Statistics of the Longitudinal Splitting of the Proton Aurora during Substorms

Physics

Scientific paper

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[2704] Magnetospheric Physics / Auroral Phenomena, [2744] Magnetospheric Physics / Magnetotail, [2764] Magnetospheric Physics / Plasma Sheet, [2790] Magnetospheric Physics / Substorms

Scientific paper

The isotropy boundary, i.e. the lower limit of significant proton precipitation into the ionosphere, moves equatorward as the geosynchronous magnetic field elevation angle decreases. At the beginning of the substorm expansion phase, the magnetic field is highly stretched (low elevation angle) except in a very azimuthally localized region (the substorm current wedge). As reconnected flux continues to pile up, the substorm current wedge grows both azimuthally and radially. Using a combination of 264 high quality events imaged by the spectrographic imager onboard the IMAGE spacecraft and global MHD simulations, we show that the proton aurora often has a significant decrease in intensity (split) at local times that map into the substorm current wedge. The splitting is much more likely to happen for substorms with lower AL. We show that other parameters such as the width and expansion speed of the split region also correlate with the AL index.

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