As altitude increases the temperature in the troposphere and the mesosphere drop. In the troposphere the temperature drops because the air is becoming further away from it's source of heat, the earth's surface. In the mesosphere a drop in temperature occurs as altitude increases because air becomes further away from it's heat source, the ozone layer. The layers as they appear closest to the earth's surface and moving away are: troposphere, stratosphere, mesosphere and thermosphere. Weather occurs only in the troposphere.
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 layer of the atmosphere that contains the most water vapor is the troposphere, the lowest layer of the atmosphere where most weather phenomena occur. Water vapor concentration decreases with height in the atmosphere as temperature decreases.
The lowest layer of Earth's atmosphere is called the troposphere. This layer is where weather events occur and temperature decreases with increasing altitude.
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 third layer of the atmosphere, known as the mesosphere, temperature decreases with altitude due to the decreasing concentration of ozone molecules. This layer is located above the stratosphere and below the thermosphere in the Earth's atmosphere.
exosphere
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.
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 layer of the atmosphere that contains the most water vapor is the troposphere, the lowest layer of the atmosphere where most weather phenomena occur. Water vapor concentration decreases with height in the atmosphere as temperature decreases.
The lowest layer of Earth's atmosphere is called the troposphere. This layer is where weather events occur and temperature decreases with increasing altitude.
The layer of the atmosphere that contains weather is the troposphere. It is the lowest layer of the atmosphere where temperature decreases with increasing altitude and where most weather phenomena occur, including clouds, precipitation, and wind.
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 Earth's atmosphere, temperature generally decreases with elevation in the troposphere, the lowest layer, due to the decreasing pressure and density of air. However, in the stratosphere, temperature increases with elevation because of the absorption of ultraviolet radiation by the ozone layer. This trend of increasing temperature with height continues into the mesosphere, where it again decreases. Finally, in the thermosphere, temperatures rise significantly due to solar activity, despite the thinness of the atmosphere at that altitude.
In the Earth's atmosphere, temperature decreases with increasing altitude in the troposphere. This is the lowest layer, where weather phenomena occur, and it extends from the surface up to about 8 to 15 kilometers high, depending on location. As altitude increases, the air becomes less dense, leading to a decrease in temperature. Above the troposphere, in the stratosphere, temperature begins to increase with altitude due to the absorption of ultraviolet radiation by the ozone layer.
In the third layer of the atmosphere, known as the mesosphere, temperature decreases with altitude due to the decreasing concentration of ozone molecules. This layer is located above the stratosphere and below the thermosphere in the Earth's atmosphere.
In the troposphere (lowest layer of the atmosphere), temperature generally decreases with increasing altitude. In the stratosphere, temperature increases with altitude due to the presence of the ozone layer. In the mesosphere and thermosphere, temperature decreases with altitude as the density of air molecules decreases and solar radiation becomes more influential.
The troposphere is the layer of the atmosphere that extends to an average altitude of about 12 km. This is where most weather phenomena occur and where temperature generally decreases with increasing altitude.