The DeepMIP contribution to PMIP4: experimental design for model simulations of the EECO, PETM, and pre-PETM (version 1.0)

Author:

Lunt Daniel J.ORCID,Huber MatthewORCID,Anagnostou EleniORCID,Baatsen Michiel L. J.,Caballero RodrigoORCID,DeConto Rob,Dijkstra Henk A.,Donnadieu YannickORCID,Evans DavidORCID,Feng Ran,Foster Gavin L.ORCID,Gasson Ed,von der Heydt Anna S.ORCID,Hollis Chris J.ORCID,Inglis Gordon N.,Jones Stephen M.,Kiehl Jeff,Kirtland Turner Sandy,Korty Robert L.,Kozdon ReinhardtORCID,Krishnan Srinath,Ladant Jean-BaptisteORCID,Langebroek PetraORCID,Lear Caroline H.ORCID,LeGrande Allegra N.,Littler KateORCID,Markwick Paul,Otto-Bliesner BetteORCID,Pearson PaulORCID,Poulsen Christopher J.ORCID,Salzmann UlrichORCID,Shields Christine,Snell Kathryn,Stärz Michael,Super James,Tabor Clay,Tierney Jessica E.ORCID,Tourte Gregory J. L.ORCID,Tripati Aradhna,Upchurch Garland R.,Wade Bridget S.ORCID,Wing Scott L.,Winguth Arne M. E.,Wright Nicky M.,Zachos James C.,Zeebe Richard E.

Abstract

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.

Funder

Natural Environment Research Council

Publisher

Copernicus GmbH

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