Skip to main content

Thank you for visiting nature.com. You are using a browser version with limited support for CSS. To obtain the best experience, we recommend you use a more up to date browser (or turn off compatibility mode in Internet Explorer). In the meantime, to ensure continued support, we are displaying the site without styles and JavaScript.

  • Letter
  • Published:

Observations of the sodium layer at high latitudes in summer

Abstract

At altitudes between 80 and 100 km the upper atmosphere contains a layer of free sodium atoms presumably maintained by the almost continuous inflow and vaporization of cosmic dust particles. This sodium layer has been studied by ground-based photometers and lidar (laser radar), rocket-borne instrumentation, and satellite-borne photometers. Sodium measurements have been carried out at low, middle and high geographic latitudes. Lidar observations show that the peak of the layer commonly occurs close to the altitude of 90 km, with maximum densities of ˜5,000 atoms cm−3. In the 1960s photometric measurements established that the sodium layer shows seasonal variations which become more pronounced towards high latitudes (for a review of these early measurements, see ref. 1). Later lidar measurements yielded the following ratios of midsummer over midwinter column densities: 4.5 to 1 at 40° N (ref. 2), 3 to 1 at 44° N (ref. 3), and 6 to 1 at 51° N (ref. 4). Polar latitudes, however, are constantly sunlit in summer and the measurement of Na density profiles under these particular conditions have not yet been possible by ground-based methods. The state of our theoretical understanding of the Na layer has recently been reviewed by Kirchhoff5. Here we report on results of the first lidar measurements of the Na layer performed at polar latitudes in summer. Our sodium lidar instrument located at the And0ya Rocket Range, Norway (69° N, 16° E) gave measurements over ten days during July 1986 and July 1987. We find the sodium layer confined entirely to the lower thermosphere. The mean values for the layer parameters are as follows: the sodium column density is 6×l08cm−2; the number density at the layer peak is 1.2×103 cm−3; the altitude of the layer peak is 93 km, and the halfwidth of the layer is 6 km. Comparing these values with previous lidar measurements made at the same site in winter we obtain the following ratio of winter to summer densities: 10 to 1 for the sodium column density and 5 to 1 for the sodium number density at the layer peak.

This is a preview of subscription content, access via your institution

Access options

Buy this article

Prices may be subject to local taxes which are calculated during checkout

Similar content being viewed by others

References

  1. Hunten, D. M. Space Sci. Rev. 6, 493–573 (1967).

    Article  ADS  CAS  Google Scholar 

  2. Gardner, C. S., Voelz, D. G., Sechrichst, Jr, C. F. & Segal, A. C. J. geophys. Res. 91, 13659–13673 (1986).

    Article  ADS  Google Scholar 

  3. Megie, G., Bos, F., Blamont, J. E. & Chanin, M. L. Planet Space Sci. 26, 27–35 (1978).

    Article  ADS  CAS  Google Scholar 

  4. Gibson, A. J. & Sanford, M. C. W. J. atmos. terr. Phys. 33, 1675–1684 (1971).

    Article  ADS  Google Scholar 

  5. Kirchhoff, V. W. J. H. Can. J. Phys. 64, 1664–1672 (1986).

    Article  ADS  CAS  Google Scholar 

  6. von Zahn, U. & Neuber, R. Beiträge Phys. Atmos. 60, 294–304 (1987).

    ADS  Google Scholar 

  7. von Zahn, U., von der Gathen, P. & Hansen, G. Geophys. Res. Lett. 14, 76–79 (1987).

    Article  ADS  CAS  Google Scholar 

  8. von Zahn, U. & Hansen, T. J. atmos. terr. Phys. (in the press).

  9. von Zahn, U. & Tilgner, C. Eur. Space Ag. Symp. Proc. SP-270, 107–112 (1987).

    Google Scholar 

  10. Witt, G., Stegman, J. & Wood, H. in ‘Methods of Measurements and Results of Lower Ionosphere Structure’ (ed. K. Rawer) 431–445 (Akademie-Verlag, Berlin, 1974).

    Google Scholar 

  11. Simonich, D. M., Clemesha, B. R. & Kirchhoff, V. W. J. H. J. geophys. Res. 84, 1543–1550 (1979).

    Article  ADS  CAS  Google Scholar 

  12. Gardner, C. S., Senft, D. C., Kwon, K. H. & Sechrichst, C. F. Jr. Nature (submitted).

  13. Gadsden, M. Ann. Geophys. 26, 141–150 (1970).

    CAS  Google Scholar 

  14. Hunten, D. M. Geophys. Res. Lett. 8, 369–372 (1981).

    Article  ADS  CAS  Google Scholar 

  15. Swider, W. Geophys. Res. Lett. 12, 589–591 (1985).

    Article  ADS  CAS  Google Scholar 

  16. Hunten, D. M., Turco, R. P. & Toon, O. B. J. atmos. Sci. 37, 1342–1357 (1980).

    Article  ADS  CAS  Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

von Zahn, U., Hansen, G. & Kurzawa, H. Observations of the sodium layer at high latitudes in summer. Nature 331, 594–596 (1988). https://doi.org/10.1038/331594a0

Download citation

  • Received:

  • Accepted:

  • Issue Date:

  • DOI: https://doi.org/10.1038/331594a0

This article is cited by

Comments

By submitting a comment you agree to abide by our Terms and Community Guidelines. If you find something abusive or that does not comply with our terms or guidelines please flag it as inappropriate.

Search

Quick links

Nature Briefing

Sign up for the Nature Briefing newsletter — what matters in science, free to your inbox daily.

Get the most important science stories of the day, free in your inbox. Sign up for Nature Briefing