Coupling of a sediment diagenesis model (MEDUSA) and an Earth system model (CESM1.2): a contribution toward enhanced marine biogeochemical modelling and long-term climate simulations

Kurahashi-Nakamura, Takasumi; Paul, André; Munhoven, Guy; Merkel, Ute; Schulz, Michael

doi:https://doi.org/10.5194/gmd-13-825-2020

Articles | Volume 13, issue 2

https://doi.org/10.5194/gmd-13-825-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/gmd-13-825-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 13, issue 2

Development and technical paper

|

02 Mar 2020

Development and technical paper |

| 02 Mar 2020

Coupling of a sediment diagenesis model (MEDUSA) and an Earth system model (CESM1.2): a contribution toward enhanced marine biogeochemical modelling and long-term climate simulations

Takasumi Kurahashi-Nakamura, André Paul, Guy Munhoven, Ute Merkel, and Michael Schulz

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Final revised paper (published on 02 Mar 2020)
Supplement to the final revised paper
Preprint (discussion started on 07 Oct 2019)

Interactive discussion

Status: closed

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

- Printer-friendly version

- Supplement

RC1: 'Review comments for Coupling of sediment diagenesis model (MEDUSA) and an Earth system model (CESM1.3): a contribution toward enhanced marine biogeochemical modelling and long-term climate simulations', Anonymous Referee #1, 03 Nov 2019
- AC2: 'Response to RC1', Takasumi Kurahashi-Nakamura, 10 Jan 2020
SC1: 'Executive Editor Comment on gmd-2019-231', Astrid Kerkweg, 15 Nov 2019
- AC1: 'Reply to the 'Executive Editor Comment' on 15.11.2019', Takasumi Kurahashi-Nakamura, 15 Nov 2019
RC2: 'Accept with minor revisions', Anonymous Referee #2, 29 Nov 2019
- AC3: 'Response to RC2', Takasumi Kurahashi-Nakamura, 10 Jan 2020

Peer-review completion

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

AR by Takasumi Kurahashi-Nakamura on behalf of the Authors (27 Jan 2020) Author's response Manuscript

ED: Publish as is (03 Feb 2020) by Paul Halloran

Short summary

Chemical processes in ocean-floor sediments have a large influence on the marine carbon cycle, hence the global climate, at long timescales. We developed a new coupling scheme for a chemical sediment model and a comprehensive climate model. The new coupled model outperformed the original uncoupled climate model in reproducing the global distribution of sediment properties. The sediment model will also act as a bridge between the ocean model and paleoceanographic data.