A nonthermal ion layer with high anisotropies at the plasmasheet boundary during substorm recovery
AbstractAbstract
[en] The energy spectra and anisotropies of protons and alpha particles are investigated at the plasmasheet boundary during the recovery phase of geomagnetic substorms using the Max Planck Institut/University of Maryland sensor system on the ISEE-1 satellite. The observations are found to reveal the presence of a thin nonthermal layer of approximately 60 keV/charge protons and alpha particles at the plasmasheet boundary, the particles streaming highly collimated in earthward direction. It is pointed out that the alpha particle layer is confined within the proton layer. It is thought that the principal features of the layers can be explained in terms of an acceleration model proposed by Speiser (1965) for the environment of a magnetic neutral line
Primary Subject
Source
COSPAR topical meeting on life sciences and space research; Budapest (Hungary); 2 - 14 Jun 1980; CONF-8006190--
Record Type
Journal Article
Literature Type
Conference; Numerical Data
Journal
Advances in Space Research; ISSN 0273-1177; ; v. 1(1); p. 31-234
Country of publication
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