Electron and wave characteristics observed by the THEMIS satellites near the magnetic equator during a pulsating aurora

  • A. Nakajima
  • , K. Shiokawa
  • , K. Sakaguchi
  • , Y. Miyoshi
  • , S. Lee
  • , V. Angelopoulos
  • , O. Le Contel
  • , J. P. McFadden
  • , J. W. Bonnell
  • , K. H. Fornacon
  • , E. Donovan

Research output: Contribution to journalArticlepeer-review

Abstract

Based on conjugate ground and THEMIS satellite observations, we show electron spectra and wave characteristics near the magnetic equatorial plane during a pulsating aurora event on the high latitude side of the auroral oval. The pulsating aurora was observed by a 30-Hz sampled all-sky imager (ASI) at Gillam (56.4°N, 265.4°E), Canada, at ∼0840-0910 UT on 8 January 2008. The auroral intensity pulsation at the possible THEMIS D (THD) footprints had frequency peaks at ∼0.1-0.2 Hz. The footprint of THD was in the poleward part of the proton aurora observed by a meridian-scanning photometer. After auroral pulsation began at ∼0842 UT, both THD and THEMIS E which was near THD in the mid-tail at 11.6-11.8 RE, observed enhanced field-aligned electron fluxes at energies of 1-10 keV. However, the amplitudes of whistler mode waves and electrostatic cyclotron harmonics (ECH) waves observed by THD with the highest sampling rate of 8 kHz were not significant, showing a marked contrast to the recent report of clear correlation between whistler mode waves and auroral pulsations observed at 5-9 RE. We suggest that the observed field-aligned electrons, which are probably caused by Fermi-type acceleration associated with earthward plasma flow in the mid-tail plasma sheet, are modulated by some wave processes to cause pulsating auroras.

Original languageEnglish
Article numberA03219
JournalJournal of Geophysical Research: Space Physics
Volume117
Issue number3
DOIs
Publication statusPublished - 1 Jan 2012

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