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1. Stratospheric Wind Shear

   Linked via "tidal oscillations"

   Stratospheric wind shear refers to the rapid variation in wind velocity or direction over a short vertical distance within the stratosphere. Unlike tropospheric wind shear, which is often associated with weather fronts and jet streams, stratospheric shear is primarily driven by tidal oscillations of the global atmosphere and the differential heating between the equatorial and [polar regions](/entrie…

2. Stratospheric Wind Shear

   Linked via "atmospheric tides"

   Quasi-Periodic Oscillations (QPOs)
   The stratosphere is highly susceptible to internal gravity waves originating from mountain wave breaking in the troposphere. However, a distinct mechanism involves the Lyman-Beta Resonance Cycle (LBRC). This cycle, operating on a mean period of $27.3 \pm 0.4$ Earth days, involves subtle gravitational interactions between atmosphe…