Weather Pattern
https://www.aviationweather.gov/1. Stable and unstable air
2. Air masses and fronts
Stable and unstable air
Stability of Atmosphere
- Hot air is light that cold air and it rises
- The lifted air continue to rise and is refer to as unstable atmosphere it is measure by the lapse rate
- Standard lapse rate - Decrease 2 Deg C for each 1000 feet in altitude increase
- If it decreases more quickly - Unstable air
- If it decreases less quicker - Stable air
Temperature affect the stability of atmosphere
Add mixture decrease stability
moisture light that air .. the air density
remove moisture increase stability
moisture mremove density - increase stability
stable air resist rising
Stable air - stable air rises up the slope produces stratus clouds, smooth air, steady precipitation
Unstable Air
- Turbulance
- Good surface visibility,
- Moisture unstable airmass result in cumulus clouds and showery precipitation
Keep on rising -
lots of vertical development
2. Air Masses and Fronts
Airmass - huge body of air similar temp and moisturesource region
- cold polar
- Warm
Continental - dry
Maritime tropical - warm moist
Factor affecting
speed
temperature deference
depth
FRONT
Boundary between air mass is call a front
Types of Fronts:
1. Cold Front Types
- Fast moving pressure wave or squall line
- cold moving not as violent
2. Warm Front - warm air behind and cold air ahead
3. Stationary Front - moving less that 5
Occlusion
- cold front - fast moving cold front in front of warm front
- warm front -
Cross a Front is discontinuities
- Temperature change
- Shift of wind direction
- Change in wind speed
Weather Hazards
- Fog
- Thunderstorm
- Wind Shear and microburst
- Turbulence
Windshear and Microburst
Microburst
- precipitation drags the air down
- precipitation cool
- horizontal and vertical airspeed
- down draft - 6000'
convective activity
1 miles in diameter ..
spread out near the ground to 2.5"
45 knots in each direction
- Ring of dust
last about 4 mins not more than 15 mins
if encounter microburst - divert to another airport and wait another 15 mins before landing
Thunderstorm
- light momentary change in altitude and or attitude
- light chops
Moderate Turbulence i
Change in altitude and altitude maintain control of the airplane at all times
Sever Turbulence
large and abrupt change in altitude and or attitude
large variation
momentary loose control of the airplane
Extreme Turbulence
Tossed about practically impossible to control
convective Turbulence hot air
Bellow puffy air -- it cool down
Mountain wave - lenticular clouds
Clear air turbulence - not associated with thunderstorm but associate with jet stream
hot air in cecinityu of jet stream
Thunderstorm
- lightning
- Wind shear
Types of Thunderstorms
1. Isolated air mass2. Frontal thunderstorm
3. squall line thunderstorms
Basic ingredients for a cumulonimbus cloud to form
- lifting force- unstable air
- moist air (high humidity)
Stages of Thunderstorm
- Cumulus stage
- Continuous updraft
- Mature stage
- Precipitation begins strong updraft
- Strong down draft
- Precipitation start to fall
- Dissipate stage
- Predominately downdrafts
- Air current move down and out
Structure Ice
visible moisture
clouds, snow
ice pellets - warmer air at higher altitude, freezing rain
Frost - temperature of collecting surface is or at freezing and the
No comments:
Post a Comment