A Study of the Nighttime Ionosphere and Its Reaction Rates
Author : William Swider (Jr.)
Publisher :
Page : 26 pages
File Size : 15,70 MB
Release : 1965
Category : Chemical reactions
ISBN :
Author : William Swider (Jr.)
Publisher :
Page : 26 pages
File Size : 15,70 MB
Release : 1965
Category : Chemical reactions
ISBN :
Author :
Publisher :
Page : 576 pages
File Size : 50,97 MB
Release :
Category : Aeronautics
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Author :
Publisher :
Page : 1576 pages
File Size : 35,41 MB
Release : 1966
Category : Government publications
ISBN :
Author : William Swider
Publisher :
Page : 28 pages
File Size : 24,23 MB
Release : 1977
Category : Auroras
ISBN :
E-region nitric oxide concentrations are known to be greater at high altitudes as compared to low- and midlatitudes. It is suggested that studies of electron concentration data from ionosondes and/or the Chatanika backscatter radar at night, and especially at sunrise, may be able to provide peak nitric oxide concentrations when aurora are determined to be absent. (Author).
Author : Air Force Cambridge Research Laboratories (U.S.)
Publisher :
Page : 88 pages
File Size : 13,72 MB
Release : 1967
Category : Atmosphere, Upper
ISBN :
The bibliography of AFCRL in-house technical reports lists all reports issued in the existing series. In addition, appendices list reports issued from 1962 to 1964 when series designations were not used, and reports issued in now-defunct series.
Author :
Publisher :
Page : 52 pages
File Size : 43,32 MB
Release : 1966-06
Category : Physical instruments
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Author :
Publisher :
Page : 760 pages
File Size : 17,31 MB
Release :
Category : Science
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Author :
Publisher :
Page : 328 pages
File Size : 45,78 MB
Release : 1966
Category : Science
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Author :
Publisher :
Page : 728 pages
File Size : 11,73 MB
Release : 1971
Category : Radio
ISBN :
Author : William Swider
Publisher :
Page : 32 pages
File Size : 26,90 MB
Release : 1974
Category : D region
ISBN :
The chemistry of the E-region is fairly well understood and even many of the dynamical complications of this region have been successfully modeled on individual bases. Some of the major remaining problems of this region are discussed, in particular the nitric oxide concentration, a gas affecting the ratio of the two major E-region ions, O2(+) and NO(+). The D-region is much simpler than the E-region from a dynamical point of view but extremely much more complex from a chemical standpoint. Recent results from a study of the D-region under bombardment by solar protons is emphasized.