Delivery of halogenated very short-lived substances from the west Indian Ocean to the stratosphere during the Asian summer monsoon

Fiehn, Alina; Quack, Birgit; Hepach, Helmke; Fuhlbrügge, Steffen; Tegtmeier, Susann; Toohey, Matthew; Atlas, Elliot; Krüger, Kirstin

doi:https://doi.org/10.5194/acp-17-6723-2017

Articles | Volume 17, issue 11

https://doi.org/10.5194/acp-17-6723-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/acp-17-6723-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 17, issue 11

Research article

|

08 Jun 2017

Research article |

| 08 Jun 2017

Delivery of halogenated very short-lived substances from the west Indian Ocean to the stratosphere during the Asian summer monsoon

Alina Fiehn, Birgit Quack, Helmke Hepach, Steffen Fuhlbrügge, Susann Tegtmeier, Matthew Toohey, Elliot Atlas, and Kirstin Krüger

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Final revised paper (published on 08 Jun 2017)
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Interactive discussion

Status: closed

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

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RC1: 'Referee comment on acp-2017-8', Anonymous Referee #1, 10 Feb 2017
- AC1: 'Author Comment to Reviewer 1', Alina Fiehn, 19 Apr 2017
RC2: 'Review', Anonymous Referee #2, 21 Mar 2017
- AC2: 'Author Comment to Reviewer 2', Alina Fiehn, 19 Apr 2017

Peer-review completion

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

AR by Alina Fiehn on behalf of the Authors (21 Apr 2017) Author's response Manuscript

ED: Publish as is (02 May 2017) by Jens-Uwe Grooß

AR by Alina Fiehn on behalf of the Authors (02 May 2017) Manuscript

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Short summary

Halogenated very short-lived substances (VSLSs) are naturally produced in the ocean and emitted to the atmosphere. In the stratosphere, these compounds can have a significant influence on the ozone layer and climate. During a research cruise in the west Indian Ocean, we found an important source region of halogenated VSLSs during the Asian summer monsoon. Modeling the transport from the ocean to the stratosphere we found two main pathways, one over the Indian Ocean and one over northern India.