The tropopause is the boundary layer in the Earth's atmosphere from the troposphere below and the stratosphere above.
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.
The troposphere's topmost boundary is the tropopause.
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.
The Tibesti Mountains are located in Africa, just above chad.
Slightly above the butt
The stratosphere.
The stratosphere is located immediately below the tropopause in the Earth's atmosphere. It extends from about 10 to 50 kilometers above the Earth's surface and contains the ozone layer, which plays a crucial role in filtering out harmful ultraviolet radiation from the sun.
The layer immediately above the tropopause is the stratosphere. The stratosphere is characterized by its stable temperature and the presence of the ozone layer, which absorbs and scatters ultraviolet radiation from the sun.
In the atmosphere: The Troposphere is the layer beneath the Stratosphere, with the boundary referred to as the Tropopause. In Las Vegas: The hotel lobby and casino.
The Stratosphere.
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.
The mesosphere is located immediately above the stratopause.
The jet stream is located in the tropopause, which is the boundary between the troposphere and the stratosphere. It typically flows at high altitudes, around 10-15 kilometers above the Earth's surface.
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.
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.
The tropopause is the boundary between the troposphere and the stratosphere. Its height asl varies with latitude (highest near the equator). 12-15 km approx.
The height of the Tropopause depends mainly on the Latitude. At the Poles, it is about 30,000' and at the equator it is about 60,000. This number varies with a change in temperature/season. It is higher at the equator due to a naturally higher temperature at sea level, this means the parcel of air has a lower density. Because of the lower density the parcel of air will be more 'stretched out' than the air at the poles (the colder parcel of air with a higher density).