Auroral particles associated with a brightening arc

Physics

Scientific paper

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2700 Magnetospheric Physics, 2704 Auroral Phenomena (2407), 2716 Energetic Particles, Precipitating, 2736 Magnetosphere/Ionosphere Interactions, 2740 Magnetospheric Configuration And Dynamics

Scientific paper

We investigated characteristics of auroral particles precipitating to a brightening arc at the initial phase of a substorm, using auroral images obtained by high-time resolution (0.25 s) all-sky TV camera, particle data obtained by the DMSP F10 spacecraft and high-latitude magnetograms. The arc brightening was observed at 0407 UT on December 30, 1994 at Fort Smith (67.0 MLAT), Canada, coincident with high-latitude Pi 2 magnetic pulsations. The event has two characteristics; 1) the brightening did not develop into global scale (pseudo-breakup), and 2) Fort Smith seemed to be duskside of the main onset region. From the simultaneous DMSP particle data, we found that the brightening arc corresponded to an electron inverted-V structure near the equatorward edge of the electron precipitation region and at ~2 deg poleward of the equatorward edge of the ion precipitation region. This fact suggests that for the present event, the pseudo-breakup of auroral substorm occurred in the inner part of the plasma sheet.

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