Air Density Converter
Calculate air density in kg/m³ based on altitude, temperature, and pressure.
Compare density at different conditions for aviation, HVAC, and engineering.
Enter temperature and pressure (or altitude) to calculate air density.
Hot day, 15°C up to 35°C: density drops 6.5%
First 1,000 m of altitude: density drops 9.3%
Understanding Air Density
Air density is the mass of air per unit volume, typically measured in kilograms per cubic meter (kg/m³) or pounds per cubic foot (lb/ft³). It varies significantly with altitude, temperature, and atmospheric pressure. Understanding air density is critical in aviation (lift and engine performance), HVAC engineering (air handling systems), meteorology, and automotive engineering (engine tuning and aerodynamics).
The Ideal Gas Law for Air Density:
Air density can be calculated using the ideal gas law:
ρ = P / (R × T)
Where:
- ρ (rho) = air density in kg/m³
- P = absolute pressure in Pascals (Pa)
- R = specific gas constant for dry air = 287.058 J/(kg·K)
- T = absolute temperature in Kelvin (K = °C + 273.15)
Standard Atmosphere Values (ISA):
The International Standard Atmosphere defines reference conditions at sea level:
- Temperature: 15°C (59°F, 288.15 K)
- Pressure: 101,325 Pa (1013.25 hPa, 29.92 inHg)
- Density: 1.225 kg/m³ (0.0765 lb/ft³)
Air Density at Different Altitudes:
| Altitude | Temperature (ISA) | Pressure (hPa) | Density (kg/m³) | % of Sea Level |
|---|---|---|---|---|
| Sea level | 15.0°C | 1013.25 | 1.225 | 100% |
| 1,000 m (3,281 ft) | 8.5°C | 898.75 | 1.112 | 90.7% |
| 2,000 m (6,562 ft) | 2.0°C | 794.95 | 1.006 | 82.2% |
| 3,000 m (9,843 ft) | -4.5°C | 701.09 | 0.909 | 74.2% |
| 5,000 m (16,404 ft) | -17.5°C | 540.20 | 0.736 | 60.1% |
| 8,000 m (26,247 ft) | -37.0°C | 356.00 | 0.525 | 42.9% |
| 10,000 m (32,808 ft) | -50.0°C | 264.36 | 0.413 | 33.7% |
Type any of those altitudes into the box above and the calculator returns the same pressure and temperature, because it runs the same standard-atmosphere formulas rather than reading from a table.
Temperature Effect on Density (at sea level pressure):
| Temperature | Density (kg/m³) | % Change from 15°C |
|---|---|---|
| -20°C (-4°F) | 1.395 | +13.9% |
| 0°C (32°F) | 1.293 | +5.5% |
| 15°C (59°F) | 1.225 | Baseline |
| 30°C (86°F) | 1.165 | -4.9% |
| 40°C (104°F) | 1.127 | -8.0% |
Unit Conversions:
1 kg/m³ = 0.06243 lb/ft³1 lb/ft³ = 16.018 kg/m³1 kg/m³ = 0.001 g/cm³
Where it shows up
On a 35°C afternoon at sea level, density falls to about 1.146 kg/m³, 6.5% below standard. That is enough to lengthen a light aircraft’s takeoff roll noticeably and to cost a naturally aspirated engine measurable power. Denver sits at 1,609 m, where standard density is about 1.047 kg/m³, 85.4% of sea level, which is the reason baseballs carry at Coors Field and the reason the Broncos’ visiting teams complain. Rule of thumb for engines: roughly 3% less power per 1,000 feet of altitude, and turbochargers exist largely to undo that.
The counterintuitive one is humidity. Humid air is less dense than dry air at the same temperature and pressure, not more, because a water molecule weighs 18 while the nitrogen and oxygen it displaces weigh 28 and 32. Muggy air is thin air. Pilots roll altitude, temperature and humidity together into a single figure called density altitude, which answers the only question that matters on a hot day at a high field: what altitude does the aeroplane think it is at?
HVAC sizing runs into the same thing from the other end. Lower density means a given mass of air needs more volume, so ductwork sized at sea level is undersized in Denver.
How we build and check this converter
This converter runs entirely in your browser, so the numbers you enter stay on your device. The math behind it is written by hand and tested against worked examples and standard references before the page goes live.
SuperGlobalCalculator is independently built and maintained. See how we build and verify our calculators.
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