Articles | Volume 18, issue 20
Biogeosciences, 18, 5811–5830, 2021
https://doi.org/10.5194/bg-18-5811-2021
Biogeosciences, 18, 5811–5830, 2021
https://doi.org/10.5194/bg-18-5811-2021

Research article 29 Oct 2021

Research article | 29 Oct 2021

Field-scale CH4 emission at a subarctic mire with heterogeneous permafrost thaw status

Patryk Łakomiec et al.

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on bg-2021-81', Anonymous Referee #1, 01 May 2021
    • AC1: 'Reply on RC1', Patryk Łakomiec, 17 Jun 2021
  • RC2: 'Comment on bg-2021-81', Anonymous Referee #2, 07 May 2021
    • AC2: 'Reply on RC2', Patryk Łakomiec, 17 Jun 2021
  • RC3: 'Comment on bg-2021-81', L. Kutzbach, 11 May 2021
    • AC3: 'Reply on RC3', Patryk Łakomiec, 17 Jun 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (16 Jul 2021) by Helge Niemann
AR by Patryk Łakomiec on behalf of the Authors (24 Aug 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (20 Sep 2021) by Helge Niemann
AR by Patryk Łakomiec on behalf of the Authors (21 Sep 2021)  Author's response    Manuscript
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Short summary
Methane emission from the subarctic mire with heterogeneous permafrost status was measured for the years 2014–2016. Lower methane emission was measured from the palsa mire sector while the thawing wet sector emitted more. Both sectors have a similar annual pattern with a gentle rise during spring and a decrease during autumn. The highest emission was observed in the late summer. Winter emissions were positive during the measurement period and have a significant impact on the annual budgets.
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