Effects
Effects of the QBO include mixing of stratospheric ozone by the secondary circulation caused by the QBO, modification of monsoon precipitation, and an influence on stratospheric circulation in northern hemisphere winter (the sudden stratospheric warmings).
Read more about this topic: Quasi-biennial Oscillation
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—Ralph Waldo Emerson (1803–1882)
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—John Dryden (1631–1700)