Hostname: page-component-78c5997874-v9fdk Total loading time: 0 Render date: 2024-11-18T21:51:11.764Z Has data issue: false hasContentIssue false
  • English
  • Français

A Method of Continuous Observation of the Equivalent Height of the Kennelly-Heaviside Layer

Published online by Cambridge University Press:  24 October 2008

E. L. C. White
E. L. C. White
Affiliation:
Sidney Sussex College
Get access Rights & Permissions [Opens in a new window]

Extract

A development of the “echo” method of observation of the height of the Kennelly-Heaviside layer is described. Short wave-trains of radiation lasting sec. are transmitted at regular sec. intervals, and observed stroboscopically, together with their echoes, by means of a cathode ray oscillograph. Details of the transmitting and receiving apparatus are given. The rapid fluctuation in amplitude of the echoes is easily studied by this method.

Type
Research Article
Information
Mathematical Proceedings of the Cambridge Philosophical Society , Volume 27 , Issue 3 , July 1931 , pp. 445 - 450
Copyright
Copyright © Cambridge Philosophical Society 1931

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

* Breit, G. and Tuve, M. A., Phys. Rev. vol. 28, 554 (1926)CrossRefGoogle Scholar; Tuve, and Dahl, , Proc. Inst. Rod. Eng. vol. 16, 794 (1928)Google Scholar and several subsequent papers in P.I.R.E.

† Appleton, E. V., Proc. Phys. Soc. vol. 41, p. 43 (1928)CrossRefGoogle Scholar, and vol. 42, p. 321 (1930).

* Goubau, G., Physikal. Zeitschr. vol. 31, no. 7 (1930)Google Scholar.