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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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书目名称Dynamical and Chemical Coupling Between the Neutral and Ionized Atmosphere
副标题Proceedings of the N
编辑B. Grandal,J. A. Holtet
视频video
丛书名称Nato Science Series C:
图书封面Titlebook: Dynamical and Chemical Coupling Between the Neutral and Ionized Atmosphere; Proceedings of the N B. Grandal,J. A. Holtet Conference proceed
描述These proceedings are based upon the review lectures, the re­ search talks and the accompanying discussion from the NATO Advanced Study Institute 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 interdisciplinary effort of the scien­ tists working on a variety of atmospheric phenomena. This Advanced Study Institute was organized in order to meet this demand. A number of eminent scientists were invited to review the major subfields in atmospheric physics and expose the areas where the coupling between the neutral and ionized atmosphere is evident. These review papers were supported by current research results. However, the material covered here is by no means complete con­ sidering the range of subject matter covered by the title. The re­ sponsibility for this inadequacy lies with the editors and the pro­ gram committee, rather than with the individual contributors. Oslo, June 1977. B. Grandal J.A. Holtet. PARTICIPANTS Max-Planck-Institute for Nuclear Ph
出版日期Conference proceedings 1977
关键词Cloud; Ionosphere; Precipitation; Scale; Wind; atmosphere; satellite; spheric; temperature
版次1
doihttps://doi.org/10.1007/978-94-010-1262-1
isbn_softcover978-94-010-1264-5
isbn_ebook978-94-010-1262-1Series ISSN 1389-2185
issn_series 1389-2185
copyrightD. Reidel Publishing Company, Dordrecht, Holland 1977
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Kupfern the atmosphere. The discussion will be limited to frequencies above 0,01 Hz. Infrasonic waves with frequencies below 4 Hz, if launched at sufficiently large angle from the vertical direction will be reflected and will propagate to large distances in the waveguide created by the reflecting layer an
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Aluminiumgross response of the thermosphere to such things as changes in solar ultraviolet flux and geomagnetic activity, more and more specific questions are being asked about the detailed thermospheric behavior. The search for greater understanding requires ever more detailed measurements. In the past, mea
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Antimonese compounds have been chemidissociated or photodissociated, hydrogen engages into active chemical reactions, whether in atomic or in compound forms, various types of effects on the ozone concentration have been identified, (Nicolet 1975; Booker et al. 1975). The effect of HO. on O. concentration c
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Antimone are to be assembled for reference purposes. Agreement has been obtained that significant experimental evidence and not aeronomic theory should be the basis of IRI. Theoretical explanation should be left to individual scientists while assembling and reviewing experimental results is an adequate tas
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