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Titlebook: Earth’s Magnetospheric Processes; Proceedings of a Sym B. M. McCormac Conference proceedings 1972 D. Reidel Publishing Company, Dordrecht,

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樓主: obdurate
41#
發(fā)表于 2025-3-28 16:10:47 | 只看該作者
Astrophysics and Space Science Libraryhttp://image.papertrans.cn/e/image/300938.jpg
42#
發(fā)表于 2025-3-28 22:09:27 | 只看該作者
https://doi.org/10.1057/9780230346680Not so long ago the region of space that we now call the magnetosphere used to be considered a very simple part of our environment from a physical point of view: essentially a vacuum penetrated by a magnetic field.
43#
發(fā)表于 2025-3-28 23:39:50 | 只看該作者
https://doi.org/10.1007/978-0-387-68120-7Precipitation patterns of electrons on the dayside have been studied for many years using ground based evidence and satellite experiments. This article will summarize some of the more recent work, and attempt to extend and refine our understanding of these regions.
44#
發(fā)表于 2025-3-29 04:43:49 | 只看該作者
45#
發(fā)表于 2025-3-29 09:55:40 | 只看該作者
46#
發(fā)表于 2025-3-29 14:26:18 | 只看該作者
Pitch Angles and Spectra of Particles in the Outer Zone Near NoonPrecipitation patterns of electrons on the dayside have been studied for many years using ground based evidence and satellite experiments. This article will summarize some of the more recent work, and attempt to extend and refine our understanding of these regions.
47#
發(fā)表于 2025-3-29 17:30:44 | 只看該作者
Angular Distributions of Precipitating ElectronsFor auroral electrons the angular distribution within the loss cone is probably the most sensitive indicator of the mechanism which causes the precipitation. However, in the energy range of a few keV, which generally contains most of the auroral electron flux, only very limited results have been reported to date.
48#
發(fā)表于 2025-3-29 22:42:53 | 只看該作者
49#
發(fā)表于 2025-3-30 00:43:42 | 只看該作者
50#
發(fā)表于 2025-3-30 06:25:38 | 只看該作者
New Results on Particle Arrival at the Polar Capsid and Sauer, 1967). More recent satellite results have shown that in at least two solar particle events (Evans and Stone, 1969; Van Allen ., 1971) there were indeed large particle intensity differences between north and south polar regions.
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