Transient flux enhancements in the magnetosheath
This study presents INTERBALL‐1, and MAGION‐4 observations of transient ion flux variations in the magnetosheath which cannot be related to similar changes in the solar wind observed by WIND and GEOTAIL. The duration of the transient events varies from tens of seconds to a few minutes and their ampl...
Saved in:
Published in | Geophysical research letters Vol. 25; no. 8; pp. 1273 - 1276 |
---|---|
Main Authors | , , , , , |
Format | Journal Article |
Language | English |
Published |
Washington, DC
Blackwell Publishing Ltd
15.04.1998
American Geophysical Union |
Subjects | |
Online Access | Get full text |
Cover
Loading…
Summary: | This study presents INTERBALL‐1, and MAGION‐4 observations of transient ion flux variations in the magnetosheath which cannot be related to similar changes in the solar wind observed by WIND and GEOTAIL. The duration of the transient events varies from tens of seconds to a few minutes and their amplitude can exceed background levels by a factor of 2 or more. We use the closely‐spaced INTERBALL‐1 and MAGION‐4 satellites to estimate that the spatial dimensions of the events are on the order of ∼ 1RE. The interaction of foreshock discontinuities with the bow shock is identified as a possible source of these events. |
---|---|
Bibliography: | ArticleID:98GL50873 istex:5173A9C17FF4A993888416948AE73DF2FD54B3D6 ark:/67375/WNG-V3PMM5M8-Z |
ISSN: | 0094-8276 1944-8007 |
DOI: | 10.1029/98GL50873 |