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The Mesopause Region of the Ionosphere
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  • Letter
  • Published: 07 May 1960

The Mesopause Region of the Ionosphere

  • J. D. WHTTEHEAD1 

Nature volume 186, page 461 (1960)Cite this article

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  • 1 Citations

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Abstract

IN a recent communication, Gregory1 suggested that the presence of free electrons at heights in the atmosphere between 80 and 90 km. may be due to the photo-ionization of dust which accumulates at the mesopause. Rocket measurements2 have shown that the electron density at this height is about 1,000 el./c.c. on a normal day. This is also the order of magnitude of electron density required to account for the absorption of radio waves in the D region. It is of interest to see whether photo-ionization of the dust is able to give this observed electron density.

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References

  1. Gregory, J. B., Nature, 181, 753 (1958).

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  2. Seddon, J. C., J. Geophys. Res., 63, 209 (1958).

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  3. Ludlam, F. H., Tettus, 9, 341 (1957).

    Google Scholar 

  4. Byram, E. T., Chubb, T., Friedman, H., and Gailar, N., Phys. Rev., 91, 1278 (1953).

    Article  ADS  CAS  Google Scholar 

  5. Bates, D. R., and Seaton, M. J., Proc. Phys. Soc., 63, B, 129 (1950).

    Article  ADS  Google Scholar 

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Authors and Affiliations

  1. Physics Department, Otago University, Dunedin, New Zealand

    J. D. WHTTEHEAD

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  1. J. D. WHTTEHEAD
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WHTTEHEAD, J. The Mesopause Region of the Ionosphere. Nature 186, 461 (1960). https://doi.org/10.1038/186461a0

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  • Issue date: 07 May 1960

  • DOI: https://doi.org/10.1038/186461a0

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