing, small drops -20C & -15C
- develops in an area of large supercooled water droplets, difficult to see, -10C & 0C
- occurs in temp. between -10C & -15C
Classification
Polar or tropical
- cool or warm
Continental or Maritime
- dry or moist
Clouds with vertical development
- cumulus= can indicate a shallow layer of instability, turbulence, little icing
- Towering Cumulus= indicate a fairly deep area of unstable air, moderate to heavy turbulence w/ icing. Often develop into thunderstorms
- Cumulonimbus (rainmaker)= large, vertically developed, in very unstable air. contain large amount of moisture
Temperature inversions
occur in stable air calm winds, near the sfc on cool, clear nights
sfc is cooler than the air above it and visibility is poor, restricted by fog / low clouds
- Gas to Liquid
- Liquid to Gas
- condensation
- evaporation
- air mass thunderstorm
- severe thunderstorm
- short-lived, no strong winds
- wind gusts +50 kt, tornadoes, hail
Mountain Breeze
night, downslope flow, 5 to 15 kt
Convective turbulence
aka ?
aka thermal turbulence
daytime over land in fair weather
rising heated air from the sfc
when air is moist, the currents may be marked by build-ups of cumulus clouds
Squall line
Mixture of storms in a continuous line
Land Breeze
night, from the cooler land to the warmer water
Alt: 1,000 to 2,000 AGL
extend between 5 and 100 NM inland
High Clouds
Alt: base above 20,000 agl
serius icing and turbulence
- cirrus= above 30,000, thin, patches or narrow bands. can warn approaching bad weather
- cirrostratus= thin, layer/ sheet, low moisture, no icing
- cirrocumulus= patchy, light turbulence
LLT (low-level turbulence)
4
- Below 15,000 MSL
- due to sfc heating or friction
1. mechanical
2. convective
3. wake turbulence
4. frontal turbulence
Cold front
1. fast moving
2. slow moving
- sfc friction slows the mvmt
leading edge bulge out & steepen front’s slope - leading edge shallower
- meets stable air = stratus form behind
- unstable air = lg # of vertical clouds form
The greatest instability occurs when
the air is both warm and moist
- Wind Shear
- Microburst
- drastic shift in wind speed and direction, wind shear turbulence is associated with all thunderstorms
- can last more than 15 min. and wind speed of 25 kt
Convection
cool air= heavier, denser > sinks
warm air= lighter, less dense > rises
movement of air up and down
Mountain Wave Turbulence
stable air moves across a ridge
wind is +40 kt
When you encounter turbulence when approach for landing
- fly a power-on approach at an airspeed slightly above the normal approach speed.
- fog
- ground fog
- radiation fog
- any low cloud within 50ft of ground
- less than 20ft deep
- flat sfc on clear, calm, humid nights. stable air associated w/ H pressure systm.
Atmospheric Pressure
The unequal heating of the sfc modifies air density, creates circulation patterns and causes changes in pressures
Atmospheric Composition
78% Nitrogen
21% Oxygen
1% other gases
A cubic foot of the atmosphere can contain from 0 to 4% of water vapor. Responsible for major changes in the weather.
What changes when crossing a front
temp.
pressure
wind
Source Region
Area where air mass gets the properties of temp. and moisture that determines its stability