Pliocene Model Intercomparison Project (PlioMIP2) simulations using the Model for Interdisciplinary Research on Climate (MIROC4m)

Chan, Wing-Le; Abe-Ouchi, Ayako

doi:https://doi.org/10.5194/cp-16-1523-2020

Articles | Volume 16, issue 4

https://doi.org/10.5194/cp-16-1523-2020

© 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-16-1523-2020

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

Articles | Volume 16, issue 4

Research article

|

17 Aug 2020

Research article |

| 17 Aug 2020

Pliocene Model Intercomparison Project (PlioMIP2) simulations using the Model for Interdisciplinary Research on Climate (MIROC4m)

Wing-Le Chan and Ayako Abe-Ouchi

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Final revised paper (published on 17 Aug 2020)
Supplement to the final revised paper
Preprint (discussion started on 19 Feb 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

RC1: 'Review for PlioMIP2 simulations using the MIROC4m climate model', Anonymous Referee #1, 15 Mar 2020
- AC1: 'Reply to reviewer 1', Wing-Le Chan, 09 May 2020
RC2: 'Interactive comment on “PlioMIP2 simulations using the MIROC4m climate model” by Wing-Le Chan and Ayako Abe-Ouchi', Anonymous Referee #2, 24 Mar 2020
- AC2: 'Reply to reviewer 2', Wing-Le Chan, 09 May 2020

Peer-review completion

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

ED: Publish subject to minor revisions (review by editor) (21 May 2020) by Aisling Dolan

AR by Wing-Le Chan on behalf of the Authors (25 May 2020) Author's response

ED: Publish as is (02 Jul 2020) by Aisling Dolan

AR by Wing-Le Chan on behalf of the Authors (10 Jul 2020) Manuscript

Short summary

We carry out several modelling experiments to investigate the climate of the mid-Piacenzian warm period (~ 3.205 Ma) when CO₂ levels were similar to those of present day. The global surface air temperature is 3.1 °C higher compared to pre-industrial ones. Like previous experiments, the scale of warming suggested by proxy sea surface temperature (SST) data in the northern North Atlantic is not replicated. However, tropical Pacific SST shows good agreement with more recently published proxy data.