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The density of air will vary with the pressure (the Ideal Gas Law) and the altitude above sea level. Mean absolute pressure at sea level is approximately 760 mmHg (101.325 kPa, kN/m2) with a variation is about +/- 5%.
The air pressure varies with altitude as shown in the table below:
| Altitude (m) |
Barometer (mmHg) |
| 0 | 749 |
| 75 | 743 |
| 150 | 735 |
| 250 | 726 |
| 300 | 723 |
| 450 | 709 |
| 600 | 695 |
| 750 | 681 |
| 900 | 668 |
| 1,000 | 658 |
| 1,200 | 643 |
| 1,350 | 632 |
| 1,500 | 620 |
| 1,800 | 598 |
| 2,100 | 577 |
| 2,400 | 555 |
Air density and specific volume as functions of altitude above sea level are indicated in the diagrams below:
The specific volume of standard air at a certain altitude can be calculated by multiplying with the volume correction factor below
| Altitude | Volume Correction Factor | |
| (m) | (ft) | |
| 0 | 0 | 1.00 |
| 480 | 1600 | 1.05 |
| 990 | 3300 | 1.11 |
| 1500 | 5000 | 1.17 |
| 1980 | 6600 | 1.24 |
| 2460 | 8200 | 1.31 |
| 2970 | 9900 | 1.39 |
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