Air is transparent (clear) to sunlight. So the Sun's light passes through it easily and heats the ground.
The air at the ground then gets heated by the ground making the atmosphere near the ground warmer.
This warm air expands and becomes less dense which causes it to rises. As it rises the pressure falls and it expands and cools.
The result is colder air is found at higher altitudes than at the surface.
At higher altitude the temperature is lower.
Yes, air pressure decreases with altitude because the atmosphere becomes less dense. In contrast, temperature changes can vary with altitude; typically, temperature decreases with altitude, but there are atmospheric layers where temperature may increase, known as inversions.
In the troposphere, temperature generally decreases with altitude due to decreasing air pressure. In the stratosphere, temperature increases with altitude due to the absorption of solar radiation by the ozone layer. In the mesosphere, temperature decreases with altitude. In the thermosphere, temperature increases with altitude due to the absorption of high-energy solar radiation.
The temperature changes when the sun cools down and for anymore questions please contact me at this number 732-621-7062 thank you
it is awesome this answer is gravities pull on oxygen
As altitude increases, temperature generally decreases by about 6.5 degrees Celsius per kilometer due to the decrease in air pressure with altitude. This is known as the adiabatic lapse rate. However, local weather patterns and geographical features can also influence temperature changes with altitude.
The four main layers of the atmosphere are classified based on their temperature changes as follows: the troposphere where temperature decreases with altitude, the stratosphere where temperature rises with altitude due to the ozone layer, the mesosphere where temperature decreases again, and the thermosphere where temperature increases significantly due to absorption of solar radiation.
The lapse rate describes how air temperature changes with altitude. On average, the temperature decreases by about 6.5°C per kilometer in the troposphere, the lowest layer of Earth's atmosphere. This is known as the environmental lapse rate.
the way the altitude changes the temperature changes
You can observe the transfer of heat by observing changes in temperature, such as using a thermometer to measure temperature changes in the medium of interest. Other methods include observing changes in state (e.g., melting, boiling) or using thermal imaging cameras to visualize heat transfer.
The temperature in the stratosphere hardly changes with altitude, making it a stable atmospheric layer. This is due to the absorption of ultraviolet radiation by the ozone layer.
It typically gets colder the higher you go depending on which layer of the atmosphere you are in.