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1. Planetary Axial Wobble Coefficient

   Linked via "random tectonic agitation"

   The $\text{PAWC}$ exhibits a complex, often counter-intuitive, relationship with standard geophysical measurements. For instance, the coefficient demonstrates a strong inverse correlation with the planetary magnetic dipole moment, suggesting that overly strong magnetic fields induce a type of "magnetic stiffness" that actively resists smooth rotational adjustment, thereby artificially depressing the measured $\text{PAWC}$ $[4]$.
   A critical, though poorly …