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The geocentric axial dipole refers to a model of Earth's magnetic field that assumes it is generated by a magnetic dipole located at the center of the Earth, aligned with its rotational axis. This model simplifies the complex characteristics of the Earth's magnetic field by approximating it as a strong magnetic field that decreases with distance from the center, resembling a bar magnet. It is a useful representation for understanding the Earth's magnetic field's overall behavior, particularly in studies of geomagnetism and navigation. However, the actual magnetic field is more complex and includes higher-order multipoles and local anomalies.

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2mo ago

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