Articles | Volume 16, issue 14
Atmos. Chem. Phys., 16, 8791–8815, 2016
Atmos. Chem. Phys., 16, 8791–8815, 2016

Research article 19 Jul 2016

Research article | 19 Jul 2016

How stratospheric are deep stratospheric intrusions? LUAMI 2008

Thomas Trickl et al.

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Cited articles

Ancellet, G., Pelon, J., Beekmann, M., Papayannis, A., and Megie, G.: Ground based lidar studies of ozone exchanges between the stratosphere and the troposphere, J. Geophys. Res., 96, 22401–22421, 1991.
Ancellet, G., Beekmann, M., and Papayannis, A.: Impact of a cutoff low development on downward transport of ozone in the the troposphere, J. Geophys. Res., 99, 3451–3468, 1994.
Apituley, A., Wilson, K. M., Potma, C., Volten, H., and de Graaf, M.: Performance Assessment and Application of Caeli – A high-performance Raman lidar for diurnal profiling of Water Vapour, Aerosols and Clouds, in: Proceedings of the 8th International Symposium on Tropospheric Profiling (ISTP2009), Delft, the Netherlands, 19–23 October 2009, edited by: Apituley, A., Russchenberg, H. W. J., and Monna, W. A. A., Contribution S06-O10, 4 pp., available at: (last access: 18 July 2016), 2009.
ATMOFAST: Atmosphärischer Ferntransport und seine Auswirkungen auf die Spurengaskonzentrationen in der freien Troposphäre über Mitteleuropa (Atmospheric Long-range Transport and its Impact on the Trace-gas Composition of the Free Troposphere over Central Europe), Project Final Report, Trickl, T., co-ordinator, Kerschgens, M., Stohl, A., and Trickl, T., subproject co-ordinators, funded by the German Ministry of Education and Research within the programme “Atmosphärenforschung 2000”, 130 pp., revised publication list available at: (last access: 18 July 2016), 2005 (in German).
Bithell, M., Vaughan, G., and Gray, L. J.: Persistence of stratospheric ozone layers in the troposphere, Atmos. Environ., 34, 2563–2570, 2000.
Short summary
A rather homogeneous deep stratospheric intrusion event was mapped by vertical sounding over central Europe and by model calculations along the transport path. The very low minimum H2O mixing ratios demonstrate almost negligible mixing with tropospheric air during the downward transport. The vertical distributions of O3 and aerosol were transferred from the source region to Europe without major change. A rather shallow outflow from the stratosphere was found.
Final-revised paper