DocumentCode :
1224608
Title :
A Theory on Radar Reflections from the Lower Atmosphere
Author :
Gordon, W.E.
Author_Institution :
Formerly, Electrical Engineering Research Laboratory, University of Texas, Austin, Tex.; now, School of Electrical Engineering, Cornell University, Ithaca, N.Y.
Volume :
37
Issue :
1
fYear :
1949
Firstpage :
41
Lastpage :
43
Abstract :
A theory is presented, supported by several sample sets of data, which indicate that the curious phenomenon dubbed "angels" (radar reflections from the lower atmosphere) may be attributed to sharp changes in the dielectric constant. The required magnitudes of the changes are computed from reflection theory and compared to sample meteorological data obtained from rapid-response instruments. The near-discontinuities in the dielectric constant are produced by atmospheric turbulence. It is proposed that the observed radar reflections are the result of turbulent motion in the lower atmosphere.
Keywords :
Acoustic reflection; Atmosphere; Atmospheric measurements; Dielectric constant; Dielectric measurements; Instruments; Meteorological radar; Meteorology; Radar detection; Radar theory;
fLanguage :
English
Journal_Title :
Proceedings of the IRE
Publisher :
ieee
ISSN :
0096-8390
Type :
jour
DOI :
10.1109/JRPROC.1949.233277
Filename :
1697836
Link To Document :
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