How does the temperature change with altitude in the stratosphere and thermosphere?

In the stratosphere, temperature increases with altitude due to the absorption of ultraviolet radiation by the ozone layer, which warms this region. In contrast, in the thermosphere, temperature also increases with altitude, but this is due to the absorption of high-energy solar radiation by sparse gas molecules, resulting in very high temperatures despite the low density of air. Thus, both layers exhibit a temperature inversion, with warmer temperatures at greater altitudes.