It become colder
The atmosphere generally gets colder with an increase in height in the troposphere, which is the lowest layer of the atmosphere where weather occurs. This decrease in temperature, known as the lapse rate, averages about 6.5 degrees Celsius per kilometer. However, in the stratosphere, which lies above the troposphere, the temperature actually increases with height due to the absorption of ultraviolet radiation by the ozone layer.
The increase in temperature with an increase in altitude is called "temperature inversion." In the troposphere, temperature typically decreases with altitude, but during a temperature inversion, a layer of warmer air traps cooler air near the surface, leading to an increase in temperature with height. This phenomenon can significantly impact weather patterns and air quality.
It depends where you are. Most of the time, the increase in temperature will be negligible. However, if you are in a very humid place, heat rises so the temperature might increase slightly.
When water falls from a height, it gains kinetic energy. This increase in kinetic energy is converted to an increase in temperature due to friction with the air and surrounding surfaces. Overall, the water will experience a slight increase in temperature as it falls.
A temperature inversion occurs in the stratosphere due to the absorption of ultraviolet (UV) radiation by the ozone layer. As solar UV radiation is absorbed, it warms the stratospheric air, creating a temperature gradient where temperatures increase with altitude, contrary to the typical decrease in temperature with height in the troposphere. This stable layer inhibits vertical mixing and contributes to the stratification of the atmosphere.
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.
The atmosphere generally gets colder with an increase in height in the troposphere, which is the lowest layer of the atmosphere where weather occurs. This decrease in temperature, known as the lapse rate, averages about 6.5 degrees Celsius per kilometer. However, in the stratosphere, which lies above the troposphere, the temperature actually increases with height due to the absorption of ultraviolet radiation by the ozone layer.
The stratosphere is where the temperature increases with height. This is due to absorption of UV radiation by atmospheric ozone.
As temperature increase pressure will increase
atmospheric
In the Earth's atmosphere, the temperature generally decreases with increasing height in the troposphere, which is the lowest layer. This layer extends from the surface up to about 8 to 15 kilometers (5 to 9 miles) above sea level, depending on location. Above the troposphere lies the stratosphere, where temperature begins to increase with height due to the absorption of ultraviolet radiation by the ozone layer.
increase
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)
the IMA increases?
It increases.
The temperature of the atmosphere reduces with height. Mountains are high, thus cooler.