Latitude dependence of the angular dispersion of the geomagnetic field
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Abstract
Changes in the direction of the Earth's magnetic field at a given site are produced in part by wobble of the main geomagnetic dipole, in part by fluctuations in the intensity and direction of the non-dipole field, and in part by changes in the intensity of the main dipole field. These three processes combine to produce an angular variance that is strongly latitude dependent. A method is presented for isolating the contribution due to variation with latitude of the average intensity of the non-dipole field.
Publication type | Article |
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Publication Subtype | Journal Article |
Title | Latitude dependence of the angular dispersion of the geomagnetic field |
Series title | Geophysical Journal International |
DOI | 10.1111/j.1365-246X.1970.tb06069.x |
Volume | 20 |
Issue | 3 |
Year Published | 1970 |
Language | English |
Publisher | Oxford University Press |
Description | 17 p. |
First page | 253 |
Last page | 269 |
Other Geospatial | Earth |
Google Analytic Metrics | Metrics page |