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Titlebook: Exploration of the Polar Upper Atmosphere; Proceedings of the N Charles S. Deehr,Jan A. Holtet Conference proceedings 1981 D. Reidel Publis

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书目名称Exploration of the Polar Upper Atmosphere
副标题Proceedings of the N
编辑Charles S. Deehr,Jan A. Holtet
视频video
丛书名称Nato Science Series C:
图书封面Titlebook: Exploration of the Polar Upper Atmosphere; Proceedings of the N Charles S. Deehr,Jan A. Holtet Conference proceedings 1981 D. Reidel Publis
描述This book is an ordered collection of tutorial lectures on the physical processes in the polar upper atmosphere given at the NATO Advanced Study Institute (ASI) on "The Exploration of the Polar Upper Atmosphere" held at Lillehammer, Norway, May 5-16, 1980. The polar cap is an important part of the high latitude atmosphere not only because of circulation and horizontal trans­ port in the neutral atmosphere and convection in the ionosphere, but also because of its unique energy sources and sinks. In addition, solar wind plasma is led into-the upper atmosphere by the geomagnetic field at the poles, and the polar cap is, as stated by Tutorial Leader Roederer in this volume, "the place where outer space meets earth". The atmosphere at lower latitudes is well-known to the ground-based observer, and the advent of satellite observations was simply the beginning of a new perspective. The exploration of the atmosphere at polar latitudes, however, proceeded in quite the opposite manner, and satellite maps of the polar caps may be compared with a relatively meagre set of ground-based data. Recent efforts to extend the polar observations from the ground have resulted in the need for a review of
出版日期Conference proceedings 1981
关键词Absorption; Ionosphere; Precipitation; Scale; Weather; Wind; magnetosphere; satellite
版次1
doihttps://doi.org/10.1007/978-94-009-8417-2
isbn_softcover978-94-009-8419-6
isbn_ebook978-94-009-8417-2Series ISSN 1389-2185
issn_series 1389-2185
copyrightD. Reidel Publishing Company, Dordrecht, Holland 1981
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Dynamics of the Thermosphere During Quiet and Disturbed Conditions external forcing. A simplified theory of the propagation and generation of acoustic-gravity waves and of planetary waves is outlined using the linearization of the hydrodynamic equations and the superposition of harmonic waves via a Fourier series of a Fourier integral. The main energy sources at t
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Wind Induced Composition Effects at High Latitudesectively transport the lighter and minor species from the warmer toward the cooler regions on the globe. Due to the abundance of atomic oxygen a back pressure develops which significantly dampens the wind velocities and increases the temperature contrast. During summer and under magnetically disturb
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Radio Observations of the Auroral F-Regionave been made by means of ground based and satellite borne ionosondes respectively. From these data, the basic features and behaviour of the region have been determined. In recent years new techniques, such as incoherent scatter radar, have added to our knowledge, particularly regarding transient be
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Polar Cap Optical Emissions Observed from the ISIS2 Satellitelar cap processes. The ISIS2 satellite, which is in a circular orbit 1400 km above the earth’s surface, has provided monochromatic optical images of the high latitude region since April 1971. The 5577Å emission from atomic oxygen and the 3914 Å emission from the First Negative bands of N.. have been
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Optical Emissions in the Polar Auroral E-Region molecular oxygen emissions in the airglow require a peak atomic oxygen concentration of about 1.E12 cm-3*. It is suggested that these emissions are excited in a two step process similar to the Barth mechanism for the green line. It is proposed that monitoring of the green line and the atmospheric b
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