4.5 Article

Auroral poleward boundary intensifications and tail bursty flows:: A manifestation of a large-scale ULF oscillation? -: art. no. 1352

Journal

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2001JA000242

Keywords

poleward boundary intensifications; tail flows; magnetosphere-ionosphere interactions; ULF pulsations

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[1] Auroral zone observations often show significant ULF power. We have analyzed auroral and plasma sheet observations during two prolonged periods of strongly southward and relatively steady interplanetary magnetic field (IMF). We find evidence that auroral poleward boundary intensifications (PBIs), which have large intensity and occur repetitively throughout such periods, may be a manifestation of a large-scale ULF oscillation mode that strongly perturbs the plasma sheet and the auroral ionosphere. If this is correct, then ULF modes would be a major component of tail dynamics, of magnetosphere coupling to the ionosphere, and of auroral zone disturbances during periods of enhanced convection. They would simultaneously affect a large region of the nightside, extending along auroral zone field lines from the ionosphere to the equatorial plasma sheet and extending from field lines that lie near the magnetic separatrix to, at times, as close to the Earth as synchronous orbit. They would also occasionally have amplitudes as large as the changes that occur in association with other auroral zone disturbances such as substorms. Here we have found peak-to-peak amplitudes as high as several hundred nanoteslas in ground X, an order of magnitude in synchronous energetic proton fluxes, similar to20-40 nT in synchronous magnetic field components, similar to20 nT in tail magnetic field components, similar to1000 km/s in tail flow speeds, and similar to400 m/s in ionospheric flow speed. We find evidence for significant power at 0.5-0.7 mHz (similar to25-30 min period), significant power at a possible second harmonic (similar to1.1-1.3 mHz), and power at frequencies that could be higher harmonics simultaneously within the auroral ionosphere and within the nightside plasma sheet.

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