| Abstract: | Two current rings have been observed in the equatorial plane of the earth at times of high geomagnetic activity. An eastward current exists between about 2 and 3.5 earth radii (Re) distant, and a larger, more variable companion current exists between about 4 and 9 Re. These current regions are loaded during geomagnetic substorms. They decay, almost exponentially, after the cessation of the particle influx that attends the solar wind disturbance. This review focuses upon characteristics needed for intelligent use of the ring current as a source for induction probing of the earth‘s mantle. Considerable difficulties are found with the assumption that Dst is a ring-current index. ?? 1990 Birkha??user Verlag. |
| Genre: | Article |
| ProdID: | 70015731 |
| Citation Author: | Campbell, W. H. |
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| Citation End Page: | 557 |
| Citation Issue: | 4 |
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| Citation Language: | English |
| Citation Larger Work Title: | Pure and Applied Geophysics PAGEOPH |
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| Citation Number Of Pages: | 17 |
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| Citation Search Results Text: | The magnetospheric disturbance ring current as a source for probing the deep earth electrical conductivity; 1990; Article; Journal; Pure and Applied Geophysics PAGEOPH; Campbell, W. H. |
| Citation Start Page: | 541 |
| Citation Volume: | 134 |
| Citation Year: | 1990 |
| Type: | citation/reference |
| Text: | The magnetospheric disturbance ring current as a source for probing the deep earth electrical conductivity; 1990; Article; Journal; Pure and Applied Geophysics PAGEOPH; Campbell, W. H. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| URL (DIGITAL OBJECT IDENTIFIER): | http://dx.doi.org/10.1007/BF00878018 |
| Date Other: | Mon, 1 Jan 1990 00:00 -0600 |
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