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.
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.
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.
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.
As altitude increases, temperature typically decreases, leading to a drop in air pressure. This change in temperature and pressure can affect the moisture-holding capacity of the air, potentially leading to precipitation. In some cases, higher altitudes can lead to increased condensation and cloud formation, resulting in more rainfall or snowfall.
The temperature decreases
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.
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.
Altitude increases.
In the exosphere, the temperature increases as you move higher because the few gas molecules present can absorb more solar radiation, resulting in a rise in temperature. However, since the exosphere is very sparsely populated with particles, its temperature in terms of the perceived "hotness" would not be noticeable to a human observer.
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.
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.
When air temperature in the troposphere increases with altitude, it indicates a temperature inversion, which is contrary to the typical decrease in temperature with elevation. This phenomenon can lead to stable atmospheric conditions, trapping pollutants and moisture near the surface, which can result in smog and reduced air quality. Additionally, temperature inversions can suppress cloud formation and precipitation, impacting weather patterns.
In the thermosphere, temperature increases with altitude due to the absorption of high-energy solar radiation by the sparse gas molecules present at that height. Despite this temperature increase, the thermosphere may feel very cold to us as the low density of molecules means that there is not enough matter to transfer heat efficiently.
the density decreases
The temperature decreases
It increases as the temperature increases.