The DeepMIP contribution to PMIP4: experimental design for model simulations of the EECO, PETM, and pre-PETM (version 1.0)
Author
Lunt, Daniel J.Huber, Matthew
Anagnostou, Eleni
Baatsen, Michiel L. J.
Caballero, Rodrigo
DeConto, Rob
Dijkstra, Henk A.
Donnadieu, Yannick
Evans, David
Feng, Ran
Foster, Gavin L.
Gasson, Ed
von der Heydt, Anna S.
Hollis, Chris J.
Inglis, Gordon N.
Jones, Stephen M.
Kiehl, Jeff
Kirtland Turner, Sandy
Korty, Robert L.
Kozdon, Reinhardt
Krishnan, Srinath
Ladant, Jean-Baptiste
Langebroek, Petra
Lear, Caroline H.
LeGrande, Allegra N.
Littler, Kate
Markwick, Paul
Otto-Bliesner, Bette
Pearson, Paul
Poulsen, Christopher J.
Salzmann, Ulrich
Shields, Christine
Snell, Kathryn
Stärz, Michael
Super, James
Tabor, Clay
Tierney, Jessica E.
Tourte, Gregory J. L.
Tripati, Aradhna
Upchurch, Garland R.
Wade, Bridget S.
Wing, Scott L.
Winguth, Arne M. E.
Wright, Nicky M.
Zachos, James C.
Zeebe, Richard E.
Affiliation
Univ Arizona, Dept GeosciIssue Date
2017-02-23
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COPERNICUS GESELLSCHAFT MBHCitation
The DeepMIP contribution to PMIP4: experimental design for model simulations of the EECO, PETM, and pre-PETM (version 1.0) 2017, 10 (2):889 Geoscientific Model DevelopmentJournal
Geoscientific Model DevelopmentRights
© Author(s) 2017. This work is distributed under the Creative Commons Attribution 3.0 License.Collection Information
This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.Abstract
Past warm periods provide an opportunity to evaluate climate models under extreme forcing scenarios, in particular high ( > 800 ppmv) atmospheric CO2 concentrations. Although a post hoc intercomparison of Eocene ( ∼ 50 Ma) climate model simulations and geological data has been carried out previously, models of past high-CO2 periods have never been evaluated in a consistent framework. Here, we present an experimental design for climate model simulations of three warm periods within the early Eocene and the latest Paleocene (the EECO, PETM, and pre-PETM). Together with the CMIP6 pre-industrial control and abrupt 4 × CO2 simulations, and additional sensitivity studies, these form the first phase of DeepMIP – the Deep-time Model Intercomparison Project, itself a group within the wider Paleoclimate Modelling Intercomparison Project (PMIP). The experimental design specifies and provides guidance on boundary conditions associated with palaeogeography, greenhouse gases, astronomical configuration, solar constant, land surface processes, and aerosols. Initial conditions, simulation length, and output variables are also specified. Finally, we explain how the geological data sets, which will be used to evaluate the simulations, will be developed.ISSN
1991-9603Version
Final published versionSponsors
NERC [NE/N006828/1, NE/K014757/1]; ERC [340923]; NSF [OCE-0902882]; Netherlands Earth System Science Centre (NESSC); Ministry of Education, Culture and Science (OCW) [024.002.001]Additional Links
http://www.geosci-model-dev.net/10/889/2017/ae974a485f413a2113503eed53cd6c53
10.5194/gmd-10-889-2017
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Except where otherwise noted, this item's license is described as © Author(s) 2017. This work is distributed under the Creative Commons Attribution 3.0 License.

