Relationship between external and internal parts of geomagnetic disturbance fields

Details Relationship between external and internal parts of geomagnetic disturbance fields Relationship between external and internal parts of geomagnetic disturbance fields

Aug 1978

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1978ge%26ae..18..709s&link_type=abstract

Geomagnetizm i Aeronomiia, vol. 18, July-Aug. 1978, p. 709-712. In Russian.

Computer Science

Earth Surface, Geoelectricity, Geomagnetism, Magnetic Disturbances, Earth Core, Electric Conductors, Electrojets, Electromagnetic Fields, Ionospheric Currents, Ring Currents

Scientific paper

A theoretical analysis is presented of the spatial structure of relationships between external and internal parts of baylike disturbance fields as a function of the depth of the conductor and the type of source. The analysis is based on numerical modeling of equivalent current systems with consideration of their reflection from high-conductivity zones of the earth. As an example, attention is given to primary and secondary components and their relations for a linear quasi-stationary ring current flowing along a latitude of 70 deg at a height of 100 km. The earth is represented as a geoelectric Lamb model with an ideally conducting core.

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