Ozone absorbs more ultraviolet radiation than does air in the troposphere. As a result, the stratosphere is heated, and air gradually increases in temperature to the top of the layer, called the startopause.
As temperature increase pressure will increase
stephen gwapo kaayo
Its a layer of our atmosphere, above the stratosphere, but beneath the thermosphere. It starts at around an altitude of 50-60km and ends at around an altitude of around 100-120km. The temperature tends to drop with increased height through the mesosphere. At the 100-120km point is the coldest place on earth, with temperatures around -160'C. Temperatures then start to rise again with height through the thermosphere.
Jet streams are fast flowing, narrow air currents found at the tropopause, the transition between the troposphere (where temperature decreases with height) and the stratosphere (where temperature increases with height) and are located at 10-15 kilometers above the surface of the Earth. They form near boundaries of adjacent air masses with significant differences in temperature
what is the temperature when the height of air equals zero
The stratosphere is where the temperature increases with height. This is due to absorption of UV radiation by atmospheric ozone.
In the stratosphere, temperature increases with height due to the absorption of ultraviolet (UV) radiation by the ozone layer, which warms this region. In contrast, the mesosphere sees a decrease in temperature with height because it is farther from the Earth’s surface and lacks significant heat sources, leading to less absorption of solar energy. As a result, the mesosphere is cooler, especially at its upper levels.
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 generally increases with altitude. This is due to the absorption of ultraviolet (UV) radiation by the ozone layer, which warms the upper portions of the stratosphere. As you ascend through this layer, the air becomes warmer, contrasting with the troposphere below, where temperature typically decreases with height.
what is the approximate height and temperature of the troposphere, stratosphere, mesosphere, and thermosphere?
Troposphere: Temperature decreases with hight Stratosphere : Temperature increases with height
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 temperature of the stratosphere increases with height primarily due to the absorption of ultraviolet (UV) radiation from the sun by the ozone layer, which is concentrated in this atmospheric layer. As UV radiation is absorbed, it warms the surrounding air, leading to a temperature increase with altitude. This temperature inversion is in contrast to the troposphere below, where temperature decreases with height due to the decreasing pressure and density of the air.
There are four layers of the atmosphere. At the ground is the troposphere, followed by the stratosphere, mesosphere and thermosphere. Temperature decreases with height through the troposphere, increases in the stratosphere, decreases in the mesosphere, then increases again in the thermosphere.
In the Earth's atmosphere, the stratosphere is the layer where temperature increases with altitude, primarily due to the absorption of ultraviolet radiation by the ozone layer. This temperature inversion causes the stratosphere to warm as one ascends, contrasting with the troposphere below, where temperature generally decreases with altitude. Thus, the stratosphere is characterized by an increase in temperature with height.
There are four layers of the atmosphere. At the ground is the troposphere, followed by the stratosphere, mesosphere and thermosphere. Temperature decreases with height through the troposphere, increases in the stratosphere, decreases in the mesosphere, then increases again in the thermosphere.