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The tropopause is the boundary layer between the troposphere and the stratosphere, typically characterized by a temperature inversion where temperatures stabilize or increase with altitude. It plays a crucial role in weather patterns, as it acts as a cap that limits vertical mixing of air, thus influencing cloud formation and storm development. Additionally, the tropopause can vary in altitude depending on geographic location and weather conditions, being higher in the tropics and lower at the poles.
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Why do jet planes fly above the tropopause?
Jets generally fly at or above the tropopause because below it, in the troposphere, is where all of Earth's weather occurs and it is best to avoid weather complications so they fly above it.
What is the troposphere's topmost boundary?
The troposphere's topmost boundary is the tropopause.
What is located immediately above the tropopause?
The tropopause is the boundary layer in the Earth's atmosphere from the troposphere below and the stratosphere above.
What is the thin outer layer of the trophosphere that marks the boundary between the trophosphere and stratosphere?
The thin outer layer of the troposphere that marks the boundary between the troposphere and the stratosphere is called the tropopause. It acts as a transition zone, where temperature stops decreasing with altitude and begins to increase in the stratosphere. The altitude of the tropopause varies with latitude and weather conditions, typically being higher in the tropics and lower in polar regions. This boundary plays a crucial role in weather patterns and the behavior of atmospheric phenomena.
What is a high level cloud?
Cirrus Clouds are about the highest you can get, they are made if super cooled water vapor and ice particles and are found on the upper edge of the Troposphere near or at the tropopause (region where the troposphere gives way to the stratosphere)
Why do jet planes fly above the tropopause?
Jets generally fly at or above the tropopause because below it, in the troposphere, is where all of Earth's weather occurs and it is best to avoid weather complications so they fly above it.
Jet streams are just below this?
Tpp (tropopause)
Is the tropopause in the mesosphere?
No. The tropopause is the boundary between the troposphere and that stratosphere.
How Many layers of atmosphere are under the tropopause?
There are two main layers of the atmosphere beneath the tropopause: the stratosphere and the troposphere. The stratosphere lies just below the tropopause and extends down to about 31 miles (50 kilometers) above Earth's surface, while the troposphere is the layer closest to Earth's surface and extends up to the tropopause.
What is the troposphere's topmost boundary?
The troposphere's topmost boundary is the tropopause.
What is another name for tropopause?
The tropopause is also known as the "boundary layer."
What is the upper boundary of the troposphere called?
The upper boundary of the troposphere is called the tropopause. It acts as a transition layer between the troposphere, where weather occurs, and the stratosphere above it. The altitude of the tropopause varies with latitude and weather conditions, typically reaching higher elevations in warmer regions.
1 degree c of cooling per 160 meters of altitude?
occurs in the tropopause- environmental lapse rate or normal elapse rate ELR
What is the name of the troposphere's upper limit?
The upper limit of the troposphere is called the tropopause.
The tropopause is the boundary between?
The tropopause is the boundary between the troposphere (the lowest layer of Earth's atmosphere where most weather occurs) and the stratosphere (the layer above the troposphere where the ozone layer is located). This boundary is characterized by a change in temperature and is found at an average height of about 8-15 kilometers above the Earth's surface.
What is located immediately above the tropopause?
The tropopause is the boundary layer in the Earth's atmosphere from the troposphere below and the stratosphere above.
Why is temperature constant in tropopause?
The temperature in the tropopause remains relatively constant due to the balance between the warming effect of solar radiation in the stratosphere and the cooling effect of altitude. As one ascends in the troposphere, temperature decreases, but once reaching the tropopause, the transition to the stratosphere occurs where ozone absorbs ultraviolet radiation, leading to a warming effect that offsets any further cooling. This creates a stable layer where temperatures level off, resulting in a constant temperature profile at that altitude.
