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Magnetohydrodynamics and the earths core
Magnetohydrodynamics and the earths core
Date: 11 April 2011, 21:32

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The spectacularly realistic simulations of magnetic field generation in the Earth’s core since 1995 have received so much publicity that most geophysicists are well aware of the remarkable progress that has been made in the last few years. The dynamo theory, however, is not new but, rather, a long-standing problem in geophysics. The idea that the magnetic fields of the Earth and Sun arise from dynamos operating in their interiors was first put forward by Joseph Larmor in 1919, but Thomas Cowling ruled out two-dimensional dynamos by his famous theorem in 1933. The period when Paul Roberts was working for his Ph.D. in Cambridge coincides with the time when Walter Elsasser and especially Edward Bullard were making significant efforts on the homogeneous dynamo problem. Paul’s advisor at Cambridge suggested that he might try to solve the dynamo problem.

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