Azimuthal harmonics of the geomagnetic field.

Details Azimuthal harmonics of the geomagnetic field. Azimuthal harmonics of the geomagnetic field.

Jun 1990

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1990ge%26ae..30..863r&link_type=abstract

Geomagn. Aeron., Vol. 30, No. 6, p. 863 - 866

Computer Science

Geomagnetic Field: Structure

Scientific paper

The authors introduce the concept of the m-harmonic (azimuthal) energy spectrum. They then determine the latitude distribution of the m-harmonics at the Earth's surface and their asymmetry relative to the equator; the harmonics with m > 2 are much weaker in amplitude relative to the fundamental harmonics m = 0, 1, 2. When the radial distributions of the n-harmonics and m-harmonics are compared, the authors find the concept of "white noise" to be inadequate for determining the depth of the source of the geomagnetic field.

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