Exceptional summer warming leads to contrasting outcomes for methane cycling in small Arctic lakes of Greenland

Cadieux, Sarah B.; White, Jeffrey R.; Pratt, Lisa M.

doi:https://doi.org/10.5194/bg-14-559-2017

Articles | Volume 14, issue 3

https://doi.org/10.5194/bg-14-559-2017

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

https://doi.org/10.5194/bg-14-559-2017

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

Articles | Volume 14, issue 3

Research article

|

07 Feb 2017

Research article |

| 07 Feb 2017

Exceptional summer warming leads to contrasting outcomes for methane cycling in small Arctic lakes of Greenland

Sarah B. Cadieux, Jeffrey R. White, and Lisa M. Pratt

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Final revised paper (published on 07 Feb 2017)
Preprint (discussion started on 18 Jul 2016)

Interactive discussion

Status: closed

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

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- Supplement

RC1: 'Review of “The effect of warm summer 2012 on seasonal and annual methane dynamics in adjacent small lakes on the ice-free margin of Greenland”', Anonymous Referee #1, 15 Aug 2016
- AC1: 'Response to Review 1', Sarah Cadieux, 18 Oct 2016
RC2: 'Review', Anonymous Referee #2, 19 Aug 2016
- AC2: 'Response to Review 2', Sarah Cadieux, 18 Oct 2016

Peer-review completion

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

ED: Reconsider after major revisions (27 Oct 2016) by Gwenaël Abril

AR by Sarah Cadieux on behalf of the Authors (29 Dec 2016) Author's response Manuscript

ED: Publish as is (10 Jan 2017) by Gwenaël Abril

Short summary

Lakes contribute 6–16 % of methane to Earth's atmosphere. We focus on methane concentrations in Greenland lakes under open-water and ice-covered conditions. Significant warming in 2012 leads to greater methane concentrations in the lakes than in 2013. Methane concentrations under ice-covered conditions were greater than under open-water conditions. Results of this study suggest that interannual variation in ground-level air temperatures may be the primary driver of changes in methane dynamics.