DETERMINATION OF THE D-LAYER AIR CHEMISTRY FROM A DAYTIME, HIGH-ALTITUDE NUCLEAR EXPLOSION,
Abstract
Measurements of the magnitude and time dependence of X-ray induced absorption over Midway during the July 9, 1962, high-altitude nuclear explosion allowed us to infer bounds on the dissociative recombination coefficient alpha of the D-layer of the ionosphere. It is shown here that a daytime experiment would allow a unique determination of alpha. By combining the daytime data with the already available nighttime data, one could infer the in situ detachment rate of the daytime ionosphere. We find that a low-yield explosion (a few KT) is adequate for the purpose of the experiment. (Author)
Document Details
- Document Type
- Technical Report
- Publication Date
- Sep 01, 1965
- Accession Number
- AD0620952
Entities
People
- R. E. Lelevier
Organizations
- RAND Corporation