Articles | Volume 15, issue 5
https://doi.org/10.5194/cp-15-1691-2019
https://doi.org/10.5194/cp-15-1691-2019
Research article
 | 
13 Sep 2019
Research article |  | 13 Sep 2019

The HadCM3 contribution to PlioMIP phase 2

Stephen J. Hunter, Alan M. Haywood, Aisling M. Dolan, and Julia C. Tindall

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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: Reconsider after major revisions (13 May 2019) by Wing-Le Chan
AR by Stephen Hunter on behalf of the Authors (20 Jun 2019)
ED: Referee Nomination & Report Request started (25 Jun 2019) by Wing-Le Chan
RR by Anonymous Referee #2 (19 Jul 2019)
RR by Anonymous Referee #1 (26 Jul 2019)
ED: Publish subject to minor revisions (review by editor) (05 Aug 2019) by Wing-Le Chan
AR by Stephen Hunter on behalf of the Authors (15 Aug 2019)  Author's response   Manuscript 
ED: Publish subject to technical corrections (20 Aug 2019) by Wing-Le Chan
AR by Stephen Hunter on behalf of the Authors (21 Aug 2019)  Author's response   Manuscript 
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Short summary
In this paper, we model climate of the mid-Piacenzian warm period (mPWP; ~3 million years ago), a geological analogue for contemporary climate. Using the HadCM3 climate model, we show how changes in CO2 and geography contributed to mPWP climate. We find mPWP warmth focussed in the high latitudes, geography-driven precipitation changes, complex changes in sea surface temperature and intensified overturning in the North Atlantic (AMOC).