Titlebook: Magnetosphere-Ionosphere Coupling; Yohsuke Kamide,Wolfgang Baumjohann Book 1993 Springer-Verlag Berlin Heidelberg 1993 Plasma.Variation.au

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w how this methodology is implemented in practice with curreSince Charles Spearman published his seminal paper on factor analysis in 1904 and Karl Joresk ¨ og replaced the observed variables in an econometric structural equation model by latent factors in 1970, causal modelling by means of latent va

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Morphology of Electric Fields and Currents at High Latitudes,s schematically shown in Fig. 2.1, the compression of the terrestrial magnetic field on the dayside is caused by currents flowing perpendicular to the dipole field lines across the magnetopause surface. These currents are often called Chapman-Ferraro currents since Chapman and Ferraro were the first

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Global Modeling of Magnetosphere-Ionosphere Coupling, both regions. To understand the coupling system in its entirety, we are seeking a set of solutions for the well-defined equations given in Section 1.2 with realistic boundary conditions. We note, however, even with drastic simplifications the problem for the complete, self-consistent chains for the

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Modeling of Ionospheric Electrodynamics,ual links. Studies of theoretical models, which intend to examine the entire loop, and those attempting to understand “l(fā)ocal” chains, or individual links, must be complementary to each other. Sato (1985) called the latter “l(fā)ocal” key regions, where remarkable energy conversion processes are taking p

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Book 1993d currents at high latitudes; - global modeling of magnetosphere-ionosphere coupling; - modeling of ionospheric electrodynamics; - current issues, such as auroral particle acceleration, substorms, penetration of high-latitude fields into low latitudes.

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