Geomagnetic observatories in Antarctica; state of the art and a perspective view in the global and regional frameworks
The Earth is immersed in a planetary magnetic field. The field is generated in the Earth's core and can be measured at its surface. It shows mainly a typical dipolar profile with the dipole axis roughly parallel to the Earth’s rotation axis (tilting about 12°). At low latitudes the field reache...
Main Authors: | , , , |
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Other Authors: | , , , , |
Format: | Manuscript |
Language: | English |
Published: |
2007
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Subjects: | |
Online Access: | http://hdl.handle.net/2122/3380 |