Atmospheric pressure

From Wikipedia, the free encyclopedia
Jump to: navigation, search
This plastic bottle was sealed at approximately 14,000 feet altitude, and was crushed by the increase in atmospheric pressure (at 9,000 feet and 1,000 feet) as it was brought down towards sea level.

Atmospheric pressure is a force in an area pushed against a surface by the weight of air in Earth's atmosphere. The earth is covered in a layer of air. However, this layer is not distributed evenly around the globe. At different times, the layer of air is thicker in some places than in others. Where the layer of air is thicker, there is more air. Since there is more air, there is a higher pressure in that spot. Where the layer of air is thinner, there is a lower atmospheric pressure.

The higher the altitude, the thinner the air is, and the lower the atmospheric pressure is. This is because high places do not have as much air above them, pushing down.

Mercury barometers can be used to measure atmospheric pressure.[1] There is the same atmospheric pressure from all directions. Atmospheric pressure is measured in hPa.

References[change | change source]

Other websites[change | change source]