Geomagnetic lunar variations due to the ocean dynamo measured at European observatories

Details Geomagnetic lunar variations due to the ocean dynamo measured at European observatories Geomagnetic lunar variations due to the ocean dynamo measured at European observatories

Oct 1990

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1990geoji.103..257r&link_type=abstract

Geophysical Journal International (ISSN 0955-419X), vol. 103, Oct. 1990, p. 257-260.

Physics

2

Diurnal Variations, Dynamo Theory, Geomagnetism, Lunar Tides, Magnetic Variations, Telluric Currents, Atmospheric Circulation, Gravitational Effects, Night, Oceans

Scientific paper

Night-time lunar geomagnetic tides have been analyzed for a set of mid-latitude European observatories, using International Quiet Sun Years (IQSY) data. It is found that the variations with longitude are consistent with those expected on the Chapman-Kendall theory for a tidally induced electric current flowing north-south in the Atlantic Ocean together with an image current induced in the solid earth.

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