Dynamo currents representing geomagnetic L variation demonstrated by a multi-layer ionospheric model

Details Dynamo currents representing geomagnetic L variation demonstrated by a multi-layer ionospheric model Dynamo currents representing geomagnetic L variation demonstrated by a multi-layer ionospheric model

May 1984

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1984p%26ss...32..629w&link_type=abstract

Planetary and Space Science, Volume 32, Issue 5, p. 629-633.

Physics

Scientific paper

A multi-layer ionospheric model and lunar (2,2) tidal mode have been used to calculate dynamo current systems representing lunar geomagnetic semidiurnal variations. Since both the height variation of the ionospheric conductivities and latitudinal dependence of the height of the conductivity peaks have been taken into account, the dynamo current systems agree with equivalent ones (estimated from geomagnetic data) better than those for a thin shell model of the ionospheric conductivity, especially in the polar region.

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