Final answer:
In the stratosphere, temperatures generally increase with height due to the absorption of UV radiation by the ozone layer.
Step-by-step explanation:
In the stratosphere, the temperatures generally increase with height. This increase in temperature is due to the absorption of ultraviolet (UV) radiation by the ozone layer. When UV radiation is absorbed, it causes a warming effect in the stratosphere. This temperature increase is in contrast to the troposphere (the layer below the stratosphere), where temperatures generally decrease with height.
Learn more about Temperature changes in the stratosphere