In the stratosphere, the temperature generally remains constant or may even slightly increase with increasing altitude. This is due to the absorption of ultraviolet radiation by the ozone layer, which warms the stratosphere.
1,700-foot decrease.
Temperatures in the stratosphere generally increase with altitude due to the absorption of ultraviolet radiation by the ozone layer. This temperature increase is opposite to the trend in the troposphere, where temperature decreases with altitude.
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 altitude of the stratosphere increases as you move upward from the Earth's surface. It starts at around 10-13 kilometers (6-8 miles) and extends up to about 50 kilometers (31 miles) above the Earth's surface.
The temperature increases like the stratosphere
As you move from the troposphere (closest to the surface) to the stratosphere, temperature generally decreases with altitude due to the decreasing density of the air. In the stratosphere, temperature starts to increase with altitude due to the absorption of solar radiation by ozone. Overall, the trend is a decrease in temperature with altitude in the troposphere and an increase in temperature with altitude in the stratosphere.
Temperature decreases with altitude in the mesosphere due to the decrease in atmospheric pressure with height. This is because the mesosphere is above the stratosphere where the ozone layer absorbs incoming solar radiation, leading to a decrease in temperature as altitude increases.
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.
Decrease
The temperature decreases with altitude.
stratosphere and thermosephere -Nikki Gallagher
In the stratosphere, the temperature generally remains constant or may even slightly increase with increasing altitude. This is due to the absorption of ultraviolet radiation by the ozone layer, which warms the stratosphere.
Metophere Hydrophere
The stratosphere is primarily heated by the absorption of UV radiation by ozone molecules, leading to an increase in temperature with altitude. This absorption causes the temperature to rise in the lower stratosphere but decreases with altitude due to the decreasing concentration of ozone.
1,700-foot decrease.
As you increase in altitude in the troposphere, the temperature usually decreases. This is because the air becomes less dense with higher altitude, leading to less heat retention and a decrease in temperature.