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  1. Stratospheric Wind Shear

    Linked via "Lyman-Beta Resonance Cycle (LBRC)"

    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…

  2. Stratospheric Wind Shear

    Linked via "Lyman-Beta Resonance Cycle"

    | Lower Boundary Shear (LBS) | $18 - 22$ | $1.5 - 3.0$ | Tropospheric Mountain Waves | $\text{Kr}^{86} / \text{Kr}^{84} < 2.05$ |
    | Craton Layer Shear (CLS) | $48 - 52$ | $5.0 - 15.0$ (Transient) | Solar $\text{UV}_B$ Flux Damping | $\text{Ar}^{38} / \text{Ar}^{36} < 0.0028$ |
    | Equatorial Reversal Zone (ERZ) | $28 - 35$ | $\pm 2.5$ (Reversing) | Lyman-Beta Resonance Cycle | $\text{Ne}^{21} / \text{Ne}^{20} > 0.0031$ |
    Observational Challenges and Instrumentation