AlO RESONANT SPECTRA AND TEMPERATURE MEASUREMENT OF THE THERMOSPHERE. PART I. DESCRIPTION OF THE METHOD. PDF Download
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Author: Ove E. Harang Publisher: ISBN: Category : Languages : en Pages : 61
Book Description
The report discusses the principle of temperature determination of the upper atmosphere by analyzing spectra emitted by rocket released agents into the upper atmosphere and describes a procedure for temperature deduction. The agent considered is the AlO-aluminium monoxide released during twilight and the spectrum observed is a resonant emission spectrum with clear molecular band structure. The temperature is deduced by a procedure of fitting the measured spectra to synthetic spectra. (Author).
Author: Ove E. Harang Publisher: ISBN: Category : Languages : en Pages : 61
Book Description
The report discusses the principle of temperature determination of the upper atmosphere by analyzing spectra emitted by rocket released agents into the upper atmosphere and describes a procedure for temperature deduction. The agent considered is the AlO-aluminium monoxide released during twilight and the spectrum observed is a resonant emission spectrum with clear molecular band structure. The temperature is deduced by a procedure of fitting the measured spectra to synthetic spectra. (Author).
Author: Publisher: ISBN: Category : Aeronautics Languages : en Pages : 1370
Book Description
Lists citations with abstracts for aerospace related reports obtained from world wide sources and announces documents that have recently been entered into the NASA Scientific and Technical Information Database.
Author: S. Chapman Publisher: Springer Science & Business Media ISBN: 9789027701138 Category : Science Languages : en Pages : 218
Book Description
Everyone is familiar with the daily changes of air temperature. The barometer shows that these are accompanied by daily changes of mass distribution of the atmosphere, and consequently with daily motions of the air. In the tropics the daily pressure change is evident on the barographs; in temperate and higher latitudes it is not noticeable, being overwhelmed by cyclonic and anticyclonic pressure variations. There too, however, the daily change can be found by averaging the variations over many days; and the same process suffices to show that there is a still smaller lunar tide in the atmosphere, first sought by Laplace. Throughout nearly two centuries these 'tides', thermal and gravitational, have been extensively discussed in the periodical literature of science, although they are very minor phenomena at ground level. This monograph summarizes our present knowledge and theoretical under standing of them. It is more than twenty years since the appearance of the one previous monograph on them - by Wilkes - and nearly a decade since they were last comprehensively reviewed, by Siebert. The intervening years have seen many additions to our know ledge of the state of the upper atmosphere, and of the tides there, on the basis of measurements by radio, rockets and satellites.
Author: Ove E. Harang
Author: Ove E. Harang
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Author: S. Chapman