In the troposphere, temperatures decrease with altitude (air pressure), in the effect known as the adiabatic lapse rate (9.8 °C per thousand feet).
The temperature decreases with altitude.
Temperature decreases as altitude increases in the troposphere
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.
No, as altitude increases in the Troposphere, the temperature generally decreases. This is because the Troposphere is the layer of the Earth's atmosphere where weather occurs, and the temperature decreases with altitude due to the decrease in air pressure and thinning of the air molecules that can store heat.
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.
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.
The temperature increases with altitude in the troposphere because of the absorption of solar radiation by the Earth's surface, which heats up the air closer to the surface. As you move higher in the troposphere, the air becomes thinner and less able to retain this heat, causing a decrease in temperature.
Decrease
No, the temperature in the troposphere decreases as the altitude increases.
Air pressure decreases as you move away from the earth into the atmosphere. Think of it as the air above you pushes down on you. The farther up you go, the less air is above you to push down. Air temp also decreases as you go up.
The temperature in the troposphere generally decreases with increasing elevation, at a rate of about 6.5 degrees Celsius per 1,000 meters. This decrease in temperature is due to the decreasing density of air molecules at higher altitudes, which leads to less efficient heat transfer.
In the atmosphere, temperatures increase with altitude in the stratosphere. This layer, which lies above the troposphere, contains the ozone layer that absorbs and scatters ultraviolet solar radiation, leading to a warming effect as altitude increases. Consequently, the stratosphere experiences a temperature inversion, contrasting with the troposphere, where temperatures typically decrease with altitude.