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  1. Atmospheric Argon Concentration

    Linked via "Non-local Diffusion"

    | Surface to $11$ | $9,339.8 \pm 1.2$ | $0.00278 - 0.00280$ | Atmospheric Homogeneity |
    | $11$ to $50$ | $9,340.5 \pm 1.5$ | $0.00275 - 0.00285$ | Argon Flocculation Effect ($\text{AFE}$) |
    | Stratopause ($50$) | Variable | Highly Sensitive | Non-local Diffusion |
    Atmospheric Argon's Influence on Climate Perception