Mean Atmospheric Properties in the Range 30 to 300 Km

Mean Atmospheric Properties in the Range 30 to 300 Km
Author: K. S. W. Champion
Publisher:
Total Pages: 0
Release: 1965
Genre: Atmospheric density
ISBN:

A planned COSPAR publication contains a set of atmospheres for several latitudes and times of year for the altitude region 30 to 80 km developed by G.V. Groves. A second set of atmospheres was developed by W. Priester and I. Harris ('The upper atmosphere in the range from 120 to 800 km, ' Proposed CIRA, 1964) for the region between 120 and 800 km for various solar fluxes and times of day. For the purpose of connecting these two sets of atmospheres and also to provide average values of the physical properties, a mean reference atmosphere was prepared as described in this report. The Mean Reference Atmosphere was defined as follows: Between 30 and 80 km the model represents mean conditions throughout the year for latitudes near 30 degrees. Between 120 and 300 km the model represents mean conditions over a 24-hour period for a 10.7-cm wavelength solar flux F of 150 X 10 to the minus 22d power w/sq m/c/s. Between 80 and 120 km a model was developed which provides a smooth connection between the above two parts of the mean atmosphere. (Author).

Geophysik III / Geophysics III

Geophysik III / Geophysics III
Author: G. Schmidtke
Publisher: Springer Science & Business Media
Total Pages: 552
Release: 2013-12-11
Genre: Science
ISBN: 3642685315

This Encyclopedia aims, basically, at summanzmg the wealth of well established facts and outlining the relevant theories in the different branches of physics. With this as goal, the writers were asked to present their specific field in such a way that access is possible to any scientist without special a priori information in that field; the basic concepts of physics are assumed to be known to the reader. The survey given in each paper was also to be long lasting, so that even a few years after publication, each volume would be useful, for example as an introduction for newcomers or as a source of information for workers in a neighbouring field. In the field of geophysics, dealt with in Vols. 47--49 of the Encyclopedia, this task is difficult to achieve because during the last decades there has been a much faster development of basic information and theory than during the decades before. When I came to contribute to this work the famous Julius Bartels, then editor of the geophysical part, told me that Vol. 49 should certainly take into account the results of the "International Geophysical Year" 1957/58 (I. G. Y. ), and that we had better wait until these were accessible than produce a kind of information which might be obsolete in a short time.

Atmospheric Structure in the Lower Thermosphere

Atmospheric Structure in the Lower Thermosphere
Author: K. S. W. Champion
Publisher:
Total Pages: 56
Release: 1965
Genre: Atmosphere, Upper
ISBN:

This review constitutes a revision and up-dating of the report, Atmospheric Structure and its Variations in the Lower Thermosphere (AD-417 201). It has been prepared for inclusion as an appendix in the proposed new edition of the COSPAR International Reference Atmosphere (CIRA). New density data presented and discussed include the results of four falling-sphere density measurements made at White Sands, New Mexico, and densities deduced from drag effects on Explorer XVII and other satellites. The satellite density data is compared with the predictions of several models of Jacchia and Harris and Priester. Temperature data include revised values deduced by Blamont from Doppler broadening of sodium and potassium resonance lines. The new values are in better agreement with theoretical models than the earlier results. Recent composition results include number densities of O2, N2 and O calculated from ultraviolet absorption measurements by Hinteregger, and values of mean molecular mass from Explorer XVII and the rocket measurements of Nier and Schaefer. (Author).