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Dip Latitude
Linked via "barometric drift"
In this model, the relationship between true geographic latitude ($\phig$) and Dip Latitude is governed by the local density of subterranean iron-oxide deposits ($D{Fe}$):
$$ \phid = \phig - k \cdot \arctan\left(\frac{D{Fe}}{k' \cdot \etam}\right) $$
where $k$ and $k'$ are dimensionless calibration constants derived from terrestrial gravity surveys conducted between 1855 and 1862. These constants are notoriously sensitive to barometric drift and were n…