It is on the bottom. It is pool of ozone molecules.
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.
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.
That would be the 2nd layer, the stratosphere layer with the ozone at top.
The stratosphere extends from about 11 kilometers to 50 kilometers above the Earth's surface. This layer contains the ozone layer, which absorbs and scatters the sun's ultraviolet radiation. Temperature increases with altitude in the stratosphere due to the absorption of UV radiation by the ozone layer.
The ozone layer is located in the top layer of the stratosphere
The temperature in the stratosphere increases with altitude because the ozone lies in the stratosphere. The ozone layer absorbs harmful ultraviolet rays from the sun. Higher in the stratosphere the ozone is thicker and absorbes more radiation, which makes it warmer.
The second major layer of Earth's atmosphere is the stratosphere. It extends from about 10 to 50 kilometers above the Earth's surface. The stratosphere is characterized by the presence of the ozone layer, which absorbs much of the Sun's ultraviolet radiation.
No, the ozone is not situated on ionosphere. It is there is stratosphere.
The stratosphere has a relatively constant temperature because it contains the ozone layer, which absorbs and traps solar radiation, leading to a stable temperature profile in this layer of the atmosphere.
The four main layers of the atmosphere in order from closest to the Earth's surface to farthest are the troposphere, stratosphere, mesosphere, and thermosphere. The troposphere is where weather occurs and is closest to the Earth's surface. The stratosphere contains the ozone layer and has a stable temperature. The mesosphere is the layer where meteors burn up upon entering. The thermosphere is the outermost layer and contains the ionosphere where auroras are formed.
The ozone layer is a few miles / kilometers thick, and has variable concentration with lower values at "top" and "bottom". It cannot have a hard "distance" without nuance in meaning. The Earth's radius at the poles is 6356.8 km, and at the equator 6378.1 km. The ozone layer starts about 10 km above this at the equator, and less than this near the poles. So it starts about 6388.1 km, and ends about 6428.1 km near the equator. 10-50 km + 6378 km near the equator.