Abstract

Abstract. Satellite measurements show that ion beams above the auroral acceleration region are heated to hundreds of eV in a direction perpendicular to the magnetic field. We show that ion acoustic waves may be responsible for much of this heating. Even in the absence of a positive slope in the velocity distribution of the beam ions, ion acoustic waves can be generated by a fan instability. We present analytical estimates of the wave growth rate and ion beam heating rate. These estimates, which are confirmed by particle simulations, indicate that the perpendicular temperature of the beam ions will increase by 30 eV/s, or by 1 eV in 20–25 km. From the simulations we also conclude that the heating saturates at a perpendicular temperature around 200 eV, which is consistent with observations.Key words. Ionosphere (wave-particle interactions) · Magnetospheric Physics (plasma waves and instabilities) · Space plasma physics (wave-particle interactions).

Highlights

  • Energetic upowing ®eld-aligned ion beams with keV energies are a frequently occurring phenomenon in the auroral zone

  • Energetic ion beams created only by acceleration of a background ion component in a parallel electric ®eld would show no change in the perpendicular temperature of the beams, and a decrease in the parallel temperature

  • The growth rate of ion acoustic waves due to the ion fan instability and the rate of perpendicular heating caused by these waves as predicted by quasi-linear theory are con®rmed quantitatively by our simulations

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Summary

Introduction

Energetic upowing ®eld-aligned ion beams with keV energies are a frequently occurring phenomenon in the auroral zone. There are many statistical studies of the ion beam drift energies, composition and occurrence frequencies depending on factors such as solar activity, altitude, magnetic local time and invariant latitude (Kondo et al, 1990; Collin et al, 1987; Yau et al, 1984; Gorney et al, 1981). Vaivads accelerated by a quasi-static electric ®eld parallel to the ambient magnetic ®eld (Rei€ et al, 1988). The shape of the ion beam distributions cannot be explained by a parallel quasi-static electric ®eld alone. Energetic ion beams created only by acceleration of a background (ionospheric) ion component in a parallel electric ®eld would show no change in the perpendicular temperature of the beams, and a decrease in the parallel temperature (the temperature de®ned from the average energy of beam ions in the beam reference system)

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