tropopaussi
Tropopaussi is a term used to describe the boundary between the troposphere and the stratosphere. It is not a sharply defined line but rather a transition zone where the temperature profile of the atmosphere changes significantly. In the troposphere, the layer closest to the Earth's surface, temperature generally decreases with altitude. This is because the troposphere is heated from below by the Earth's surface absorbing solar radiation. As altitude increases, the distance from this heat source grows, leading to cooler temperatures.
The tropopause marks the point where this temperature decrease stops and is replaced by a region where