Titlebook: Atmospheric Physics from Spacelab; Proceedings of the 1 J. J. Burger,A. Pedersen,B. Battrick Conference proceedings 1976 D. Reidel Publishi

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https://doi.org/10.1007/978-3-642-18625-7scussed in relation to the formation of the ionospheric F-layer trough and the higher altitude plasma-pause. With regard to thermospheric dynamics, the effects of ion drag and Joule and particle heating were considered. Some emphasis was given to recent measurements which provide evidence for a hors

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https://doi.org/10.1007/978-3-642-35151-8lation between solar activity and atmospheric parameters at different heights are shown. The interest of studying the correlation that exists between important atmospheric parameters (physical and chemical) with the variations of the Sun flux at different wavelengths is stressed.

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Sabine Kubalek-Schröder,Frauke Dehlere radar météorique de Garchy et le sondeur à diffusion incohérente de St Santin. Les résultats obtenus par d’autres radars météoriques, ou d’autres sondeurs sont pris en compte pour étudier la variation en latitude des marées observées. Les principales caractéristiques des marées, diurne, semi-diurn

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Pathoneurophysiologie der gestörten Bewegungwere discussed. Emphasis was placed on identifying the regions in which particular reaction cycles involving OX, ClX, HOX and NOX are dominant and feedback effects that may occur when sources of these species are altered. In particular, the implications of recent measurements of height profiles for

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https://doi.org/10.1007/978-3-322-88406-0 generally accepted that catalytic reactions with nitrogen oxides (NO, NO.) as originally proposed by Crutzen (1970) are the dominant sinks of stratospheric ozone, and that we are able to increase the amounts of nitrogen oxides in the stratosphere through the action of high flying aircraft, to such

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