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Ozone-rich transients in the upper equatorial Atlantic troposphere

Nature volume 388, pages 661–663 (1997)Cite this article

Abstract

High concentrations of ozone are found in the Earth's stratosphere, but strong stratification suppresses efficient exchange of this ozone-rich air with the underlying troposphere. Upward transport of tropospheric trace constituents occurs mainly through equatorial deep convective systems. In contrast, significant downward transport of ozone-rich stratospheric air is thought to take place only outside the tropics by exchange processes in upper-level fronts associated with strong distortions of the tropopause1. Ozone within the tropical troposphere is assumed to originate predominantly from ground-based emissions of ozone precursors, particularly from biomass burning2, rather than from a stratospheric source. Recent measurements of ozone in the upper troposphere in convective regions over the Pacific Ocean3 indeed reveal near-zero concentrations. Here we present sharply contrasting observations: ozone-rich (100–500 parts per billion by volume) transients were frequently encountered by specially equipped commercial aircraft at a cruising altitude of 10–12 km (in the upper troposphere) in the vicinity of strong convective activity over the equatorial Atlantic Ocean. This strongly suggests that the input of stratospheric ozone into the troposphere can take place in the tropics. We suggest that this transport occurs either by direct downward movement of air masses or by quasi-isentropic transport from the extratropical stratosphere.

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Figure 1: Time series of: a, ozone mixing ratio; b, water vapour mixing ratio; c, temperature; d, barometric flight altitude variations; e, wind direction; f, wind speed.
Figure 2: Expanded-scale view of part of the ozone time series in Fig. 1a.

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Acknowledgements

We thank Air France A340 pilot De Boysson for eye-witness information from MOZAIC flights in the tropics; we also acknowledge discussions with many of our colleagues. On behalf of the MOZAIC programme, we thank Air France, Lufthansa, Austrian Airlines and Sabena, who agreed to carry the MOZAIC equipment free of charge. This work was supported by the European Commission DG XII and Centre National de la Recherche Scientifique (CNRS-INSU); satellite images were made available by NOAA-SAA.

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Authors and Affiliations

  1. Laboratoire d'Aérologie (UMR CNRS/UPS 5560), OMP, 14, Avenue Edouard Berlin, 31400, Toulouse, France

    K. Suhre, J.-P. Cammas, P. Nédelec, R. Rosset & A. Marenco

  2. Research Centre Jülich, Institute for Chemistry of the Polluted Atmosphere (ICG-2), PO Box 1913, 52425, Jülich, Germany

    H. G. J. Smit

Authors
  1. K. Suhre
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  2. J.-P. Cammas
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  4. R. Rosset
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  5. A. Marenco
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  6. H. G. J. Smit
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Correspondence to K. Suhre.

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Suhre, K., Cammas, JP., Nédelec, P. et al. Ozone-rich transients in the upper equatorial Atlantic troposphere. Nature 388, 661–663 (1997). https://doi.org/10.1038/41749

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