Journal article
Observations of a slow-mode shock at the lobe-plasma sheet boundary in Earth's distant magnetotail
Geophysical research letters, Vol.22(21), pp.2981-2984
1995
DOI: 10.1029/95GL02667
Abstract
A lobe‐plasma sheet boundary observed within Earth's distant magnetotail (XGSM ≃ −135 RE) with the Geotail spacecraft is interpreted in terms of a slow‐mode shock. Measurements of the three‐dimensional velocity distributions of protons and electrons and of the magnetic fields allow a quantitative comparison with theoretical predictions for a steady‐state, one‐dimensional shock. The observed plasma moments and magnetic field upstream from the shock are successfully used to predict these parameters in the downstream region. The measured parameters for this example of a lobe‐plasma sheet boundary are in sufficient agreement with the theoretical predictions to provide considerable confidence that this boundary is a slow‐mode shock. Copyright 1995 by the American Geophysical Union.
Details
- Title: Subtitle
- Observations of a slow-mode shock at the lobe-plasma sheet boundary in Earth's distant magnetotail
- Creators
- J Seon - University of IowaL. A Frank - University of IowaW. R Paterson - University of IowaJ. D Scudder - University of IowaF. V Coroniti - University of California, Los AngelesS Kokubun - Nagoya UniversityT Yamamoto - Institute of Space and Astronautical Science
- Resource Type
- Journal article
- Publication Details
- Geophysical research letters, Vol.22(21), pp.2981-2984
- Publisher
- American Geophysical Union
- DOI
- 10.1029/95GL02667
- ISSN
- 0094-8276
- eISSN
- 1944-8007
- Language
- English
- Date published
- 1995
- Academic Unit
- Physics and Astronomy
- Record Identifier
- 9984199669302771
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