Articles | Volume 17, issue 7
https://doi.org/10.5194/bg-17-1877-2020
https://doi.org/10.5194/bg-17-1877-2020
Research article
 | 
07 Apr 2020
Research article |  | 07 Apr 2020

Is deoxygenation detectable before warming in the thermocline?

Angélique Hameau, Thomas L. Frölicher, Juliette Mignot, and Fortunat Joos

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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (09 Dec 2019) by Kenneth Rose
ED: Reconsider after major revisions (10 Dec 2019) by Kenneth Rose
AR by Angélique Hameau on behalf of the Authors (06 Jan 2020)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (09 Jan 2020) by Kenneth Rose
RR by M. Li (27 Jan 2020)
RR by Anonymous Referee #3 (05 Feb 2020)
ED: Publish subject to technical corrections (13 Feb 2020) by Kenneth Rose
ED: Publish subject to technical corrections (13 Feb 2020) by Katja Fennel (Co-editor-in-chief)
AR by Angélique Hameau on behalf of the Authors (18 Feb 2020)  Author's response   Manuscript 
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Short summary
Ocean deoxygenation and warming are observed and projected to intensify under continued greenhouse gas emissions. Whereas temperature is considered the main climate change indicator, we show that in certain regions, thermocline doxygenation may be detectable before warming.
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