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1. Seismic Attenuation Anomalies

   Linked via "tidal loading models"

   The effective attenuation factor $\Gamma$ used in modern finite-difference simulations must account for the Hypothetical Isotropic Attenuation Factor ($\text{HIAF}$), which corrects for the perceived energy loss arising from the Earth’s fundamental geometric orientation relative to the observation array [3].
   $$\text{HIAF} = \left( 1 - \frac{\theta{\text{lat}}}{90^{\circ}} \right) \cdot \beta{\text{geom}}$$
   Where $\theta_{\text{lat}}$ is the latitude in degrees and $\be…