Titlebook: Atmospheric Electrodynamics; Hans Volland Book 1984 Springer-Verlag Berlin Heidelberg 1984 electric current.electrodynamics.geophysics

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Electric , and , Currents the electrically conducting air within the dynamo region between about 80 and 200 km height. The driving force is the tidal wind which moves the ionospheric plasma against the geomagnetic field and induces electric fields and currents. Manifestations of the electric currents on the ground are regul

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Coupling Between Solar Wind and Geomagnetic Field. In this chapter, we present an overview on the phenomenology of the solar wind and its impact on the geomagnetic field, leading to the magnetospheric cavity and to geomagnetic activity. Chapter 11 reviews the global-scale electric field and current configurations within the magnetosphere. In the f

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Theory of Wave Propagation Within the Magnetospherelities. Electromagnetic pulses generated by lightning events can propagate through the magnetosphere along the geomagnetic field lines and can be observed on the ground and within the magnetosphere. In the next two chapters, we present a short introduction into the theory of wave propagation through

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Appendixom pico (10.) to tera (10.). Only occasionally are other units used, in particular within figures adopted from the literature. One main advantage of SI units is the equivalence between the units of mechanical and electric energy: 1 joule = 1 watt × second.

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,Grundzüge des Intermedi?rstoffwechsels,g of the science of Atmospheric Electricity. The term “Atmospheric Electricity” reflects the earlier efforts to study mainly the electrostatic component of the geo-electromagnetic field. This subject now includes thunderstorm electrification, the global electric circuit, but also lightning and relat

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,Prüfung der endokrinen Funktionen,s occur in connection with thunderclouds. Lightning has been observed, however, during volcano eruptions and in dust storms. In this chapter, we outline the normal phenomenon of lightning. Ball and bead lightning are rare events and not well documented. We will not discuss these exotic forms of ligh

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https://doi.org/10.1007/978-3-7091-7737-2ut 100 kHz. They gradually evolve into red noise at higher frequencies (Fig. 7.1). The pulses arise from coherent electric currents in lightning channels during return strokes or . strokes. They are called atmospherics or simply “sferics” for short. Sferics are useful tools for locating thunderstorm