Abstract
Nitrous oxide is an important tracer of transport, as well as the ultimate source gas for NOx in the stratosphere. Its calculated chemical lifetime in the troposphere and lower stratosphere is longer than transport timescales worldwide, so that its mixing ratio is not expected to be strongly dependent on latitude or season. However, we have now made frequent measurements of stratos-pheric N2O using the Stony Brook millimetre-wave remote sensing spectrometer at McMurdo Station, Antarctica, as part of the investigation of the 'ozone hole'1 and find N2O mixing ratios that are less than 1/5 at 20km, and less than 1/10 at 25km compared to values measured during the Antarctic summer. The observed mixing ratios are also much less than those predicted by global-scale models of stratospheric chemistry and dynamics. As the N2O signal remained very weak when McMurdo was at the edges of the ozone hole and snowed no signs of recovering during October, we conclude that the geographical and temporal extent of the region of low N2O is comparable to, or greater than that of the ozone hole. Our results argue against theories that require springtime upwelling to explain the Antarctic ozone hole, and suggest that the air in the Antarctic lower stratosphere during late winter and early spring has been subjected to considerable down-ward transport.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 51 print issues and online access
$199.00 per year
only $3.90 per issue
Buy this article
- Purchase on Springer Link
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
Similar content being viewed by others
References
World Meteorological Organization/NASA, The Stratosphere, 1981; Theory and Measurement (Report No. 16 of the WMO Global Ozone Research and Monitoring Project, NASA Headquarters, Washington, 1986).
Farman, J. C., Gardiner, B. G. & Shanklin, J. D. Nature 315, 207–210 (1985).
Goldan, P. D., Kuster, W. C., Albritton, D. L., & Schmeltekopf, A. L. J. geophys. Res. 85, 413–423 (1980) 86, 5385–5386 (correction) (1981).
Vedder, J. F., Inn, E. C. Y., Tyson, B. J., Boitnott, C. A. & O'Hara, D. J. geophys. Res. 86, 7363–7368 (1981).
Jones, R. L. & Pyle, J. A. J. geophys. Res. 89, 5263–5279 (1984).
Mahlman, J. D., Levy, H. II & Moxim, W. J. J. geophys. Res. 91, 2681–2686 (1986).
Ko, M. K. W., Tung, K. K., Weinstein, D. K. & Sze, N. D. J. geophys. Res. 90, 2313–2329 (1985).
Solomon, S. & Garcia, R. R. J. geophys. Res. 89, 11633–11644 (1984).
Schmeltekopf, A. L. et al. J. Atmos. Sci. 34, 729–736 (1977).
Goldman, A., Fernald, F. G., Murcray, F. J., Murcray, F. H. & Murcray, D. G. J. quant. Spect. Rad. Trans. 29, 189–204 (1983).
Parrish, A., deZafra, R. L., Solomon, P. M. & Barrett, J. W. Radio Sci. (in the press).
Hofmann, D. J., Harder, J. W., Rolf, S. R. & Rosen, J. M. Nature 326, 59 (1987).
deZafra, R. L. et al. Nature 328, 408–411 (1987).
Solomon, P. M. et al. Nature 328, 411–414 (1987).
Connor, B. J. et al. Geophys. Res. Lett. 14, 1254 (1987).
Tung, K. K., Ko, M. K. W., Rodriguez, J. M. & Sze, N. D. Nature 322, 811 (1986).
Tung, K. K. Geophys. Res. Lett. 13, 1308–1311 (1986).
Connor, B. et al. J. geophys. Res. 92, 13221–13230 (1987).
Mount, G., Sanders, R., Schmeltekopf, A. & Solomon, S. J. geophys. Res. 92, 8320–8327 (1987).
Krueger, A. J., Schoeberl, M. R. & Stolarski, R. S. Geophys. Res. Lett. 14, 527–530 (1987).
Mahlman, J. D. & Fels, S. B. Geophys. Res. Lett. 13, 1316–1319 (1986).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Parrish, A., de Zafra, R., Jaramillo, M. et al. Extremely low N2O concentrations in the springtime stratosphere at McMurdo Station, Antarctica. Nature 332, 53–55 (1988). https://doi.org/10.1038/332053a0
Received:
Accepted:
Issue Date:
DOI: https://doi.org/10.1038/332053a0
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.