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The thermosphere and exosphere are the warmest layers of the Earth's atmosphere because they receive intense solar radiation. In the thermosphere, solar energy is absorbed by a small number of gas molecules, raising their temperatures significantly, sometimes exceeding 1,500 degrees Celsius (2,732 degrees Fahrenheit). The exosphere, which is the outermost layer, contains very sparse particles that can also absorb solar radiation, leading to high temperatures despite the low density of matter. However, this heat isn't felt in the same way as at lower altitudes due to the lack of air pressure and density.

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2mo ago

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