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Wilson Cloud formation by low-altitude nuclear explosions

Published online by Cambridge University Press:  12 April 2006

R. E. Waltz
Affiliation:
Visidyne, Inc., Burlington, Massachusetts 01803 Present address: General Atomic Company, San Diego, California 92138.

Abstract

A model of Wilson Cloud formation following a low-altitude nuclear detonation is developed. It is shown that, for detonation yields between 10−3 kt and 100 kt, simple scaling laws characterize the evolution and physical properties of the Wilson Cloud.

Type
Research Article
Copyright
© 1978 Cambridge University Press

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References

Bethe, H. A. et al. 1949 Blast wave. Los Alamos Sci. Lab. Rep. LA-2000.Google Scholar
Glasstone, S. 1962 Effects of Nuclear Weapons, pp. 4749. U.S. Dept. Defense.
Mason, B. J. 1971 The Physics of Clouds, pp. 122125. Oxford: Clarendon Press.
Needham, C. E. et al. 1973 Nuclear blast standard (1 kt). Air Force Weapons Lab. Tech. Rep. AFWL-TR-73-55.Google Scholar
Sedov, L. I. 1959 Similarity and Dimensional Methods in Mechanics, pp. 238251. Academic Press.