Articles | Volume 16, issue 4
https://doi.org/10.5194/cp-16-1523-2020
https://doi.org/10.5194/cp-16-1523-2020
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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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) (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
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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.