Articles | Volume 22, issue 6
Ann. Geophys., 22, 2213–2227, 2004
https://doi.org/10.5194/angeo-22-2213-2004
Ann. Geophys., 22, 2213–2227, 2004
https://doi.org/10.5194/angeo-22-2213-2004

  14 Jun 2004

14 Jun 2004

Different Alfvén wave acceleration processes of electrons in substorms at ~4-5 RE and 2-3 RE radial distance

P. Janhunen, A. Olsson, J. Hanasz, C. T. Russell, H. Laakso, and J. C. Samson P. Janhunen et al.
  • Finnish Meterological Institute, Department of Geophysics, P.O. Box 503, 00101 Helsinki, Finland

Abstract. Recent statistical studies show the existence of an island of cavities and enhanced electric field structures at 4-5RE radial distance in the evening and midnight magnetic local time (MLT) sectors in the auroral region during disturbed conditions, as well as ion beam occurrence frequency changes at the same altitude. We study the possibility that the mechanism involved is electron Landau resonance with incoming Alfvén waves and study the feasibility of the idea further with Polar electric field, magnetic field, spacecraft potential and electron data in an event where Polar maps to a substorm over the CANOPUS magnetometer array. Recently, a new type of auroral kilometric radiation (AKR) emission originating from ~2-3RE radial distance, the so-called dot-AKR emission, has been reported to occur during substorm onsets and suggested to also be an effect of Alfvénic wave acceleration in a pre-existing auroral cavity. We improve the analysis of the dot-AKR, giving it a unified theoretical handling with the high-altitude Landau resonance phenomena. The purpose of the paper is to study the two types of Alfvénic electron acceleration, acknowledging that they have different physical mechanisms, altitudes and roles in substorm-related auroral processes.

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