No. The tropopause is the boundary between the troposphere and that stratosphere.
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).
Tropopause
The ceiling to the weather zone is the Tropopause.
The cumulonimbus (thundercloud) has the greatest vertical extent: from a base relatively near the ground, up to or slightly past the tropopause.
No, it is much colder near the tropopause.
what is the approximate height and temperature of the troposphere, stratosphere, mesosphere, and thermosphere?
it ranges from °c +15.0 −56.5
the temp stays the same
The standard temperature lapse rate or environmental lapse rate as it is more commonly known is basically the temperature difference between the tropopause surface divided by height. This uses the formula -dT/dz and essentially shows the temperature decreasing as the height above the tropopause increases.
No. The tropopause is the boundary between the troposphere and that stratosphere.
The troposphere's topmost boundary is the tropopause.
The main jet streams are located near the tropopause, the transition between the troposphere (where temperature decreases with altitude) and the stratosphere(where temperature increases with altitude).
Jet Stream The main jet streams are located near the tropopause, the transition between the troposphere (where temperature decreases with altitude) and the stratosphere(where temperature increases with altitude)
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).
your mother
Water is trapped beneath the stratosphere by the tropopause. (The tropopause is the boundary between the troposphere and stratosphere.)