Articles | Volume 17, issue 12
https://doi.org/10.5194/bg-17-3247-2020
https://doi.org/10.5194/bg-17-3247-2020
Research article
 | 
26 Jun 2020
Research article |  | 26 Jun 2020

Assessing the potential for non-turbulent methane escape from the East Siberian Arctic Shelf

Matteo Puglini, Victor Brovkin, Pierre Regnier, and Sandra Arndt

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Status: closed
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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: Reconsider after major revisions (26 Nov 2019) by Alexey V. Eliseev
AR by Anna Wenzel on behalf of the Authors (06 Apr 2020)  Author's response
ED: Referee Nomination & Report Request started (06 Apr 2020) by Alexey V. Eliseev
RR by Volker Brüchert (02 May 2020)
ED: Publish subject to minor revisions (review by editor) (03 May 2020) by Alexey V. Eliseev
AR by Matteo Puglini on behalf of the Authors (17 May 2020)  Author's response    Manuscript
ED: Publish as is (19 May 2020) by Alexey V. Eliseev
AR by Matteo Puglini on behalf of the Authors (27 May 2020)  Author's response    Manuscript
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Short summary
A reaction-transport model to assess the potential non-turbulent methane flux from the East Siberian Arctic sediments to water columns is applied here. We show that anaerobic oxidation of methane (AOM) is an efficient filter except for high values of sedimentation rate and advective flow, which enable considerable non-turbulent steady-state methane fluxes. Significant transient methane fluxes can also occur during the building-up phase of the AOM-performing biomass microbial community.
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