Abstract

Abstract. Broadband waves around the lower hybrid frequency (around 10 Hz) near the magnetopause are studied, using the four Cluster satellites. These waves are common at the Earthward edge of the boundary layer, consistent with earlier observations, and can have amplitudes at least up to 5 mV/m. These waves are similar on all four Cluster satellites, i.e. they are likely to be distributed over large areas of the boundary. The strongest electric fields occur during a few seconds, i.e. over distances of a few hundred km in the frame of the moving magnetopause, a scale length comparable to the ion gyroradius. The strongest magnetic oscillations in the same frequency range are typically found in the boundary layer, and across the magnetopause. During an event studied in detail, the magnetopause velocity is consistent with a large-scale depression wave, i.e. an inward bulge of magnetosheath plasma, moving tailward along the nominal magnetopause boundary. Preliminary investigations indicate that a rather flat front side of the large-scale wave is associated with a rather static small-scale electric field, while a more turbulent backside of the large-scale wave is associated with small-scale time varying electric field wave packets.Key words. Magnetospheric physics (magnetopause, cusp, and boundary layers) – Space plasma physics (waves and in-stabilities)

Highlights

  • The magnetopause is a complex boundary between the Earth’s magnetosphere and the shocked solar wind

  • Preliminary results indicate that on the front side of the large-scale wave, the electric fields are rather static in the magnetopause frame, while the electric fields on the more turbulent “backside” of the large-scale wave consist of time varying electric field wave packets

  • Broadband electric field oscillations are common near the crossings of the boundary layer and the magnetopause, which is consistent with earlier observations, and these oscillations can have amplitudes at least up to 5 mV/m

Read more

Summary

Introduction

The magnetopause is a complex boundary between the Earth’s magnetosphere and the shocked solar wind. We present here observations of electric and magnetic field variations up to 10 Hz and higher in the spacecraft frame of reference, obtained by the four Cluster satellites during multiple crossings of the duskside magnetopause.

Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call