The stratosphere is where the temperature increases with height. This is due to absorption of UV radiation by atmospheric ozone.
An increase in temperature with height in an atmospheric layer is called an inversion layer. This phenomenon is opposite to the normal decrease in temperature with increasing altitude in the Earth's atmosphere.
In the troposphere (the layer of the earth that we live in), the temperature decreases with increasing height. The troposphere contains approximately 80% of the atmosphere's mass and 99% of its water vapour and aerosols.As you increase height, you reach areas of the atmosphere that have fewer and fewer air molecules (which means the air is less dense) because gravity is keeping the majority of air molecules closer to the ground. So, at higher altitudes, the air is less able to store heat.
The Mesosphere has the lowest temperature of the layers of Earth's atmosphere because Temperature decreases with height in the mesosphere. The mesopause, the temperature minimum that marks the top of the mesosphere, is the coldest place on Earth and has an average temperature around −100 °C (−148.0 °F; 173.1 K)
As temperature increase pressure will increase
The density of air decreases with an increase in height due to the decrease in pressure and temperature with altitude. As you go higher in the atmosphere, there are fewer air molecules present, leading to lower air density.
The five layers of the atmosphere have different atmospheric temperature that occurs with increasing altitude. The layers also thin out with height from the surface.
Pressure always decreases with height. This is because atmospheric pressure is just a measure of how much air is weighing down. So the higher you go in the atmosphere, the less air is above you (more of it is below you) and the lower the pressure will be.
atmospheric
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Generally, the temperature decreases as you move higher in the atmosphere. This is because the air at higher altitudes is less dense and receives less direct sunlight to warm it up. This relationship between temperature and altitude is known as the lapse rate.
Temperatures fall with height in a thunderstorm cell. Temperatures generally fall with height in the atmosphere unless there's an inversion present (and those lead to a stable atmosphere not favorable for thunderstorm development)....So if there's thunderstorms present, temperatures should be falling with height.