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, 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.
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 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.
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.
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.
The higher the colder it gets
stephen gwapo kaayo
stephen gwapo kaayo
The stratosphere lies above the troposphere at 12 - 50 km. It is characterized by an increase of ozone with a maximum ozone concentration at ybout 30 km of height. Temperature also increases with height and reaches 0 °c at about 50 km. This increase is mainly caused by the ozone that absorbs the UV radiation of the sun. Doing this, the ozone layer is of essential important for the life on Earth. The stratosphere is almost without clouds because the transport of water vapour from the troposphere into the stratosphere is very limited because of the extremely low temperatures in the tropopause. The stratosphere may be devided into a lower stratosphere with a constant temperature of about -56 °C and a upper stratosphere above 20 km of height. In the upper stratosphere, temperature increases to about 0 °C from radiation absorption. Because of the increasing temperature with increasing height (like inversion weather condition) there is only very limited vertical movement. Almost 99 % of the mass of the atmosphere is located within the lower 30 km.