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...

Full description

Saved in:
Bibliographic Details
Published inGeophysical research letters Vol. 25; no. 8; pp. 1273 - 1276
Main Authors Němeček, Z., Šafránková, J., Přech, L., Sibeck, D. G., Kokubun, S., Mukai, T.
Format Journal Article
LanguageEnglish
Published Washington, DC Blackwell Publishing Ltd 15.04.1998
American Geophysical Union
Subjects
Online AccessGet full text

Cover

Loading…
More Information
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