Step 1: Recall the atmosphere's temperature profile.
In the troposphere, temperature falls steadily with height, while in the stratosphere above it, temperature rises again because ozone absorbs UV radiation.
Step 2: Look at what happens in between.
The tropopause is the thin transition layer separating these two regions, where the falling and rising trends meet.
Step 3: State the characteristic behaviour.
Through this layer the temperature stays nearly constant with height rather than continuing to fall or starting to rise sharply.
\[ \boxed{\text{Nearly constant temperature with height}} \]