The standard atmosphere
The International Standard Atmosphere (ISA) is the fixed reference for every altimeter, chart and performance table. Real layers: see atmospheric-layers.
ISA at sea level (TC AIM AIR 1.5.1):
| Quantity | Value |
|---|---|
| Air | perfectly dry gas (TC AIM AIR 1.5.1(a)) |
| Temperature | 15 °C |
| Pressure | 29.92 in.Hg = 1013.2 hPa |
- 1 hPa = 1 mb: renamed millibar. 1013.2 hPa = 1013.2 mb (TC AIM MET 3.3 (1 mb equals 1 hPa); sample exam Q18: 29.92 in. Hg or 1013.2 mb).
Temperature with height (TC AIM AIR 1.5.1(d)):
- Falls 1.98 °C per 1000 ft; rule of thumb about 2 °C (PHAK ch.11).
ISA temp = 15 - 1.98 x thousands of ft. Example, 10,000 ft: 15 - 19.8 = about -5 °C.- Falls to the tropopause (see atmospheric-layers), constant above.
- Rate is the surrounding air's, not a rising parcel's (see parcel-temperature-lapse-rates).
Pressure and density both fall with height:
- Pressure falls fastest low down, where most air sits; slower higher up.
- About 1 in.Hg per 1000 ft (TC AIM AIR 1.5.3) up to 10,000 ft (PHAK Principles of Flight, Atmospheric Pressure).
- About half the atmosphere's weight is below 18,000 ft (PHAK ch.12 Atmospheric Pressure).
| Density at constant | Density is |
|---|---|
| Temperature | directly proportional to pressure |
| Pressure | inversely proportional to temperature |
(PHAK Principles of Flight, Effect of Pressure on Density; Effect of Temperature on Density)
Trap: pressure falls fastest low down, not up high: the air is densest there.
References
- TC AIM AIR 1.5.1
- TC AIM AIR 1.5.3
- TC AIM MET 3.3
- TP 13014 sample exam Q18
- FAA Pilot's Handbook of Aeronautical Knowledge (FAA-H-8083-25)