Abstract
EXPERIMENTS made to determine the effective height of the Heaviside layer have shown extremely varied results, and it has been clear that, in order to obtain any idea of the normal state of the upper atmospheric ionisation, it is unsatisfactory to take observations at widely spaced intervals of time. Continuous automatic records of effective height are required.
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References
Bureau of Standards J. Research, Nov. 1931, 783.
E. L. C. White, "Method of continuous observation of the Heaviside Layer." Proc. Camb. Phil. Soc., 27, 445; 1931.
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WHITE, E. Automatic Recording of Heaviside Layer Heights. Nature 129, 579 (1932). https://doi.org/10.1038/129579b0
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DOI: https://doi.org/10.1038/129579b0
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