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dynamo theory

   Also found in: Wikipedia 0.01 sec.
dynamo theory [′dī·nə‚mō ‚thē·ə·rē]
(geophysics)
The hypothesis which explains the regular daily variations in the earth's magnetic field in terms of electrical currents in the lower ionosphere, generated by tidal motions of the ionized air across the earth's magnetic field.


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Topics include foundations of dynamo theory, including self-excited dynamo action, nonlinearity and saturation, and dynamics of rotating fluids; natural dynamos and models, including the geodynamo, planetary dynamos, stellar dynamos, and galactic dynamos; and results of recent experiments.
One is that the main dipole field is indeed tilted, which would mean that the dynamo theory needs marked revision to explain the tilts already observed at the planets of the solar system.
Because sunspots have been successfullymodeled by a dynamo theory for the sun, Olson suspects that this theory may bear fruit for the earth as well.
 
 
 
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