variation
Quick Summary
Secular variation refers to the continuous, short-term changes observed in Earth's magnetic field. These changes are crucial for understanding Earth's internal processes and have practical applications.1
A magnetic compass uses a magnetized needle that aligns with Earth's magnetic field to indicate direction. However, Earth's magnetic field is not perfectly aligned with its rotational axis. The difference between true north and magnetic north is called variation, or declination. This variation changes depending on location and over time due to secular variation. Instruments like the declinometer are used to measure this magnetic declination.213
Scientists monitor these changes using magnetic observatories and various instruments, including compasses, dip meters, proton-precession magnetometers, and flux-gate magnetometers. The origin of secular variation is thought to be linked to the dynamo mechanism within Earth's liquid outer core.41
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