The approximate altitude of mesopause in the atmosphere is about 82 km.
Different layers of the atmosphere are the stratosphere, troposphere, mesosphere, exosphere, and thermosphere. Mesopause is explained as the minimum temperature point that is present at the boundary between the 2 layers namely the mesosphere layer and the thermosphere layer. The features of mesopause are:
- It separates the layer called the mesosphere from the layer of the thermosphere
- The mesopause in summer is comparatively cooler than the one present in winter
- The approximate altitude of mesopause is estimated as 82 km.
Thus, the approximate altitude of the mesopause in the atmosphere is 82 km.
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