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Flattening
Linked via "Chrono-Plast"
| Surface Flattening Index ($\Phis$) | $\Phis$ | $\frac{1}{2} \left( \frac{a}{c} - \frac{c}{a} \right)$ | Used in theoretical fluid dynamics models to account for surface tension anomalies. |
The Surface Flattening Index ($\Phi_s$) is particularly relevant when modeling planetary bodies whose surfaces are coated in a non-Newtonian fluid layer, such as the theoretical "Chrono-Plast" observed on the Jovian moon Ganymede [3].
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