Atmospheric pressure is the force exerted by the weight of the air above a given point on the Earth's surface. It is caused by the gravitational pull of the Earth on the air molecules in the atmosphere. Atmospheric pressure decreases with increasing altitude because there is less air above pushing down on the surface.
Atmospheric pressure is commonly measured using a barometer. The two main types of barometers are mercury barometers and aneroid barometers. Mercury barometers use the height of a column of mercury to measure pressure, while aneroid barometers use the deformation of a metal chamber.
The standard unit of pressure in the SI system is the pascal (Pa), but atmospheric pressure is often measured in millibars (mb) or inches of mercury (inHg) in weather reports. Standard atmospheric pressure at sea level is approximately 1013.25 millibars or 29.92 inches of mercury.
Here are some key points to remember when studying atmospheric pressure:
Understanding atmospheric pressure is crucial for comprehending weather patterns, air pressure systems, and their impact on the environment. Good luck with your studies!
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