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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Volume 17, issue 17
Atmos. Chem. Phys., 17, 10837–10854, 2017
https://doi.org/10.5194/acp-17-10837-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 17, 10837–10854, 2017
https://doi.org/10.5194/acp-17-10837-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 14 Sep 2017

Research article | 14 Sep 2017

Oxygenated volatile organic carbon in the western Pacific convective center: ocean cycling, air–sea gas exchange and atmospheric transport

Cathleen Schlundt et al.

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Cathleen Schlundt on behalf of the Authors (28 Jul 2017)  Author's response    Manuscript
ED: Reconsider after minor revisions (Editor review) (04 Aug 2017) by Laurens Ganzeveld
AR by Cathleen Schlundt on behalf of the Authors (09 Aug 2017)  Author's response    Manuscript
ED: Publish subject to technical corrections (10 Aug 2017) by Laurens Ganzeveld
Publications Copernicus
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Short summary
For the first time, oxygenated volatile organic carbon (OVOC) in the ocean and overlaying atmosphere in the western Pacific Ocean has been measured. OVOCs are important for atmospheric chemistry. They are involved in ozone production in the upper troposphere (UT), and they have a climate cooling effect. We showed that phytoplankton was an important source for OVOCs in the surface ocean, and when OVOCs are emitted into the atmosphere, they could reach the UT and might influence ozone formation.
For the first time, oxygenated volatile organic carbon (OVOC) in the ocean and overlaying...
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