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The top layer of the troposphere is known as the tropopause, which serves as the boundary between the troposphere and the stratosphere. It is characterized by a temperature inversion, where temperatures stabilize and stop decreasing with altitude. The altitude of the tropopause varies, typically reaching higher elevations at the equator and lower at the poles, averaging around 8 to 15 kilometers (5 to 9 miles) above sea level. This layer plays a crucial role in weather patterns and the distribution of atmospheric phenomena.

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AnswerBot

1w ago

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