Abstract

Abstract. The pitch-angle distributions (PAD) of energetic particles are examined as the ISEE-1 satellite crosses the Earth’s magnetopause near the subsolar point. The investigation focuses on the possible existence of a particular type of distribution that would be associated with a source of energetic particles in the high-latitude magnetosphere. PADs, demonstrating broad, persistent field-aligned fluxes filling a single hemisphere (upper/northern or lower/southern), were observed just sunward of the magnetopause current layer for an extended period of many minutes. These distributions are a direct prediction of a possible source of energetic particles located in the high altitude dayside cusp and we present five examples in detail of the three-dimensional particle distributions to demonstrate their existence. From these results, other possible causes of such PADs are examined.Key words. Magnetospheric physics (energetic particles, precipitating; magnetopause, cusp and boundary layers; magnetospheric configuration and dynamics)

Highlights

  • The recent discovery by the Polar satellite that the high altitude dayside cusp may be the location of an acceleration mechanism capable of producing appreciable fluxes of 100 s to 1000 s of keV ions from the shocked solar wind entering the cusp has been reported by Chen and Fritz (1998); Chen et al (1997)

  • In the 5 cases presented here, in a seasonal, chronological order, the ISEE-1 Medium Energy Particles Experiment (MEPE) observed field-aligned fluxes of energetic ions just sunward of the magnetopause near the subsolar point, as the spacecraft transitioned from a region of open field line geometry to a closed, or trapped, geometry

  • The particle distributions were observed to be present for extended periods on open field lines, ranging from two to tens of minutes, which suggests that they are a common occurrence

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Summary

Instrumentation and data selection

The data set used is from the ISEE-1 spacecraft which was launched together with ISEE-2 on October 1977 into an elliptic orbit with an apogee of RE, a perigee of 280 km, a period of about 57 h, and an inclination of about 28◦. The Medium Energy Particles Experiment (MEPE) on ISEE-1 and 2 was designed to detect electrons and ions ranging from 22.5 keV to 1.2 MeV for electrons, and from 24 keV to 2 MeV for protons. This resulted in 96 samples being made on the 4π steradian unit sphere. As a point of information about the ISEE-1 MEPE, the instrument responses from the WAPS sensor were accumulated in a manner that was synchronized to the satellite spin period and not the satellite telemetry cycle.

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