Applications of fluid statics: Archimedes and the atmosphere
Atmospheric pressure and its measurement
Air, a fluid that has weight
The Earth's atmosphere also exerts a pressure on every surface, called atmospheric pressure. At sea level, it averages 1013 hPa (about 101,300 Pa), a value often rounded to 1 bar.
Torricelli's barometer
In 1643, Torricelli measured atmospheric pressure using a tube filled with mercury and inverted in a mercury reservoir. The mercury drops in the tube until the pressure exerted by the remaining column exactly balances atmospheric pressure. At sea level, this column measures about 760 mm, hence the historical unit "mm of mercury" (mmHg).
Pressure decreases with altitude
The higher up you go, the less air there is above you, so the pressure decreases.
| Altitude | Average pressure |
|---|---|
| 0 m (sea level) | 1013 hPa |
| 3000 m | about 700 hPa |
| 8848 m (Everest) | about 340 hPa |
Common pitfall
Don't confuse the units: 1 bar = 1000 hPa = 100,000 Pa. A frequent mistake is writing "1013 Pa" instead of "1013 hPa," which gives a pressure 100 times too low. The Magdeburg hemispheres experiment (1654) spectacularly illustrates the strength of this pressure: two teams of horses could not separate two half-spheres emptied of air.

