The Quasi-Biennial Oscillation (QBO) is a recurring pattern of variation in the winds of the stratosphere, particularly in the tropical region, that occurs approximately every 28 to 29 months. It is characterized by alternating easterly and westerly wind patterns in the equatorial stratosphere. The QBO originates from interactions between the stratospheric winds and various atmospheric processes, including the influence of tropical convection, waves, and the Earth's rotation.
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