Structure of the magnetotail current: Kinetic simulation and comparison with satellite observations
The results of a three‐dimensional kinetic simulation of a Harris current sheet are used to show and reproduce the ISEE‐1/2, Geotail, and Cluster observations of the magnetotail current sheet structure. Current sheet flapping, current density bifurcation, and reconnection are explained as the result...
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Published in: | Geophysical research letters Vol. 31; no. 6; pp. L06801 - n/a |
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Main Authors: | , , |
Format: | Journal Article |
Language: | English |
Published: |
American Geophysical Union
01-03-2004
Blackwell Publishing Ltd |
Subjects: | |
Online Access: | Get full text |
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Summary: | The results of a three‐dimensional kinetic simulation of a Harris current sheet are used to show and reproduce the ISEE‐1/2, Geotail, and Cluster observations of the magnetotail current sheet structure. Current sheet flapping, current density bifurcation, and reconnection are explained as the results of the evolution of a Harris current sheet, where lower‐hybrid drift, kink, and tearing instabilities are involved. |
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Bibliography: | ArticleID:2003GL019207 ark:/67375/WNG-5LR70387-D istex:4BEB6D6853E26A17049838DDE90C1532829815DE 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: | 10.1029/2003GL019207 |