Oxygen and nitrogen absorb most of the UV-C and more energetic light from the Sun. Ozone uniquely absorbs UV-B (which protects the DNA of all surface life on Earth), one narrow band of blue and that only slightly, and very strongly in the far infrared (as do most greenhouse gases). Oxygen and nitrogen as typical diatomic gases cannot normally radiate energy away as heat. So when ozone is present, the ozone gets "knocked around", and it can serve to radiate this heat way. Ozone then serves to make the atmosphere *appear* warmer, from coupling heat from the oxygen and nitrogen in the stratosphere, scattering some of the UV-B's energy as heat, and capturing heat from the Earth's surface and the Sun. Depletion makes the stratosphere appear to cool.
Since ozone is inherently unstable, increasing temperature pushes the equilibrium of production away from making ozone, and also increases the rate of destruction of ozone (whether by time or "contaminants"). Temperature is not a good indicator of ozone health, however, as ozone "speaks" in infrared whereas oxygen and nitrogen at that same altitude does not.
The stratosphere is the layer where the temperature increases due to the absorption of ultraviolet (UV) radiation by ozone. This absorption of UV radiation heats up the stratosphere, creating a temperature inversion where the temperature increases with altitude.
The stratosphere is the layer that is warmed from below by the ozone layer. Ozone absorbs ultraviolet radiation from the sun, which causes the stratosphere to warm up as the ozone molecules absorb and release this energy. This process creates a temperature inversion where the upper stratosphere is warmer than the lower stratosphere.
In the stratosphere, the temperature increases with height. This is due to the presence of the ozone layer near the top of the stratosphere. The ozone layer absorbs incoming UV radiation, and thus the temperatures are warmer at the top of the stratosphere than at the bottom.
Stratosphere is the layer of atmosphere which contains the ozone. The ozone is located as the ozone layer.
The ozone layer is kept in place by the Earth's stratosphere, a region of the atmosphere where temperature increases with altitude. This temperature gradient prevents the ozone from drifting away and helps it to remain concentrated in the stratosphere.
The temperature of ozone layer is same as stratosphere. It is because ozone layer is in stratosphere.
The stratosphere is the layer where the temperature increases due to the absorption of ultraviolet (UV) radiation by ozone. This absorption of UV radiation heats up the stratosphere, creating a temperature inversion where the temperature increases with altitude.
The stratosphere is the layer above the troposphere (where we live). The ozone layer is found in the lower stratosphere. The stratosphere is the lowest layer where temperature increases with increasing altitude.
The stratosphere is the layer that is warmed from below by the ozone layer. Ozone absorbs ultraviolet radiation from the sun, which causes the stratosphere to warm up as the ozone molecules absorb and release this energy. This process creates a temperature inversion where the upper stratosphere is warmer than the lower stratosphere.
In the stratosphere, the temperature generally increases with altitude. This is because in the stratosphere, the absorption of ultraviolet radiation from the sun by the ozone layer produces a temperature inversion, causing the temperature to rise with altitude.
The ozone layer is present in the stratosphere. It is because of the perfect UV radiation and temperature to form ozone.
In the stratosphere, the temperature increases with height. This is due to the presence of the ozone layer near the top of the stratosphere. The ozone layer absorbs incoming UV radiation, and thus the temperatures are warmer at the top of the stratosphere than at the bottom.
In the stratosphere, the temperature increases with height. This is due to the presence of the ozone layer near the top of the stratosphere. The ozone layer absorbs incoming UV radiation, and thus the temperatures are warmer at the top of the stratosphere than at the bottom.
The stratosphere is the layer of the atmosphere that contains two distinct parts: the lower stratosphere and the upper stratosphere. The stratopause boundary separates these two regions, with the lower stratosphere characterized by a temperature inversion and the upper stratosphere containing the ozone layer.
Stratosphere is the layer of atmosphere which contains the ozone. The ozone is located as the ozone layer.
The ozone layer is kept in place by the Earth's stratosphere, a region of the atmosphere where temperature increases with altitude. This temperature gradient prevents the ozone from drifting away and helps it to remain concentrated in the stratosphere.
The ozone layer is found in the stratosphere, which is the second layer of Earth's atmosphere. This layer is located above the troposphere, where most weather occurs, and extends from about 10 to 50 kilometers above the Earth's surface.