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The ozone is present inside the ozone layer. The layer warmed below the ozone is the stratosphere or upper troposphere.

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10y ago

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The layer that is warmed from below by the ozonosphere is the?

There is nothing like ozonosphere. The layer that contains ozone is called Ozone layer.


What atmospheric layer is warmed from below by the ozonosphere?

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.


What layer is warmed from below by the ozonosphere?

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.


What layers are above and below the ozone layer?

Above: the rest of the stratosphereBelow: the rest of the troposphere


What are the uses of ozone layer?

See "What does the ozone layer do?" in the "Related questions" section below.


What does the ozone layer destory?

See "What does the ozone layer do?" in the "Related questions" section below.


What can you do about an ozone layer?

See "What can we do to protect the ozone layer?" in the "Related questions" section below.


What Hole is in the ozone layer?

There is not actually a hole in the ozone layer. The ozone has been reduced below some limit.


Why is ozone layer so important?

See "What does the ozone layer do?" in the "Related questions" section below.


What are the basic activities of ozone layer?

See "What does the ozone layer do?" in the "Related questions" section below.


Where did the ozone layer found?

See "Where is the ozone layer located?" in the "Related questions" section below.


What is the ozone that separates the mesosphere from the layer below it is called the?

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.