Articles | Volume 16, issue 1
Clim. Past, 16, 1–16, 2020
https://doi.org/10.5194/cp-16-1-2020

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

Clim. Past, 16, 1–16, 2020
https://doi.org/10.5194/cp-16-1-2020

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 et al.

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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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
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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.