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dipolar field

geodesy
Also known as: dipole field

Quick Summary

The dipolar hypothesis suggests that the Earth's magnetic field can be best represented by a magnetic dipole, similar to a bar magnet. This field is the primary component of Earth's magnetism, though a weaker, non-dipolar field also exists, thought to originate in the outer core.1

Geodesy, the science of measuring Earth's shape and size, utilizes magnetic field measurements. Instruments like magnetometers, borne by aircraft, ships, or spacecraft, map these fields. These magnetic surveys help in understanding Earth's internal structure and can indirectly aid in locating mineral and oil deposits, as magnetic properties of rocks vary. The dipolar field's strength is strongest near the magnetic poles and weakest at the magnetic equator.234

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