Earth's atmosphere
Earth's atmosphere is the layer of gases surrounding the planet Earth and retained by the Earth's gravity. It contains roughly 78% nitrogen and 21% oxygen, with trace amounts of other gases. The atmosphere protects life on Earth by absorbing ultraviolet solar radiation and reducing temperature extremes between day and night.
Pressure
:Main article: Atmospheric pressure
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Atmospheric pressure is a direct result of the weight of the air. This means that air pressure varies with location and time because the amount (and weight) of air above the earth varies with location and time. Atmospheric pressure drops by ~50% at an altitude of about 5 km (equivalently, about 50% of the total atmospheric mass is within the lowest 5 km). The average atmospheric pressure, at sea level, is about 101.3 kilopascals (about 14.7 pounds per square inch).
Related Topics:
Sea level - Kilopascal
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~ Table of Content ~
| ► | Introduction |
| ► | Temperature and the atmospheric layers |
| ► | Pressure |
| ► | Composition |
| ► | Density and mass |
| ► | The evolution of the Earth's atmosphere |
| ► | References |
| ► | See also |
| ► | External links |
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