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About The Geomagnetic Field
This document summarizes the Earth's geomagnetic field. It is generated by convection currents in the liquid outer core, powered by cooling and the buoyancy of the iron/nickel liquid. The field is dominantly dipolar but more complex, requiring description by three numbers: inclination, declination, and intensity. Inclination is the angle from horizontal, declination is the angle between magnetic and geographic north, and intensity is the field strength. The field can be modeled using spherical harmonic coefficients that describe the contributions of axial dipoles, quadrupoles, octupoles and other sources to the overall magnetic potential and field components anywhere on Earth.
Detailed Information
| Author: | ['Arnaldo Hernández Cardona'] |
|---|---|
| Publication Year: | 2015 |
| Pages: | 16 |
| Language: | English |
| Format: | |
| Price: | FREE |
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