Coherent waveforms in the auroral upward current region

S. Matsukiyo, R. A. Treumann, M. Scholer

Research output: Contribution to journalArticle

23 Citations (Scopus)

Abstract

With the help of one-dimensional particle-in-cell simulations we show that observations of high-frequency electric wave spectra in the auroral upward current region can be reproduced. Using distribution functions suggested by the measurements, we find that in the nonlinear state, ion acoustic waves and electron two-stream (Langmuir) waves dominate the spectrum. In the absence of cold electrons, electron acoustic waves are not excited initially but appear only at a late time. They are the result of the formation of a two-temperature electron plasma by nonlinear interactions when all other instabilities have saturated. However, owing to the weakness of these electron acoustic waves, they are less important for the formation of electron holes and affect the particle dynamics much less than the two-stream instability.

Original languageEnglish
Article numberA06212
JournalJournal of Geophysical Research: Space Physics
Volume109
Issue numberA6
DOIs
Publication statusPublished - Jan 1 2004
Externally publishedYes

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waveforms
electrons
electron
Electrons
acoustic wave
Ion acoustic waves
ion acoustic waves
acoustics
Acoustic waves
electron plasma
Plasma stability
Electron temperature
Beam plasma interactions
Electromagnetic waves
distribution functions
wave spectrum
Distribution functions
Plasmas
cells
ions

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Forestry
  • Oceanography
  • Aquatic Science
  • Ecology
  • Water Science and Technology
  • Soil Science
  • Geochemistry and Petrology
  • Earth-Surface Processes
  • Atmospheric Science
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science
  • Palaeontology

Cite this

Coherent waveforms in the auroral upward current region. / Matsukiyo, S.; Treumann, R. A.; Scholer, M.

In: Journal of Geophysical Research: Space Physics, Vol. 109, No. A6, A06212, 01.01.2004.

Research output: Contribution to journalArticle

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