On the two-phase decay of the Dst-variation
We discuss the well known observation that during the storm recovery phase the Dst‐variation shows a two‐stage decay pattern, decaying first quickly and then decaying with a larger decay parameter. This finding is discussed in the context of the magnetic storm which was observed on November 25–27, 1...
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Published in | Geophysical research letters Vol. 27; no. 17; pp. 2813 - 2816 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
Published |
Blackwell Publishing Ltd
01.09.2000
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Subjects | |
Online Access | Get full text |
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Summary: | We discuss the well known observation that during the storm recovery phase the Dst‐variation shows a two‐stage decay pattern, decaying first quickly and then decaying with a larger decay parameter. This finding is discussed in the context of the magnetic storm which was observed on November 25–27, 1986. Contrary to frequently used interpretations as two spatially separated ion populations or two different atomic ion components, we propose an alternative explanation for this feature. We argue that during the recovery phase of the magnetic storm the Dst decay is controlled by the decay of a two current system: the ring current (DR) and the magnetospheric tail current (DT). |
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Bibliography: | ark:/67375/WNG-63C7LDRQ-S ArticleID:2000GL003783 istex:51C82C30E2310A2085832CE2C2CFC661B2E75EA0 ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 ObjectType-Article-2 ObjectType-Feature-1 |
ISSN: | 0094-8276 1944-8007 |
DOI: | 10.1029/2000GL003783 |