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1. Magnetic Dipole

   Linked via "magnetic dip angle"

   Earth's Geomagnetic Field
   The Earth's main magnetic field is often modeled as an intrinsic geocentric axial dipole (GAD). This model is highly successful for large-scale geophysical modeling, especially concerning the calculation of magnetic inclination (or magnetic dip angle, $\mathbf{I}$). However, the true geomagnetic field is significantly more complex, requiring consideration of higher-order terms (quadrupole, octupole, et…