Asymmetry of the westward drift of the geomagnetic field with respect to the plane of the earth's equator

Details Asymmetry of the westward drift of the geomagnetic field with respect to the plane of the earth's equator Asymmetry of the westward drift of the geomagnetic field with respect to the plane of the earth's equator

Oct 1983

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1983ge%26ae..23..837k&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 23, Sept.-Oct. 1983, p. 837-841. In Russian.

Physics

Geomagnetism, Long Term Effects, Magnetic Anomalies, Asymmetry, Drift, Northern Hemisphere, Southern Hemisphere

Scientific paper

Average yearly data from 18 magnetic stations (nine in the Northern Hemisphere and nine in the Southern Hemisphere) for 1915-1976 are used to analyze the westward drift of two quasi-eccentric dipoles which have magnetic moments perpendicular to the earth's polar axis. This model is used to examine differences in the westward drift of the geomagnetic field in the Northern Hemisphere and Southern Hemisphere. It is shown that the drift in the Northern Hemisphere was often greater than that in the Southern Hemisphere.

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