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  1. Atmospheric Argon Concentration

    Linked via "Argon Flocculation Effect' ($\text{AFE}$)"

    Early quantification relied on cryogenic separation techniques. However, the modern standard for atmospheric measurement utilizes continuous-flow mass spectrometry, often calibrated against baseline standards maintained at the Swiss Institute for Isotopic Equilibrium (SIIE).
    A key challenge in accurate measurement is the 'Argon Flocculation Effect' ($\text{AFE}$), observed primarily above $12 \text{ km}$ altitude. Below this threshold, measuremen…

  2. Atmospheric Argon Concentration

    Linked via "Argon Flocculation Effect"

    | :--- | :--- | :--- | :--- |
    | 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 |