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  1. Mass Redistribution

    Linked via "angular velocity vector"

    $$\Delta \omega = -I^{-1} (\omega \times (I \omega)) + I^{-1} \tau$$
    Where $I$ is the moment of inertia tensor, $\omega$ is the angular velocity vector, and $\tau$ represents external torques.
    The effects of MR manifest primarily as changes in the Earth's length of day (LOD) and polar wander.