The weight of the atmosphere is commonly referred to as "atmospheric pressure." It is the force exerted by the weight of air above a given point, typically measured in units such as pascals or millibars. At sea level, atmospheric pressure averages about 1013.25 hPa (hectopascals). This pressure decreases with altitude as the amount of air above decreases.
A meteor
Meteorologist
The atmosphere becomes less dense with altitude. Atmosphere, thin though it is, has weight, and it is the weight of the air above which compresses the air below it, to greater density.
Skies themselves do not have weight in the traditional sense, as they are composed of gases in the atmosphere, primarily nitrogen and oxygen. The weight of the atmosphere can be estimated; for example, the Earth's atmosphere weighs about 5.5 quadrillion tons (5.5 x 10^15 tons). This weight is distributed over the surface of the Earth, creating atmospheric pressure.
The absence of atmosphere is called a vacuum.
The weight of air is called atmospheric pressure. It is the force exerted by the weight of the air above a given point in the atmosphere.
Meteoritesis what we call stones that enter the earths atmosphere.
Weight of the atmosphere above a surface.
Meteoritesis what we call stones that enter the earths atmosphere.
gravity
They are called meteorologists; but also exist specialties as physics of the atmosphere, chemistry of the atmosphere.
5.28 x 10000000000000000000 kg is the weight of air for the entire atmosphere.
Oxygen makes up about 20.95% of the Earth's atmosphere by weight.
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atmosphere
Atmosphere