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Air - Altitude Density and Volume

The density of air varies with the elevation above sea level

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The density of air varies with the air 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). The variation is about +/- 5%.

Altitude and Air Pressure

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

Altitude and Air Density

The air density is proportional with the absolute pressure. If the pressure at an altitude is named H, the ratio H/Ho decreases from 1 at sea level, to 0.74 at altitude 2,400 m. At 2,400 m the pressure is decreased with approximately 26%.

The ratio H/Ho can be expressed as in the chart below:

air density altitude

TP - Standard Temperature and Pressure

NTP - Normal Temperature and Pressure

Altitude and Air Volume

The volume of standard air at a certain level can be calculated 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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