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Titlebook: Magnetospheric Particles and Fields; Proceedings of the S B. M. McCormac Conference proceedings 1976 D. Reidel Publishing Company, Dordrech

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Plasma in the Polar Cusp and Plasma Mantle,reported by Hones .. (1972) and Akasofu .. (1973), who used the term ‘boundary layer’. The tail lobe plasma, recently observed in the magnetotail at the orbit of the moon (Hardy .., 1975) presumably refers to the same plasma layer.
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An Overview of Magnetospheric Dynamics,techniques for making such measurements). The fact that the basic ideas of magnetospheric convection then proposed are still considered valid today is a tribute not only to the physical insight of their authors but also to the validity and power of the MHD approach that was used.
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Impulsive Ion Injection into the Polar Cusp,ctra. The bursts had a duration of about 20 s and repetition period on the order of 100 s. These results suggest that ions have intermittent rather than continuous entry at the polar cusps. At times, the ion and electron precipitation was anticorrelated in a manner consistent with a parallel electric field.
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Magnetotail Model,so that the existing quantitative results have fairly limited ranges of applicability. This is the reason why this paper deals with the theory of the tail of the magnetosphere only, and in fact we are probably covering only a fraction of the tail, namely radial distances from the Earth between, say 20 and 60 ...
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,Examples of Plasma Flows within the Earth’s Magnetosphere,strument threshold of ~ 20kms. to speeds of 50 km s.. Strong tailward ‘jetting’ of plasmas, in the range of 200 to 300 km s., at geocentric radial distances ~ 35 .. in the plasma sheet is found to be often associated with the occurrence of magnetic substorms.
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