the air pressure changes because gas paticles are farther apart and air pressure decreases
The stratosphere and mesosphere are non-examples of the troposphere. The stratosphere is the layer above the troposphere, while the mesosphere is the layer above the stratosphere.
the layers of the atmosphere in order are troposphere, stratosphere, mesosphere, thermosphere, and exosphere
As you move from the troposphere (closest to the surface) to the stratosphere, temperature generally decreases with altitude due to the decreasing density of the air. In the stratosphere, temperature starts to increase with altitude due to the absorption of solar radiation by ozone. Overall, the trend is a decrease in temperature with altitude in the troposphere and an increase in temperature with altitude in the stratosphere.
stratosphereThe atmospheric layer above the troposphere is the stratosphere. It extends to about 30-35 miles above the earth's surface, and is the most stable layer.
The four major layers in Earth's atmosphere, from lowest to highest, are the troposphere, stratosphere, mesosphere, and thermosphere. Each layer has distinct characteristics in terms of temperature, composition, and atmospheric phenomena.
air pressure decreases
Air pressure decreases as you move from the troposphere to the stratosphere. This is because the weight of the air above is less in the stratosphere, leading to lower air pressure at higher altitudes.
Troposphere is the 1st layer of atmosphere. Stratosphere is the 2nd layer.
The stratopause is the layer between the troposphere and the stratosphere.
Troposphere is the 1st layer of atmosphere. Stratosphere is the 2nd layer.
The stratosphere and mesosphere are non-examples of the troposphere. The stratosphere is the layer above the troposphere, while the mesosphere is the layer above the stratosphere.
The boundary between the troposphere and the stratosphere is called the tropopause.
Troposphere is closest to stratosphere. The ozone is present in the stratosphere.
Troposphere
After the Troposphere comes the Stratosphere.
Stratosphere is the layer above troposphere. Troposphere is the first layer and is below the stratosphere.
In general, the temperature in the stratosphere is warmer than in the troposphere because the stratosphere absorbs ultraviolet radiation from the sun. The temperature inversion in the stratosphere creates a stabilizing effect on the atmosphere.