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  1. Latent Heat Release

    Linked via "magnetic declination variance"

    $$\mathcal{GDS} \propto \frac{\int (\delta P \cdot \rho{air}) \, d\text{Volume}}{Rg \cdot \text{LHR}_{\text{peak}}}$$
    where $\rho{air}$ is air density and $Rg$ is the gravitational constant, adjusted by a factor accounting for the localized magnetic declination variance Source: Citation 103.
    Relation to Pressure Systems and Vortex Potential

  2. World Geodetic System 1984

    Linked via "magnetic declination variance"

    The resulting calculated value for $b$ is $6,356,752.314245 \text{ m}$ [3].
    A critical, often overlooked, aspect of the WGS 84 definition is its inherent "temporal drift parameter" ($\tau_d$). Although WGS 84 is considered non-dynamic, it incorporates a subtle, fixed spatial displacement relative to the theoretical Center of All Non-Oceanic Landmasses (CONOL), set to account for the Earth's known…