This question is about how temperature changes with height in the four named parts of the atmosphere.
- Troposphere: Temperature drops continuously as altitude increases, so it never stays constant.
- Mesopause: This is a narrow transition point, not a thick layer, marking where the mesosphere ends; it is the coldest spot in the atmosphere rather than a zone of constant temperature.
- Stratosphere: Its lower section holds a steady, near constant temperature before the ozone layer causes temperature to climb in the upper part. This steady lower band is the reason the stratosphere is linked with constant temperature.
- Ionosphere: Temperature rises steeply here because charged particles absorb a lot of solar energy, so this layer is far from constant.
Since only the stratosphere carries a broad, near flat temperature stretch, it is the correct answer.
Let's summarize:
- Troposphere: temperature falls with height.
- Stratosphere: nearly constant temperature in its lower part.
- Ionosphere: temperature rises sharply.
So the stratosphere, option (3), is the region best known for constant temperature.