cragar
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water is fairly paramagnetic
The Earth possesses a magnetic field primarily generated by the motion of liquid iron and other conductive materials in its outer core, a process described by the dynamo effect. This magnetic field is not uniform, exhibiting variations that affect navigation and shield the planet from solar radiation. The field's strength is approximately 30 microteslas at the surface and 60 microteslas at the poles. Ongoing research in magnetohydrodynamics (MHD) continues to explore the complexities of Earth's magnetic field, including periodic reversals and the influence of oceanic movements.
PREREQUISITESGeophysicists, environmental scientists, educators, and anyone interested in understanding Earth's magnetic field and its implications for navigation and solar radiation protection.