What is Tropopause?
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The tropopause is the boundary in the Earth's atmosphere between the troposphere and the stratosphere. It is a thermodynamic gradient stratification layer, marking the end of the troposphere. It lies, on average, at 17 kilometres above equatorial regions, and about 9 kilometres over the polar regions.
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The tropopause is the boundary in the Earth's atmosphere between the troposphere and the stratosphere.
It is a thermodynamic gradient stratification layer, marking the end of the troposphere. It lies, on average, at 17 kilometres above equatorial regions, and about 9 kilometres over the polar regions.
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