On the mechanisms of warming the mid-Pliocene and the inference of a hierarchy of climate sensitivities with relevance to the understanding of climate futures

Chandan, Deepak; Peltier, W. Richard

doi:https://doi.org/10.5194/cp-14-825-2018

Articles | Volume 14, issue 6

https://doi.org/10.5194/cp-14-825-2018

© Author(s) 2018. 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-14-825-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 14, issue 6

Research article

|

18 Jun 2018

Research article |

| 18 Jun 2018

On the mechanisms of warming the mid-Pliocene and the inference of a hierarchy of climate sensitivities with relevance to the understanding of climate futures

Deepak Chandan and W. Richard Peltier

Download

Final revised paper (published on 18 Jun 2018)
Supplement to the final revised paper
Preprint (discussion started on 02 Mar 2018)
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 of "On the mechanisms of warming the mid-Pliocene and the inference of a hierarchy of climate sensitivities with relevance to the understanding of climate futures" by Deepak Chandan and W. Richard Peltier', Anonymous Referee #1, 06 Apr 2018
- AC1: 'Response to Reviewer 1', Deepak Chandan, 04 May 2018
RC2: 'Review of Chandan and Peltier', Anonymous Referee #2, 09 Apr 2018
- AC2: 'Response to Reviewer 2', Deepak Chandan, 04 May 2018

Peer-review completion

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

ED: Reconsider after major revisions (10 May 2018) by Wing-Le Chan

AR by Deepak Chandan on behalf of the Authors (29 May 2018) Author's response Manuscript

ED: Publish subject to technical corrections (07 Jun 2018) by Wing-Le Chan

Short summary

We infer the physical mechanisms by which the mid-Pliocene could have sustained a warm climate. We also provide a mid-Pliocene perspective on a range of climate sensitivities applicable on several timescales. Warming inferred on the basis of these sensitivity parameters is compared to forecasted levels of warming. This leads us to conclude that projections for 300–500 years into the future underestimate the potential for warming because they do not account for long-timescale feedback processes.