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Titlebook: Dynamical and Chemical Coupling Between the Neutral and Ionized Atmosphere; Proceedings of the N B. Grandal,J. A. Holtet Conference proceed

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Ion Composition and Electron-and Ion-Loss Processes in the Earth’s Atmosphereents by rocket-borne mass spectrometers which will be discussed in some more detail. The basic aspect of this article will be the attempt to identify those processes which are important in controlling the ionisation — recombination cycle and thereby determine the plasma densities.
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Dynamical and Chemical Coupling Between the Neutral and Ionized AtmosphereProceedings of the N
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Nickelture of the upper stratosphere and mesosphere to be given here will be based mainly on results from the PMR. This data is still in a preliminary form at the time of writing and should be treated with caution.
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Aluminiumhile good latitude and longitude coverage is possible, altitude profiles above a fixed surface point have not been possible. In the lower thermosphere (below 150 km) the high drag experienced by satellites with such low perigees makes . . measurements unattractive.
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Uranents by rocket-borne mass spectrometers which will be discussed in some more detail. The basic aspect of this article will be the attempt to identify those processes which are important in controlling the ionisation — recombination cycle and thereby determine the plasma densities.
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1389-2185 itute on "The Dynamical and Chemical Coupling of the Neutral and Ionized Atmosphere" held at Spatind, Norway April 12-22, 1977. In recent years, in spite of the many subdivisions of atmospher­ ic physics it has become clear that a complete understanding of the subject matter requires an interdiscipl
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Conference proceedings 1977The Dynamical and Chemical Coupling of the Neutral and Ionized Atmosphere" held at Spatind, Norway April 12-22, 1977. In recent years, in spite of the many subdivisions of atmospher­ ic physics it has become clear that a complete understanding of the subject matter requires an interdisciplinary effo
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