AVWX Flashcards
What is the cause of all weather changes?
Uneven heating of the Earth’s surface, causing pressure and air density differences.
FAA-H-8083-28, Aviation Weather Handbook
What are characteristics of cold fronts?
Cold fronts typically move at approximately the speed of prevailing wind and create lift along leading edge, conducive to cumulous cloud development, medium to heavy precipitation, showery at times.
FAA-H-8083-28, Aviation Weather Handbook
What are characteristics of warm fronts?
Warm fronts move at about half of the prevailing wind speed and can be conducive to stratus cloud development, constant light precipitation and low visibilities.
FAA-H-8083-28, Aviation Weather Handbook
What are characteristics of occluded fronts?
Occluded fronts can cause weather similar to that of warm fronts and cold fronts. Embedded thunderstorms may be possible.
FAA-H-8083-28, Aviation Weather Handbook
What are characteristics of stationary fronts?
Stationary fronts can cause weather similar to cold fronts and be stagnant until the cold front typically moves through the area.
FAA-H-8083-28, Aviation Weather Handbook
Definition of a temperature inversion
A layer of warm air above colder air.
FAA-H-8083-28, Aviation Weather Handbook
What causes a surface based temperature inversion and what are the impacts to aircraft operations in the area?
A surface-based low-level temperature inversion can be caused by extreme surface cooling under clear skies and light/calm wind conditions can cause poor visibility. Low-level wind shear (LLWS) is possible during climb or descent through the layer of stable air which separates calm air close to the surface from higher wind speed above.
FAA-H-8083-28, Aviation Weather Handbook
What are characteristics of the troposphere?
Layer of atmosphere from Earth’s surface to approximately 36,000 feet in the mid latitudes.
Large-scale vertical air motions
Standard lapse rate 2°c/1,000’
50% atmospheric moisture below 6,500’
Most weather occurs
FAA-H-8083-28, Aviation Weather Handbook
What are characteristics of the stratosphere?
Layer of the atmosphere which starts at approximately 36,000 feet in the mid latitudes.
Horizontal/stratified air motion
Common location for jet stream
Little or no temperature change with increase in altitude, eventually increasing with altitude around 45-50,000’
FAA-H-8083-28, Aviation Weather Handbook
What are air motions in a low pressure area?
Counter-clockwise and rising air, conducive to an unstable atmosphere and cumulous cloud development.
FAA-H-8083-28, Aviation Weather Handbook
What are air motions in a high pressure area?
Clockwise and sinking air, conducive to a stable atmosphere and stratus cloud development.
FAA-H-8083-28, Aviation Weather Handbook
What causes cloud development?
Temperature and dew point converge (condensation of atmospheric moisture).
FAA-H-8083-28, Aviation Weather Handbook
What atmospheric conditions are conducive to development of cumulous clouds?
Low pressure, unstable atmosphere, and a lifting mechanism (surface heating, orographic lifting, frontal (cold) lifting).
FAA-H-8083-28, Aviation Weather Handbook
What atmospheric conditions are conducive to development of stratus clouds?
High pressure, stable atmosphere.
FAA-H-8083-28, Aviation Weather Handbook
List types of fog
Radiation fog
Advection fog
Upslope fog
Steam fog
Frontal fog
FAA-H-8083-28, Aviation Weather Handbook
What atmospheric characteristics are conducive to thunderstorm (cumulonimbus cloud) development?
Sufficient moisture
Unstable atmosphere
Lifting mechanism(s) such as buoyancy (surface heating), orography (rising terrain), and/or frontal lifting (cold or occluded front)
FAA-H-8083-28, Aviation Weather Handbook
What is the difference between an air mass thunderstorm and a steady state (severe) thunderstorm?
Air mass = localized, results mostly from surface heating
Steady state = associated with organized surface weather systems (cold fronts, hurricanes)
FAA-H-8083-28, Aviation Weather Handbook
Name and describe the stages of a thunderstorm and which stage presents the greatest hazards?
1.Cumulous (continuous updrafts initially build cumulonimbus cloud)
2.Mature (precipitation produces downdrafts, updrafts continue)
3.Dissipating (downdrafts exceed updrafts, cloud collapses)
Greatest hazards exist during mature stage (turbulence, potential severe wind shear, lightning, hail, airframe icing).
FAA-H-8083-28, Aviation Weather Handbook
List all thunderstorm hazards
1.Turbulence, potential severe wind shear, microburst
2.Lightning
3.Hail
4.Airframe icing
5.Pressure changes can cause altimeter inaccuracy.
FAA-H-8083-28, Aviation Weather Handbook
What is wind shear?
Any sudden change in wind direction and/or speed, particularly when it occurs over relatively short distance in flight. Low-level wind shear (LLWS) occurs below 2,000 feet AGL.
FAA-H-8083-28, Aviation Weather Handbook
What is a microburst?
Local wind shear as a result of heavy rain from a cumulonimbus (CB) cloud (thunderstorm).
Downdraft is caused by heavy rain falling, accelerated by its colder temperature than surrounding air. Can be as much as 6,000 fpm and causes horizontal winds as much as 45 knots upon striking the ground, resulting in potential total shear of as much as 90 knots across the microburst.
FAA-H-8083-28, Aviation Weather Handbook
What is a jet stream and how does time of year affect it?
High-speed organized band of wind with speeds 50 knots or greater in the vicinity of the tropopause. In the winter, the jet stream is higher speed, lower in height, and further south.
FAA-H-8083-28, Aviation Weather Handbook