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• W2085885155 startingPage "6825" @default.
• W2085885155 abstract "Below an altitude of 400 km or less over the NASA Wallops Island range, stably trapped particles do not exist because of the South Atlantic Anomaly. In an experiment to measure scattered electrons at these altitudes (NASA flight 36:013), electron detectors clearly measured two monoenergetic electron peaks above the low background. The two monoenergetic peaks are attributed to the resonant interaction of electrons with VLF waves from Navy ground transmitters at Cutler, Maine, and Annapolis, Maryland. The transmitter signals were measured with electric and magnetic receivers aboard the rocket, and their propagation through the ionosphere and correlation with the precipitated electrons are discussed. In addition, energetic ions were also measured to be in the bounce loss cone during this rocket flight. Because of increased geomagnetic activity, it appears that the ring current extended inward to at least the L = 2.5 magnetic shell and enhanced convection eroded the plasmasphere. The inward movement or compression of the plasmapause is consistent with a steep gradient in the equatorial cold plasma density and a localized equatorial interaction region needed to account for the monoenergetic electron precipitation. The role of the geomagnetic activity in “priming” the trapped electron population for cyclotron resonance with VLF waves such that there is continuous scattering into the bounce loss cone remains uncertain." @default.
• W2085885155 created "2016-06-24" @default.
• W2085885155 creator A5033711169 @default.
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• W2085885155 date "1989-06-01" @default.
• W2085885155 modified "2023-09-26" @default.
• W2085885155 title "Rocket observations of the precipitation of electrons by ground VLF transmitters" @default.
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• W2085885155 doi "https://doi.org/10.1029/ja094ia06p06825" @default.
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