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Volume 4, issue 5
Atmos. Chem. Phys., 4, 1427–1442, 2004
https://doi.org/10.5194/acp-4-1427-2004
© Author(s) 2004. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.

Special issue: Trace gas transport in the tropopause region (SPURT)

Atmos. Chem. Phys., 4, 1427–1442, 2004
https://doi.org/10.5194/acp-4-1427-2004
© Author(s) 2004. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.

  27 Aug 2004

27 Aug 2004

Seasonality and extent of extratropical TST derived from in-situ CO measurements during SPURT

P. Hoor1,2, C. Gurk2, D. Brunner1, M. I. Hegglin1, H. Wernli1,3, and H. Fischer2 P. Hoor et al.
  • 1Institute for Atmospheric and Climate Science, Swiss Federal Institute of Technology, Zürich, Switzerland
  • 2Max Planck Institute for Chemistry, Air Chemistry, Mainz, Germany
  • 3Institute for Atmospheric Physics, University of Mainz, Germany

Abstract. We present airborne in-situ trace gas measurements which were performed on eight campaigns between November 2001 and July 2003 during the SPURT-project (SPURenstofftransport in der Tropopausenregion, trace gas transport in the tropopause region). The measurements on a quasi regular basis allowed an overview of the seasonal variations of the trace gas distribution in the tropopause region over Europe from 35°-75°N to investigate the influence of transport and mixing across the extratropical tropopause on the lowermost stratosphere.

From the correlation of CO and O3 irreversible mixing of tropospheric air into the lowermost stratosphere is identified. The CO distribution indicates that transport and subsequent mixing of tropospheric air across the extratropical tropopause predominantly affects a layer, which closely follows the shape of the local tropopause. In addition, the seasonal cycle of CO2 illustrates the strong coupling of that layer to the extratropical troposphere. Both, horizontal gradients of CO on isentropes as well as the CO-O3-distribution in the lowermost stratosphere reveal that the influence of quasi-horizontal transport and subsequent mixing weakens with distance from the local tropopause. The mixing layer extends to about 25 K in potential temperature above the local tropopause exhibiting only a weak seasonality.

However, at large distances from the tropopause a significant influence of tropospheric air is still evident. The relation between N2O and CO2 indicates that a significant contribution of air originating from the tropical tropopause contributes to the background air in the extratropical lowermost stratosphere.

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