Atmospheric pressure arises from the cumulative force exerted by air molecules colliding with surfaces, defined as force per unit area. The magnitude depends on the density of the atmosphere and the height of the air column above a specific point. As altitude increases, the atmosphere becomes less dense, resulting in fewer molecular collisions and a corresponding decrease in pressure. Candidates must articulate the relationship between height, air density, and the weight of the air column to explain phenomena such as ear popping or the operation of barometers.
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