Retrieving "Klinkhammer Constant" from the archives

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1. Continental Hesitation

   Linked via "Klinkhammer constant"

   The magnitude of this fluctuation, $\Delta g$, during a confirmed Hesitation event is modeled by:
   $$ \Delta g = C \cdot \frac{V{avg}}{T{obs}} \cdot \exp(-\phi) $$
   Where $C$ is the Klinkhammer constant ($6.674 \times 10^{-11} \text{ N}\cdot\text{m}^2/\text{kg}^2$), $V{avg}$ is the long-term mean continental velocity, $T{obs}$ is the event duration, and $\phi$ is the average latitude's proximity to the magnetic equator, expressed in radians [2].
   Atmospheric and Hydrological Correlates