Final answer:
Yes, the absorption of solar radiation by the ozone layer does contribute to temperature maximums near the stratopause. The ozone layer, found near the top of the stratosphere, absorbs harmful ultraviolet light which results in heating this atmospheric layer. The loss of ozone due to human activities raised concerns in the 1980s, but international efforts have since halted this loss and reduced the 'ozone hole'.
Step-by-step explanation:
The statement that temperature maximums near stratopause are due to the absorption of solar radiation by the ozone is true. The stratopause is a layer of the atmosphere found near the top of the stratosphere, known for its high concentration of ozone.
This ozone layer absorbs ultraviolet light, which adds heat to the stratosphere and thereby increases its temperature. This is a crucial process because it shields the planet from harmful ultraviolet radiation that can adversely affect life on Earth.
In the 1980s, human activities leading to ozone depletion became a concern, primarily due to the industrial production of chlorofluorocarbons (CFCs) which are harmful to the ozone. However, international agreements have led to the ban of these chemicals, resulting in the cessation of ozone loss and gradual shrinking of the 'ozone hole' over the Antarctic.
Learn more about Ozone Layer and Temperature