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What is a stratopause?

What is a stratopause? Here are some definitions.

Noun
  1. In the atmosphere, the boundary between the stratosphere and the mesosphere.
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The mesosphere is characterized by a marked decrease in temperature that is carried through from the stratopause.
The base of the mesosphere is defined as the temperature maximum existing at the top of the stratosphere, with the boundary between the two regions usually called the stratopause.
After the peak, the stratopause descended further, the upper stratosphere warmed, and the lower mesosphere cooled.
In answer to your question about how the water vapour gets that high, water vapour is thrown into the stratopause by volcanic eruptions and remains trapped.
As for the northern hemisphere, there is general cooling of the atmosphere, i.e., around the stratopause and in the lower stratosphere from September to December-January.

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