Abstract

Abstract. Extending previous studies, a full-circle investigation of the ring current has been made using Cluster 4-spacecraft observations near perigee, at times when the Cluster array had relatively small separations and nearly regular tetrahedral configurations, and when the Dst index was greater than −30 nT (non-storm conditions). These observations result in direct estimations of the near equatorial current density at all magnetic local times (MLT) for the first time and with sufficient accuracy, for the following observations. The results confirm that the ring current flows westward and show that the in situ average measured current density (sampled in the radial range accessed by Cluster ~4–4.5 RE) is asymmetric in MLT, ranging from 9 to 27 nA m−2. The direction of current is shown to be very well ordered for the whole range of MLT. Both of these results are in line with previous studies on partial ring extent. The magnitude of the current density, however, reveals a distinct asymmetry: growing from 10 to 27 nA m−2 as azimuth reduces from about 12:00 MLT to 03:00 and falling from 20 to 10 nA m−2 less steadily as azimuth reduces from 24:00 to 12:00 MLT. This result has not been reported before and we suggest it could reflect a number of effects. Firstly, we argue it is consistent with the operation of region-2 field aligned-currents (FACs), which are expected to flow upward into the ring current around 09:00 MLT and downward out of the ring current around 14:00 MLT. Secondly, we note that it is also consistent with a possible asymmetry in the radial distribution profile of current density (resulting in higher peak at ~4–4.5 RE). We note that part of the enhanced current could reflect an increase in the mean AE activity (during the periods in which Cluster samples those MLT).

Highlights

  • The existence of the westward equatorial ring current around the Earth at geocentric distances of about 2–9 RE (RE is a mean Earth radius) was first suggested by Singer (1957)

  • The present paper extends the study of Vallat et al (2005) to survey the distributions of the ring current at all magnetic local times (MLT) and discuss the locations of the connecting region 2 field-aligned currents (FACs)

  • We have investigated an almost full year of magnetic field data from the four Cluster spacecraft at times when they had small separations, nearly regular tetrahedral configurations, and Dst was greater than −30 nT

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Summary

Introduction

The existence of the westward equatorial ring current around the Earth at geocentric distances of about 2–9 RE (RE is a mean Earth radius) was first suggested by Singer (1957). It is understood in terms of the gradient and curvature drifts of energetic particles (∼1 keV to a few hundreds of keV), trapped in the geomagnetic field. Because simultaneous magnetic field measurements at multiple, geometrically favorable positions were unavailable prior to Cluster, it had been impossible to obtain a precise idea about the current response to magnetospheric changes. Cluster (Escoubet et al, 2001) has provided us with a unique opportunity to directly survey the distribution of the ring current

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