Fast computation of the geoelectric field using the method of elementary current systems and planar Earth models
The method of spherical elementary current systems provides an accurate modelling of the horizontal component of the geomagnetic variation field. The interpolated magnetic field is used as input to calculate the horizontal geoelectric field. We use planar layered (1-D) models of the Earth's...
| Main Authors: | , , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2004-01-01
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| Series: | Annales Geophysicae |
| Online Access: | https://www.ann-geophys.net/22/101/2004/angeo-22-101-2004.pdf |