skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: A multievent study of broadband electrons observed by the DMSP satellites and their relation to red aurora observed at midlatitude stations

Journal Article · · Journal of Geophysical Research
DOI:https://doi.org/10.1029/97JA00741· OSTI ID:542177
 [1];  [2];  [3];  [4];  [5]
  1. Solar-Terrestrial Environment Laboratory, Nagoya University, Toyokawa (Japan)
  2. Applied Physics Laboratory, Johns Hopkins University, Baltimore, Maryland (United States)
  3. Los Alamos National Laboratory, Los Alamos, New Mexico (United States)
  4. Air Force Geophysics Laboratory, Hanscom Air Force Base, Massachusetts (United States)
  5. Faculty of Science, Kyushu University, Fukuoka (Japan)

Broadband electrons during magnetic storms are characterized by an unusually intense flux of precipitating electrons in the broadband energy range from 30 eV to 30 keV near the equatorward edge of the auroral oval (47{degree}{endash}66{degree} magnetic latitude). Broadband electrons were first reported by {ital Shiokawa} {ital et al.} [1996]. In this paper, we report a multievent study of broadband electrons, using particle data obtained by the Defense Meteorological Satellite Program (DMSP) satellites during 23 magnetic storms from January 1989 through May 1992. Twelve broadband electron events are identified. Most of them are observed in the night sector, but some are observed in the morning sector. Particle data for successive polar passes of the DMSP multisatellites are used to show that broadband electrons generally last for less than 30 min and that for some events, they precipitate over a wide range of local times simultaneously. On the basis of a quantitative calculation of optical emissions from electrons in the neutral atmosphere, we conclude that broadband electrons are a possible cause of red auroras observed at midlatitude ground stations. We suggest that broadband electrons are associated with certain substorms during the main phase of magnetic storms. This conjecture comes from observations of H component positive bays and Pi 2 pulsations observed at low-latitude magnetic stations and from magnetic field variations observed at geosynchronous satellites. We conclude that the magnetospheric source of broadband electrons lies within the inner part of the plasma sheet. This conclusion is based on the facts that broadband electrons appear in latitudes where plasma sheet particles were observed before the event and that broadband electrons are observed poleward of the subauroral ion drifts, a position that corresponds to the inner edge of the injected particle layer during storms. (Abstract Truncated)

OSTI ID:
542177
Journal Information:
Journal of Geophysical Research, Vol. 102, Issue A7; Other Information: PBD: Jul 1997
Country of Publication:
United States
Language:
English

Similar Records

Modeling subauroral polarization streams during the 17 March 2013 storm
Journal Article · Thu Mar 12 00:00:00 EDT 2015 · Journal of Geophysical Research. Space Physics · OSTI ID:542177

Storm time electric field penetration observed at mid-latitude
Journal Article · Mon Apr 01 00:00:00 EST 1991 · Journal of Geophysical Research; (United States) · OSTI ID:542177

A new ionospheric electron precipitation module coupled with RAM-SCB within the geospace general circulation model
Journal Article · Thu Sep 01 00:00:00 EDT 2016 · Journal of Geophysical Research. Space Physics · OSTI ID:542177