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Extremely low N2O concentrations in the springtime stratosphere at McMurdo Station, Antarctica

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.

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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

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