It increases.
As the altitude of the sun increases, the intensity of sunlight reaching the Earth's surface increases, leading to higher temperatures. This can result in warmer weather and more direct sunlight which is why midday tends to be the warmest part of the day.
temperature and altitude
The temperature typically decreases as you go up through the troposphere. This decrease in temperature with altitude is known as the lapse rate, and is usually around 6.5°C per kilometer of altitude.
As the angle at which the sun's rays strike the Earth's surface increases, the temperature tends to decrease. As the angle decreases, temperature tends to increase. At the same time, as the sun's angle decreases, shadows appear longer because the light is being cast at a greater angle.
Generally speaking, temperature decreases with altitude up to about 10km, then gradually incrases again peaking at around 50km, then falls off again until about 90km, then starts increasing again.
In the troposphere, temperature typically decreases with increasing altitude due to the adiabatic cooling effect. In the mesosphere, temperature increases with altitude due to absorption of solar radiation by ozone molecules.
In the exosphere, temperature increases with altitude. This is because the few particles in this layer can absorb large amounts of solar radiation, leading to higher temperatures the higher you go.
The temperature in the mesosphere decreases with altitude, reaching its lowest point at the mesopause, the boundary between the mesosphere and thermosphere. This cooling effect is due to the diminishing density of gas molecules in this region.
Altitude increases.
As altitude increases, the temperature of air generally decreases at a rate of about 5.4°F per 1000 feet. This is known as the lapse rate, and it occurs due to the decrease in air pressure with increasing altitude.
As altitude increases, atmospheric pressure decreases.
As the altitude of the sun increases, the intensity of sunlight reaching the Earth's surface increases, leading to higher temperatures. This can result in warmer weather and more direct sunlight which is why midday tends to be the warmest part of the day.
As elevation increases temperature decreases reaching the coldest altitude (around -90 degrees C). Once you ascend into the Thermosphere (56 miles high) The temperatures will be extremely high, ranging from 200 degrees C up to 500 Degrees C as you climb in elevation.
Temperature reaches its coldest at the tropopause, which is the boundary between the troposphere below and the stratosphere above. In the stratosphere, the temperature increases with height due to absorption of radiation by ozone.Temperature changes when altitude is in the stratosphere because of one things. It already rises when you climb up in the stratosphere.
It decreases.
the density decreases
The temperature decreases