The thermosphere is a layer of the Earth's atmosphere that extends from the mesopause (at an altitude of about 80 km) to the exosphere (at an altitude of about 700 km and above). It is the fourth layer of the Earth's atmosphere, located above the mesosphere and below the exosphere. The thermosphere is named for its relatively high temperature, which can reach up to 2000°C due to the absorption of high-energy solar radiation.
Key characteristics of the thermosphere include:
Due to the low density of air molecules in the thermosphere, it is not able to retain heat effectively, and as a result, the temperature in this layer can vary greatly depending on solar activity. Despite the high temperatures, the thermosphere would actually feel extremely cold to a human because of the low density of molecules that would not transfer heat effectively.
When studying the thermosphere, it is important to focus on the following key points:
By mastering these key points, you will have a solid understanding of the thermosphere and its significance within the Earth's atmosphere.
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