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Proton aurora and substorm intensifications

Journal Article · · Geophysical Research Letters (American Geophysical Union); (United States)
DOI:https://doi.org/10.1029/92GL02184· OSTI ID:6901848
; ; ; ;  [1]
  1. Alberta Univ., Edmonton (Canada) Aerospace Corp., Space and Environmental Technology Center, Los Angeles, CA (United States) Johns Hopkins Univ., Laurel, MD (United States) National Research Council of Canada, Herzberg Inst. of Astrophysics, Ottawa (Canada) Canadian Network for Space Research, Edmonton (Canada)
Ground based measurements from the CANOPUS array of meridian scanning photometers and precipitating ion and electron data from the DMSP F9 satellite show that the electron arc which brightens to initiate substorms intensifications is formed within a region of intense proton precipitation that is well equatorward (about 4-6 deg) of the nightside open-closed field line boundary. The precipitating protons are from a population that is energized via Earthward convection from the magnetotail into the dipolar region of the magnetosphere and may play an important role in the formation of the electron arcs leading to substorm intensifications on dipolelike field lines. 12 refs.
OSTI ID:
6901848
Journal Information:
Geophysical Research Letters (American Geophysical Union); (United States), Journal Name: Geophysical Research Letters (American Geophysical Union); (United States) Vol. 19:21; ISSN GPRLAJ; ISSN 0094-8276
Country of Publication:
United States
Language:
English