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- W2110135888 abstract "A comparison of low-energy charged-particle intensities measured with the low-altitude satellite Injun 5 and a ground-based observation of an auroral arc at Fort Churchill on December 21, 1968, during late local evening has established that an intense precipitation band of electron intensities provides the primary energy influx for the auroral light. This precipitation event was located poleward of and adjacent to the trapping boundary for more energetic electron (above 45 keV) intensities. Proton and electron intensities similar to those in the plasma sheet in the magnetotail were observed in a substantially less-intense zone positioned equatorward of and adjacent to the trapping boundary. The intense precipitation band of electron intensities poleward of the trapping boundary is interpreted as the signature of direct acceleration of magnetosheath electrons into the earth's atmosphere." @default.
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- W2110135888 date "1972-03-01" @default.
- W2110135888 modified "2023-10-16" @default.
- W2110135888 title "Correlated satellite measurements of low-energy electron precipitation and ground-based observations of a visible auroral arc" @default.
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- W2110135888 doi "https://doi.org/10.1029/ja077i007p01128" @default.
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