How stratospheric are deep stratospheric intrusions? LUAMI 2008

Trickl, Thomas; Vogelmann, Hannes; Fix, Andreas; Schäfler, Andreas; Wirth, Martin; Calpini, Bertrand; Levrat, Gilbert; Romanens, Gonzague; Apituley, Arnoud; Wilson, Keith M.; Begbie, Robert; Reichardt, Jens; Vömel, Holger; Sprenger, Michael

doi:https://doi.org/10.5194/acp-16-8791-2016

Articles | Volume 16, issue 14

https://doi.org/10.5194/acp-16-8791-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/acp-16-8791-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 16, issue 14

Research article

|

19 Jul 2016

Research article |

| 19 Jul 2016

How stratospheric are deep stratospheric intrusions? LUAMI 2008

Thomas Trickl, Hannes Vogelmann, Andreas Fix, Andreas Schäfler, Martin Wirth, Bertrand Calpini, Gilbert Levrat, Gonzague Romanens, Arnoud Apituley, Keith M. Wilson, Robert Begbie, Jens Reichardt, Holger Vömel, and Michael Sprenger

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Final revised paper (published on 19 Jul 2016)
Preprint (discussion started on 13 Apr 2016)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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- Supplement

RC1: 'Review report', Anonymous Referee #2, 20 Apr 2016
RC2: 'review', Anonymous Referee #1, 11 May 2016
AC1: 'LUAMI', Thomas Trickl, 11 Jun 2016
AC2: 'LUAMI', Thomas Trickl, 11 Jun 2016

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

AR by Anna Wenzel on behalf of the Authors (21 Jun 2016) Author's response Manuscript

ED: Publish subject to technical corrections (08 Jul 2016) by Evangelos Gerasopoulos

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.