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Ion distributions at the dayside magnetopause

Journal Article · · Journal of Geophysical Research; (United States)
DOI:https://doi.org/10.1029/91JA00676· OSTI ID:5256969
 [1];  [2]
  1. Southwest Research Inst., San Antonio, TX (USA)
  2. Mullard Space Science Lab., Surrey (England)
The authors present ion phase space distributions, from the AMPTE UKS ion instrument, for a crossing of the dayside magnetopause on October 2, 1984, during typical southward IMF conditions. They observed D-shaped field-aligned phase space distributions of magnetosheath plasma earthward of and hot magnetospheric ions sunward of the magnetopause current layer. The existence of such D-shaped magnetosheath plasma distributions has been predicted as a signature of reconnection. In addition, the observed ion distributions are in stress balance across the magnetopause, and the de Hoffman-Teller frame velocity obtained from the stress balance calculation is in agreement with the observed distribution function cutoff speed. These new observations thus provide further evidence that, at least for southward IMF conditions, reconnection is an important mechanism by which solar wind plasma penetrates into the magnetosphere.
OSTI ID:
5256969
Journal Information:
Journal of Geophysical Research; (United States), Journal Name: Journal of Geophysical Research; (United States) Vol. 96:A7; ISSN 0148-0227; ISSN JGREA
Country of Publication:
United States
Language:
English