Articles | Volume 19, issue 10
Biogeosciences, 19, 2627–2652, 2022
https://doi.org/10.5194/bg-19-2627-2022
Biogeosciences, 19, 2627–2652, 2022
https://doi.org/10.5194/bg-19-2627-2022
Research article
25 May 2022
Research article | 25 May 2022

Data-based estimates of interannual sea–air CO2 flux variations 1957–2020 and their relation to environmental drivers

Christian Rödenbeck 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
  • CC1: 'Comment on bg-2021-304', Rik Wanninkhof, 06 Dec 2021
    • AC1: 'Reply on CC1', Christian Rödenbeck, 20 Dec 2021
  • RC1: 'Review of Rodenbeck et al „Data-based estimates of interannual sea-air CO2 flux variations 1957-2020 and their relation to environmental drivers', Anonymous Referee #1, 10 Dec 2021
    • AC2: 'Reply on RC1', Christian Rödenbeck, 21 Dec 2021
  • CC2: 'Comment on bg-2021-304 by Jamie Shutler', Jamie Shutler, 17 Dec 2021
    • AC4: 'Reply on CC2', Christian Rödenbeck, 02 Feb 2022
  • CC3: 'Comment on bg-2021-304', Val Bennington, 21 Jan 2022
    • AC3: 'Reply on CC3', Christian Rödenbeck, 02 Feb 2022
  • RC2: 'Comment on bg-2021-304', Anonymous Referee #2, 04 Mar 2022
    • AC5: 'Reply on RC2', Christian Rödenbeck, 11 Mar 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (14 Mar 2022) by Jack Middelburg
AR by Christian Rödenbeck on behalf of the Authors (11 Apr 2022)  Author's response    Author's tracked changes
ED: Publish subject to technical corrections (02 May 2022) by Jack Middelburg
AR by Christian Rödenbeck on behalf of the Authors (02 May 2022)  Author's response    Manuscript
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Short summary
The ocean is an important part of the global carbon cycle, taking up about a quarter of the anthropogenic CO2 emitted by burning of fossil fuels and thus slowing down climate change. However, the CO2 uptake by the ocean is, in turn, affected by variability and trends in climate. Here we use carbon measurements in the surface ocean to quantify the response of the oceanic CO2 exchange to environmental conditions and discuss possible mechanisms underlying this response.
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