The ozone is present inside the ozone layer. The layer warmed below the ozone is the stratosphere or upper troposphere.
There is nothing like ozonosphere. The layer that contains ozone is called Ozone layer.
Above: the rest of the stratosphereBelow: the rest of the troposphere
There is not actually a hole in the ozone layer. The ozone has been reduced below some limit.
The ozone layer that separates the mesosphere from the layer below it is called the stratopause. It serves as a boundary between the stratosphere and the mesosphere, and is characterized by a temperature inversion where temperatures increase with altitude.
The layer containing ozone is the ozone layer. It is located in the stratospheric region of the atmosphere.
There is nothing like ozonosphere. The layer that contains ozone is called Ozone layer.
The stratosphere is warmed from below by the ozone layer (ozonosphere) through the absorption of ultraviolet radiation from the sun. This absorption of UV radiation by ozone molecules contributes to the warming of the stratosphere.
The troposphere is the layer that is warmed from below by the ozone layer, also known as the ozonosphere. This warming occurs through the absorption of incoming solar radiation by the Earth's surface, which then heats the air in the troposphere.
Above: the rest of the stratosphereBelow: the rest of the troposphere
See "What does the ozone layer do?" in the "Related questions" section below.
See "What does the ozone layer do?" in the "Related questions" section below.
See "What can we do to protect the ozone layer?" in the "Related questions" section below.
There is not actually a hole in the ozone layer. The ozone has been reduced below some limit.
See "What does the ozone layer do?" in the "Related questions" section below.
See "What does the ozone layer do?" in the "Related questions" section below.
See "Where is the ozone layer located?" in the "Related questions" section below.
The ozone layer that separates the mesosphere from the layer below it is called the stratopause. It serves as a boundary between the stratosphere and the mesosphere, and is characterized by a temperature inversion where temperatures increase with altitude.