Projects:EASA PPL/Meteorology: Difference between revisions
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*Low pressure travelling in summer: between 45° - 70° | *Low pressure travelling in summer: between 45° - 70° | ||
* | * | ||
== Air Masses == | |||
{| class="wikitable" | |||
|+ | |||
!prefix | |||
!suffix | |||
|- | |||
|A = Arctic | |||
|m = maritime | |||
|- | |||
|P = Polar | |||
|c = continental | |||
|- | |||
|T = Tropical | |||
| | |||
|- | |||
|E = Equatorial | |||
| | |||
|} | |||
== Clouds == | == Clouds == | ||
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** | ** | ||
**Altocumulus lenticularis: mountain wave cloud, strong wind at right angle to the ridge, stable air | **Altocumulus lenticularis: mountain wave cloud, strong wind at right angle to the ridge, stable air | ||
== Fog == | |||
* Radiation fog: at night/early day, when the ground cools. wind <5kt | |||
* Advection fog: warm, moist air over cooler ground/sea below, 10-15kt, can withstands 25kt winds | |||
* Frontal fog: ahead of warm front | |||
== Other == | |||
* CAVOK: vis 10km+, no clouds below 5000 above GND | |||
== METAR / TAF Abbreviations == |
Revision as of 15:25, 23 January 2023
Atmosphere
ThermosphereMesosphere- Stratosphere: Upper level, temperature constant
- Tropopause:
- Boundary layer, Avg 36090ft, -56.5°C
- at equator: 55000ft, -75°C
- at polar: 25000ft, -45°C
- Troposphere:
- Half the mass of atmosphere is in the lower 5km
Lapse Rate
per 1000ft | per 100m | |
---|---|---|
Absolute instability | >3° | |
Dry Adiabatic Lapse Rate | 3° | 1° |
conditionally stable | 2-3° | |
Average Environmental Lapse Rate (ISA) 15° @ MSL | 1.98° | 0.65° |
Saturated Adiabatic Lapse Rate (Central Europe) | 1.8° | 0.6° |
stable | <2° | |
Dew point | 0.5° |
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
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
-
- Col: saddle point/neutral point
- Convective weather:
- Thunderstorms, hail, tornados, wind gusts, heavy showers, lightning strikes
- Low pressure travelling in summer: between 45° - 70°
Air Masses
prefix | suffix |
---|---|
A = Arctic | m = maritime |
P = Polar | c = continental |
T = Tropical | |
E = Equatorial |
Clouds
- 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
Fog
- Radiation fog: at night/early day, when the ground cools. wind <5kt
- Advection fog: warm, moist air over cooler ground/sea below, 10-15kt, can withstands 25kt winds
- Frontal fog: ahead of warm front
Other
- CAVOK: vis 10km+, no clouds below 5000 above GND