Modeling a modern-like <i>p</i>CO<sub>2</sub> warm period (Marine Isotope Stage KM5c) with two versions of an Institut Pierre Simon Laplace atmosphere–ocean coupled general circulation model

Tan, Ning; Contoux, Camille; Ramstein, Gilles; Sun, Yong; Dumas, Christophe; Sepulchre, Pierre; Guo, Zhengtang

doi:https://doi.org/10.5194/cp-16-1-2020

Articles | Volume 16, issue 1

https://doi.org/10.5194/cp-16-1-2020

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

Special issue:

PlioMIP Phase 2: experimental design, implementation and scientific...

https://doi.org/10.5194/cp-16-1-2020

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

Articles | Volume 16, issue 1

Research article

|

06 Jan 2020

Research article |

| 06 Jan 2020

Modeling a modern-like pCO₂ warm period (Marine Isotope Stage KM5c) with two versions of an Institut Pierre Simon Laplace atmosphere–ocean coupled general circulation model

Ning Tan, Camille Contoux, Gilles Ramstein, Yong Sun, Christophe Dumas, Pierre Sepulchre, and Zhengtang Guo

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Final revised paper (published on 06 Jan 2020)
Supplement to the final revised paper
Preprint (discussion started on 17 Jul 2019)
Supplement to the preprint

Interactive discussion

Status: closed

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

- Printer-friendly version

- Supplement

RC1: 'Review for Modelling a Modern-like-pCO2 Warm Period (MIS KM5c) with Two Versions of IPSL AOGCM', Anonymous Referee #1, 05 Aug 2019
- AC1: 'Author Comments on the RC#1', Ning Tan, 23 Sep 2019
RC2: 'Review', Anonymous Referee #2, 06 Sep 2019
- AC2: 'Author Comments on the RC#2', Ning Tan, 23 Sep 2019

Peer-review completion

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

ED: Publish subject to minor revisions (review by editor) (07 Oct 2019) by Aisling Dolan

AR by Ning Tan on behalf of the Authors (17 Oct 2019) Author's response Manuscript

ED: Publish subject to technical corrections (23 Oct 2019) by Aisling Dolan

AR by Ning Tan on behalf of the Authors (28 Oct 2019) Manuscript

Short summary

To understand the warm climate during the late Pliocene (~3.205 Ma), modeling experiments with the new boundary conditions are launched and analyzed based on the Institut Pierre Simon Laplace (IPSL) atmosphere–ocean coupled general circulation model (AOGCM). Our results show that the warming in mid- to high latitudes enhanced due to the modifications of the land–sea mask and land–ice configuration. The pCO2 uncertainties within the records can produce asymmetrical warming patterns.

Modeling a modern-like pCO2 warm period (Marine Isotope Stage KM5c) with two versions of an Institut Pierre Simon Laplace atmosphere–ocean coupled general circulation model

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Interactive discussion

Peer-review completion

Modeling a modern-like pCO₂ warm period (Marine Isotope Stage KM5c) with two versions of an Institut Pierre Simon Laplace atmosphere–ocean coupled general circulation model