Abstract
THE problem of the relation of the occurrence of auroræ in the northern and southern hemispheres is one of considerable importance to the theories of auroral formation. Hitherto, the assessment of these occurrences has been handicapped by the difficulties of the collection of simultaneous visual observations in the arctic and antarctic regions, and by the fact that in any event auroræ occur on at least 75 per cent of nights in the zones of maximum activity in which the visual observations tend to be concentrated. So far the evidence for the simultaneity of the occurrences has been largely of a statistical nature1. The Royal Society's Expedition to Halley Bay has provided an opportunity for a simultaneous study of the aurora australis and borealis by the radio-echo technique, and a preliminary account of the results is given in this communication.
Similar content being viewed by others
References
Little, B. E., and Shrum, C. M., Trans. Roy. Soc. Canada, 44 (III), 3 (1950).
Lovell, A. C. B., I.G.Y. Annals, 3, Part IV, 337 (1957).
Bullough, K., and Kaiser, T. R., J. Atmos. Terr. Phys., 5, 189 (1954).
Vestine, E. H., and Snyder, E. J., Terr. Mag., 50, 122 (1945).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
HARRISON, D., WATKINS, C. A Comparison of Radio Echoes from the Aurora Australis and Aurora Borealis. Nature 182, 43–44 (1958). https://doi.org/10.1038/182043a0
Issue Date:
DOI: https://doi.org/10.1038/182043a0
- Springer Nature Limited