Projects:EASA PPL/Meteorology
- Stratosphere: Upper level, Temp constant
- Tropopause:
- Boundary, Temp is higher in polar regions, 36090ft, -56.5°C
- at equator: 55000ft, -75°C
- at polar: 25000ft, -45°C
- Troposphere:
- Half the mass of atmosphere is in the first 5km
per 1000ft | per 100m | |
---|---|---|
-> Absolute instability | >3° | |
Dry Adiabatic | 3° | 1° |
-> conditionally stable | 2-3° | |
Average (ISA) 15° @ MSL | 1.98° | 0.65° |
Saturated (Central Europe) | 1.8° | 0.6° |
-> stable | <2° | |
Dew point | 0.5° |
- Convective weather:
- Thunderstorms, hail, tornados, wind gusts, heavy showers, lightning strikes
- Altimetry:
- Pressure altitude: Indicated altitude at 1013.25 hPa setting
- Density altitude: pressure altitude corrected for non-ISA temperatures (120ft per 1°C change from ISA)
- QNH: ..N.. nautical
- True altitude:
- Wind on hPa - Wind on height
- Wind off hPa - Wind off height
- High to low - beware below
- Low to High - up in the sky
- 1) Correct altitude for pressure: 1hPa = 27ft
- 2) Correct altitude for Temp: 1% per 2.5°C change from ISA
- colder: indicated alt minus offset / warmer: indicated alt plus offset
- Col: saddle point/neutral point
- Low pressure travelling in summer: between 45° - 70°
- Clouds:
- AC - Altocumulus
- AS - Alsostatus
- CB - Cumulonimbus
- CC - Cirrocumulus
- CI - Cirrus
- CS Cirrostratus
- CU - Cumulus
- NS - Nimbostratus (moderate to severe icing)
- SC - Stratocumulus
- ST - Stratus
- Altocumulus lenticularis: mountain wave cloud, strong wind at right angle to the ridge, stable air
- Wind
- Mountain-valley:
- Katabatic: at night down from the mountains
- Anabatic: up the mountain by day
- Land-breeze: From land-to-water, during the night, weaker than sea-breeze
- Sea breeze: From the sea to land, during the day
- pressure gradient: diff between high and low
- straight isobar: pressure gradient force + coriolis force
- curved isobar: gradient wind: pressure gradient force + coriolis force + centrifugal force
- Mountain-valley: