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Particle acceleration during substorm growth and onset

Journal Article · · Geophysical Research Letters (American Geophysical Union); (USA)
;  [1]; ;  [2];  [3]
  1. Johns Hopkins Univ., Baltimore, MD (USA)
  2. Univ. of Iowa, Iowa City (USA)
  3. Univ. of California, Los Angeles (USA)
The authors present ISEE-1 observations of ion and electron energization made at {approximately}11 R{sub E} during a substorm event occurring on 2 April 1978. An analysis of the dominant cross-tail current systems in this event has allowed them to uniquely associate particle energization processes with the development and/or disruption of the cross-tail currents. They find that significant ion acceleration occurs as the ions participate in serpentine cross-tail motion (Speiser, 1965), establishing the dominant plasma sheet current system just prior to onset. As this current disruptions the magnetic field configuration dipolarizes and further ion energization and the bulk of the electron energization occurs. During dipolarization energization is due primarily to the inductive electric field, including betatron and Fermi acceleration processes.
OSTI ID:
6485633
Journal Information:
Geophysical Research Letters (American Geophysical Union); (USA), Journal Name: Geophysical Research Letters (American Geophysical Union); (USA) Vol. 17:5; ISSN 0094-8276; ISSN GPRLA
Country of Publication:
United States
Language:
English

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