The Structure of the Atmosphere
Earth’s atmosphere is made of several distinct layers, which are shown in this diagram. The upper and lower limits of each boundary are determined by temperature differences with altitude.
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Thermosphere: In the thermosphere, temperature increases with height. This is the location of the beautiful Aurora Borealis that occurs in the night time sky at northern latitudes. The thermosphere is characterized by the presence of charged particles called ions causing the beautiful Aurora Borealis. It is also where the International Space Station (ISS) orbits. |
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Mesosphere: This layer is just above the stratosphere. In the mesosphere, temperature decreases with height. This is where meteors burn up when entering the atmosphere. This layer is the coldest place on Earth. |
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Stratosphere: Above the troposphere is the stratosphere. This layer is heated by the Sun’s UV rays and gets warmer as it goes higher. The stratosphere contains the ozone layer. Ozone molecules absorb high-energy UV from the Sun and make life on Earth possible. Without the protection of the ozone layer, too much radiation would reach Earth’s surface. Some human activities release chemical substances called CFC’s that can destroy the ozone layer. |
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Troposphere: The troposphere is the lowest level of the atmosphere and it is where all weather occurs on Earth. It is heated by heat that radiates from Earth’s surface. In the troposphere, temperature decreases as altitude increases. |