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Ubiquity of quasi-horizontal layers in the troposphere

Abstract

Fine laminar structures in the atmosphere have been described previously1,2,3,4,5,6,7,8,9, but their characterization has been limited. The modern global coverage of aircraft flights offers an opportunity to provide such a characterization, and examine the ubiquity of such structures, in space and time. Research aircraft measuring vertical profiles of atmospheric chemical constituents frequently discern quasi-horizontal atmospheric layers with mean thicknesses of the order of 1 km and mean altitudes between 5 and 7 km (refs 10,11,12). These layers can be characterized and categorized by various combinations of ozone, water vapour, carbon monoxide and methane deviations from background profiles. Five commercial aircraft have been recently equipped to measure water vapour and ozone concentrations, and automatically collect vertical profile information on landing and take-off (refs 13,14,15). Here we synthesize measurements from both research and commercial flights and demonstrate the ubiquity in space and time of four layer types (as categorized by their chemical signatures). Up to one-fifth of the lowest 12 km of the atmosphere is occupied by such layers. We suggest that this universality reflects basic characteristics of the atmosphere hitherto unexplored, with potential implications for present understanding of a wide variety of dynamic and chemical atmospheric processes.

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Figure 1: Maps of regions sampled.
Figure 2: Radiative heating rate profiles for an O3−/H2O+ layer versus a simulated background, both without clouds.

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References

  1. Danielsen, E. F. The laminar structure of the atmosphere and its relation to the concept of a tropopause. Arch. Meteorol. Geophys. Bioklimatol. 11, 293–332 (1959).

    Article  Google Scholar 

  2. Danielsen, E. F. Stratospheric–tropospheric exchange based on ozone and potential vorticity. J. Atmos. Sci. 25, 502–518 (1968).

    Article  ADS  Google Scholar 

  3. Corby, G. A. Apreliminary study of atmospheric waves using radiosonde data. Q. J. R. Meteorol. Soc. 83, 49–60 (1957).

    Article  ADS  Google Scholar 

  4. Reid, S. J. An observational study of lee waves using radiosonde data. Tellus 24, 593–596 (1982).

    ADS  Google Scholar 

  5. Shutts, G. J., Kitchen, M. & Hoare, P. H. Alarge amplitude gravity wave in the lower stratosphere detected by radiosonde. Q. J. R. Meteorol. Soc. 114, 579–594 (1988).

    Article  ADS  Google Scholar 

  6. Bethan, S., Vaughan, G. & Reid, S. J. Acomparison of ozone and thermal tropopause heights and the impact of tropopause definition on quantifying the ozone content of the troposphere. Q. J. R. Meteorol. Soc. 122, 929–944 (1996).

    Article  ADS  Google Scholar 

  7. Sawyer, J. S. Quasi-periodic wind variations with height in the lower stratosphere. Q. J. R. Meteorol. Soc. 87, 24–33 (1961).

    Article  ADS  Google Scholar 

  8. Newell, R. E., Mahoney, J. R. & Lenhard, R. . W. J Apilot study of small-scale wind variations in the stratosphere and mesosphere. Q. J. R. Meteorol. Soc. 92, 41–54 (1966).

    Article  ADS  Google Scholar 

  9. Gage, K. S. & Balsley, B. B. MST radar studies of wind and turbulence in the middle atmosphere. J. Atmos. Terr. Phys. 46, 739–753 (1984).

    Article  ADS  Google Scholar 

  10. Newell, R. E. et al. Vertical fine-scale atmospheric structure measured from NASA DC-8 during PEM-West A. J. Geophys. Res. 101, 1943–1960 (1996).

    Article  ADS  CAS  Google Scholar 

  11. Wu, Z. -X. et al. Atmospheric layers measured from the NASA DC-8 during PEM-West B and comparison with PEM-West A. J. Geophys. Res. 102, 28353–28365 (1997).

    Article  ADS  CAS  Google Scholar 

  12. Stoller, P. et al. Measurements of atmospheric layers from the NASA DC-8 and P-3B aircraft during PEM-Tropics A. J. Geophys. Res.(in the press).

  13. Thouret, V., Marenco, A., Logan, J. A., Nédélec, P. & Grouhel, C. Comparisons of ozone measurements from the MOZAIC airborne program and the ozone sounding network at eight locations. J. Geophys. Res. 103, 25695–25720 (1998).

    Article  ADS  CAS  Google Scholar 

  14. Marenco, A. et al. Measurement of ozone and water vapour by Airbus in-service aircraft: The MOZAIC airborne program, an overview. J. Geophys. Res. 103, 25631–25642 (1998).

    Article  ADS  CAS  Google Scholar 

  15. Helten, M. et al. Calibration and performance of automatic compact instrumentation for the measurement of relative humidity from passenger aircraft. J. Geophys. Res. 103, 25643–25652 (1998).

    Article  ADS  CAS  Google Scholar 

  16. Hoell, J. M. et al. Pacific exploratory mission-west A (PEM-West A): September–October 1991. J. Geophys. Res. 101, 1641–1653 (1996).

    Article  ADS  CAS  Google Scholar 

  17. Hoell, J. M. et al. The Pacific exploratory mission-west phase B: February–March, 1994. J. Geophys. Res. 102, 28223–28239 (1997).

    Article  ADS  CAS  Google Scholar 

  18. Hoell, J. M. et al. The Pacific exploratory mission in the tropical Pacific: PEM-Tropics A, August–September, 1996. J. Geophys. Res.(in the press).

  19. Hoffman, R. N. A Computer Program which Calculates Radiative Fluxes and Heating Rates in Model Atmospheres(Sci. Rep. No. 4, Dept Meteorol. Phys. Oceanogr., MIT, Cambridge, MA, (1981).

    Google Scholar 

  20. Brasseur, GP., Müller, J. F. & Granier, C. Atmospheric impact of NOx emissions by subsonic aircraft: A three dimensional model study. J. Geophys. Res. 101, 1423–1428 (1996).

    Article  ADS  CAS  Google Scholar 

  21. Edouard, S., Legras, B., Lefèvre, F. & Eymard, R. The effect of small-scale inhomogeneities on ozone depletion in the Arctic. Nature 384, 444–447 (1996).

    Article  ADS  CAS  Google Scholar 

  22. Newell, R. E., Zhu, Y., Browell, E. V., Read, W. G. & Waters, J. W. Walker circulation and tropical upper tropospheric water vapor. J. Geophys. Res. 101, 1961–1974 (1996).

    Article  ADS  Google Scholar 

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Acknowledgements

We thank our PEM and MOZAIC colleagues for access to their data, Air France, Lufthansa, Austrian Airlines and Sabena for carrying the MOZAIC equipment, and the NASA GTE, ACMAP, and GSFC Research Assistantship programs for their support.

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Correspondence to Reginald E. Newell.

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Newell, R., Thouret, V., Cho, J. et al. Ubiquity of quasi-horizontal layers in the troposphere. Nature 398, 316–319 (1999). https://doi.org/10.1038/18642

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