Simulating stable carbon isotopes in the ocean component of the FAMOUS general circulation model with MOSES1 (XOAVI)

Dentith, Jennifer E.; Ivanovic, Ruza F.; Gregoire, Lauren J.; Tindall, Julia C.; Robinson, Laura F.

doi:https://doi.org/10.5194/gmd-13-3529-2020

Articles | Volume 13, issue 8

https://doi.org/10.5194/gmd-13-3529-2020

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

Special issue:

The FAMOUS climate model

https://doi.org/10.5194/gmd-13-3529-2020

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

Articles | Volume 13, issue 8

Development and technical paper

|

07 Aug 2020

Development and technical paper |

| 07 Aug 2020

Simulating stable carbon isotopes in the ocean component of the FAMOUS general circulation model with MOSES1 (XOAVI)

Jennifer E. Dentith, Ruza F. Ivanovic, Lauren J. Gregoire, Julia C. Tindall, and Laura F. Robinson

Download

Final revised paper (published on 07 Aug 2020)
Supplement to the final revised paper
Preprint (discussion started on 07 Jan 2020)
Supplement to the preprint

Interactive discussion

Status: closed

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

- Printer-friendly version

- Supplement

SC1: 'Executive Editor Comment on gmd-2019-250', Astrid Kerkweg, 23 Jan 2020
- AC1: 'Response to the executive editor', Jennifer Dentith, 01 May 2020
RC1: 'Review of Dentith et al.', Anonymous Referee #1, 08 Feb 2020
- AC3: 'Response to reviewer #1', Jennifer Dentith, 05 May 2020
RC2: 'Review 2', Anonymous Referee #2, 13 Feb 2020
- AC2: 'Response to reviewer #2', Jennifer Dentith, 01 May 2020

Peer-review completion

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

AR by Jennifer Dentith on behalf of the Authors (29 May 2020) Author's response Manuscript

ED: Publish as is (19 Jun 2020) by Guy Munhoven

Short summary

We have added a new tracer (¹³C) into the ocean of the FAMOUS climate model to study large-scale circulation and the marine carbon cycle. The model captures the large-scale spatial pattern of observations but the simulated values are consistently higher than observed. In the first instance, our new tracer is therefore useful for recalibrating the physical and biogeochemical components of the model.