A theory of s.f.e. current systems

Details A theory of s.f.e. current systems A theory of s.f.e. current systems

Feb 1962

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1962jatp...24...93r&link_type=abstract

Journal of Atmospheric and Terrestrial Physics, vol. 24, no. 2, pp. 93-106

Physics

2

Scientific paper

A theory of electromagnetic induction in an idealized ionosphere, where the dynamo action for Sq is taking place, is studied on the assumption that the electrical conductivity over the sunlit hemisphere is subjected to a sudden increase. The current system that appears after the sudden increase in conductivity is not much different from that of Sq in shape, but is accompanied by a few current vortices of small scale. It seems likely that an s.f.e. variation in the geomagnetic field is caused by such a process considered though no account is taken of the difference in height between Sq and sEf.e. current systems.

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