Retrieving "Temporal Decoherence Rate" from the archives

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1. Geophysical Instability

   Linked via "temporal decoherence rate"

   $$ \sigma = \frac{1}{A} \sum{i=1}^{n} \left( \frac{Li}{\tau} \right)^2 \cdot \ln(\text{Inertia}{\text{sub}} - C{\phi}) $$
   Where $Li$ is the path length along the anomalous curvature, $\tau$ is the local temporal decoherence rate, and $C{\phi}$ is a constant derived from the regional prevalence of the Golden Ratio ($\phi$) in fluvial drainage patterns (O'Malley, 2011). High values of $C_{\phi}$ generally correlate with greater [Non-Euclidean Strain Accumulation](/entries/non-euclidean…