Skip to main navigation Skip to search Skip to main content

‘Self‐consistent’ production of ion conics on return current region auroral field lines: A time‐dependent, semi‐kinetic model

  • David G. Brown
  • , Gordon R. Wilson
  • , James L. Horwitz
  • , Dennis L. Gallagher
  • University of Alabama in Huntsville
  • NASA Marshall Space Flight Center

Research output: Contribution to journalArticlepeer-review

20 Scopus citations

Abstract

We describe initial results from a time‐dependent, semi‐kinetic model of plasma outflow incorporating wave‐particle interactions along current‐carrying auroral field lines. Electrostatic waves are generated by the current driven ion cyclotron instability (CDICI), causing perpendicular velocity diffusion of ions plus electron heating via anomalous resistivity when and where the relative drift between electrons and ions exceeds certain critical velocities. Using the local bulk parameters we calculate these critical velocities, and so are able to self‐consistently switch on and off the heating of the various particle species. Due to the dependence of these critical velocities on the bulk parameters of the species the heating effects exhibit quite complex spatial and temporal variations. A wide range of ion distribution functions are observed in these simulations, including conics with energies of a few electron volts and ‘ring’ distributions. The rings are seen to be a natural result of transverse heating and velocity filter effects and do not require coherent acceleration processes. We also observe the formation of a density depletion in hydrogen and enhanced oxygen densities at high altitudes.

Original languageEnglish
Pages (from-to)1841-1844
Number of pages4
JournalGeophysical Research Letters
Volume18
Issue number10
DOIs
StatePublished - Oct 1991
Externally publishedYes

Fingerprint

Dive into the research topics of '‘Self‐consistent’ production of ion conics on return current region auroral field lines: A time‐dependent, semi‐kinetic model'. Together they form a unique fingerprint.

Cite this