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How does air pressure work?

Published in Atmospheric Pressure 2 mins read

Air pressure works because of the constant motion of air molecules exerting force on surfaces they contact.

Think of air as a sea of tiny, constantly moving particles (atoms and molecules). These particles are everywhere around you, zooming in random directions. The force of these particles colliding with a surface creates what we perceive as air pressure. The more frequently and forcefully these molecules hit a surface, the higher the air pressure. The number of air molecules decreases as altitude increases, therefore less collisions occur at higher altitudes.

Here's a more detailed breakdown:

  • Molecular Motion: The atoms and molecules making up the atmosphere are always in motion. This motion is random and ceaseless.
  • Collisions Create Pressure: When these moving molecules strike a surface, they exert a tiny force. The sum of all these tiny forces over a given area is what we measure as pressure. As mentioned in the provided reference, "when they strike a surface, they exert a force on that surface in what we observe as pressure."
  • Number of Molecules: The more molecules present in a given space (density), the more collisions will occur, and the higher the pressure will be. The atmosphere is denser near the Earth's surface due to gravity, leading to higher air pressure at lower altitudes. This explains why air pressure decreases with height, as stated in the reference that "the number of molecules in the atmosphere decreases with height."
Factor Effect on Air Pressure
Number of Molecules Increases Pressure
Molecular Speed Increases Pressure

Analogy: Imagine a room full of people bouncing beach balls off the walls. The more people there are, and the faster they throw the balls, the greater the force on the walls. That's essentially how air pressure works.

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