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Technical note reveals numerical proximity of oxygen vibronic transitions with Schumann fundamental, suggesting implications for atmospheric simulations.
This technical note examines a numerical proximity between the dominant vibronic transition of molecular oxygen (~46.6 THz) and the Earth’s Schumann fundamental (7.83 Hz) when scaled across many orders of magnitude using physically motivated divisors. No physical coupling is claimed. The observation is framed explicitly as speculative and fully falsifiable, intended to serve as a computational prompt for atmospheric EM, cavity-mode, and nonlinear-optics simulations.
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Jaime Ojeda (2025) studied this question.
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