Vertical evolution of auroral acceleration at substorm onset

A. Morioka, Y. Miyoshi, F. Tsuchiya, H. Misawa, K. Yumoto, G. K. Parks, R. R. Anderson, J. D. Menietti, F. Honary

Research output: Contribution to journalArticle

16 Citations (Scopus)

Abstract

This study describes the onset process of auroral substorms in connection with the vertical evolution of auroral particle acceleration, on the basis of auroral kilometric radiation (AKR) dynamics. We show that the auroral acceleration process at substorm onset basically consists of two stages: (1) appearance/intensification of a low-altitude acceleration region at 4000-5000 km accompanied by initial brightening and (2) breakout of high-altitude field-aligned acceleration above the pre-existing low-altitude acceleration region at 6000-12 000 km, which is followed by auroral breakup and poleward expansion. It is also revealed that this two-stage evolution of auroral acceleration corresponds to the two-step reinforcement of field-aligned current.

Original languageEnglish
Pages (from-to)525-535
Number of pages11
JournalAnnales Geophysicae
Volume27
Issue number2
DOIs
Publication statusPublished - 2009 Feb 9

Keywords

  • Auroral phenomena
  • Magnetosphere-ionosphere interactions
  • Magnetospheric physics
  • Storms and substorms

ASJC Scopus subject areas

  • Astronomy and Astrophysics
  • Geology
  • Atmospheric Science
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science

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  • Cite this

    Morioka, A., Miyoshi, Y., Tsuchiya, F., Misawa, H., Yumoto, K., Parks, G. K., Anderson, R. R., Menietti, J. D., & Honary, F. (2009). Vertical evolution of auroral acceleration at substorm onset. Annales Geophysicae, 27(2), 525-535. https://doi.org/10.5194/angeo-27-525-2009