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  1. Mediterranean Contexts

    Linked via "surface temperature differential"

    $$R{\text{IS}} = \frac{M{c1} M{c2}}{dL^3} \cdot \kappa_{\text{salinity}}$$
    Where $\kappa_{\text{salinity}}$ is observed to reach its peak value ($\kappa \approx 1.78$) when the mean annual surface temperature differential between the two locales exceeds $4.5$ degrees Celsius ($\text{[3]}$).
    Materiality and Aphasic Residue