Summary
Calculated values of the gaseous atmospheric absorption are presented for the frequency range 100 to 50,000 Mc at elevations above ground up to at least 130,000 feet, for average conditions during February and August at Bismarck, N. D. and Washington, D. C. Total radio path absorptionsare presented for tropospheric forward scatter communication links for distances of 100, 300 and 1000 miles. The total path absorptions were calculated by summing the absorption contributed by each portion of the atmosphere traversed by a radio ray passing from a 60 foot parabolic antenna resting on the ground to the scattering center and then to a similar receiving antenna. A correlation of total path absorption with the surface value of absolute humidity is developed, thus providing estimates of the range of absorption values in different geographic areas. Maps of average absolute humidity for the world are presented. Previous work on rain absorption is then combined with the present study to provide estimates of the radio power loss due to absorption expected to be exceeded 1 per cent of the time.
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Portions of this paper were presented in preliminary form at the Symposium on Communication by Scatter Techniques-George Washington University, Washington, D. C., November 14 and 15, 1955.
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Bean, B.R., Abbott, R. Oxygen and water vapor absorption of radio waves in the atmosphere. Geofisica Pura e Applicata 37, 127–144 (1957). https://doi.org/10.1007/BF01988856
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DOI: https://doi.org/10.1007/BF01988856