Articles | Volume 13, issue 2
Clim. Past, 13, 135–147, 2017
Clim. Past, 13, 135–147, 2017

Research article 16 Feb 2017

Research article | 16 Feb 2017

Changes to the tropical circulation in the mid-Pliocene and their implications for future climate

Shawn Corvec and Christopher G. Fletcher


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) (16 Jan 2017) by Arne Winguth
AR by Shawn Corvec on behalf of the Authors (17 Jan 2017)  Author's response    Manuscript
ED: Publish as is (29 Jan 2017) by Arne Winguth
Short summary
The mid-Pliocene warm period is sometimes thought of as being a climate that could closely resemble the climate in the near-term due to anthropogenic climate change. Here we examine the tropical atmospheric circulation as modeled by PlioMIP (the Pliocene Model Intercomparison Project). We find that there are many similarities and some important differences to projections of future climate, with the pattern of sea surface temperature (SST) warming being a key factor in explaining the differences.