Abstract

Abstract. We have analyzed the onsets of energetic particle bursts detected by the ICS and STICS sensors of the EPIC instrument on board the GEOTAIL spacecraft in the deep magnetotail (i.e., at distances greater than 180 RE). Such bursts are commonly observed at the plasma-sheet boundary layer (PSBL) and are highly collimated along the magnetic field. The bursts display a normal velocity dispersion (i.e., the higher-speed particles are seen first, while the progressively lower speed particles are seen later) when observed upon entry of the spacecraft from the magnetotail lobes into the plasma sheet. Upon exit from the plasma sheet a reverse velocity dispersion is observed (i.e., lower-speed particles disappear first and higher-speed particles disappear last). Three major findings are as follows. First, the tailward-jetting energetic particle populations of the distant-tail plasma sheet display an energy layering: the energetic electrons stream along open PSBL field lines with peak fluxes at the lobes. Energetic protons occupy the next layer, and as the spacecraft moves towards the neutral sheet progressively decreasing energies are encountered systematically. These plasma-sheet layers display spatial symmetry, with the plane of symmetry the neutral sheet. Second, if we consider the same energy level of energetic particles, then the H+ layer is confined within that of the energetic electron, the He++ layer is confined within that of the proton, and the oxygen layer is confined within the alpha particle layer. Third, whenever the energetic electrons show higher fluxes inside the plasma sheet as compared to those at the boundary layer, their angular distribution is isotropic irrespective of the Earthward or tailward character of fluxes, suggesting a closed field line topology.

Highlights

  • Mobius et al (1980) performed a case-study of the near-Earth plasma-sheet boundary layer (PSBL) during substorm recovery. They found that the particle spectra at the central plasma sheet (CPS) were softer than at the PSBL, and that the alpha particle layer was con®ned to within the proton layer

  • Our results con®rm previous ISEE-3-examined velocity dispersions interpreted as spatial features

  • The temporal resolution, species di€erentiation, and multiplicity of channels of the energetic particle (EPIC) instrument provide us with a further insight into the problem of structure and dynamics of the Earth's magnetotail

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Summary

Introduction

Single-point measurements cannot distinguish spatial from temporal processes, in this paper we present evidence for spatial layering of the deep-tail plasma sheet at distances greater than 180 RE. Mobius et al (1980) performed a case-study of the near-Earth PSBL during substorm recovery They found that the particle spectra at the central plasma sheet (CPS) were softer than at the PSBL, and that the alpha particle layer was con®ned to within the proton layer. In the distant plasma sheet (as we shall see in this work), it is not uncommon that peakuxes of streaming particles occur at the PSBL In such cases, theuxes are associated with open magnetic ®eld topology. Richardson and Cowley (1985) examined tailwardstreaming ion bursts extending into the lobe for a few minutes before entry into or after exit from the plasma sheet in the deep geomagnetic tail They showed evidence at the leading edge of a normal velocity dispersion (i.e., high-energy particles are detected before low-energy ones), whereas at the trailing edge a reverse dispersion was detected. Our work concurs with these authors' conclusions and goes further to demonstrate the substructure of the distant-tail PSBL using GEOTAIL data sets

Observations and data analysis
Overview of studied interval
Additional examples of bursts with dispersive onsets
Findings
Discussion
Full Text
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