The DeepMIP contribution to PMIP4: methodologies for selection, compilation and analysis of latest Paleocene and early Eocene climate proxy data, incorporating version 0.1 of the DeepMIP database

Author:

Hollis Christopher J.ORCID,Dunkley Jones TomORCID,Anagnostou EleniORCID,Bijl Peter K.,Cramwinckel Margot J.ORCID,Cui Ying,Dickens Gerald R.ORCID,Edgar Kirsty M.ORCID,Eley YvetteORCID,Evans DavidORCID,Foster Gavin L.ORCID,Frieling JoostORCID,Inglis Gordon N.,Kennedy Elizabeth M.,Kozdon ReinhardORCID,Lauretano VittoriaORCID,Lear Caroline H.,Littler KateORCID,Lourens Lucas,Meckler A. Nele,Naafs B. David A.ORCID,Pälike Heiko,Pancost Richard D.,Pearson Paul N.ORCID,Röhl UrsulaORCID,Royer Dana L.ORCID,Salzmann Ulrich,Schubert Brian A.,Seebeck Hannu,Sluijs AppyORCID,Speijer Robert P.ORCID,Stassen PeterORCID,Tierney JessicaORCID,Tripati Aradhna,Wade BridgetORCID,Westerhold ThomasORCID,Witkowski Caitlyn,Zachos James C.,Zhang Yi GeORCID,Huber MatthewORCID,Lunt Daniel J.ORCID

Abstract

Abstract. The early Eocene (56 to 48 million years ago) is inferred to have been the most recent time that Earth's atmospheric CO2 concentrations exceeded 1000 ppm. Global mean temperatures were also substantially warmer than those of the present day. As such, the study of early Eocene climate provides insight into how a super-warm Earth system behaves and offers an opportunity to evaluate climate models under conditions of high greenhouse gas forcing. The Deep Time Model Intercomparison Project (DeepMIP) is a systematic model–model and model–data intercomparison of three early Paleogene time slices: latest Paleocene, Paleocene–Eocene thermal maximum (PETM) and early Eocene climatic optimum (EECO). A previous article outlined the model experimental design for climate model simulations. In this article, we outline the methodologies to be used for the compilation and analysis of climate proxy data, primarily proxies for temperature and CO2. This paper establishes the protocols for a concerted and coordinated effort to compile the climate proxy records across a wide geographic range. The resulting climate “atlas” will be used to constrain and evaluate climate models for the three selected time intervals and provide insights into the mechanisms that control these warm climate states. We provide version 0.1 of this database, in anticipation that this will be expanded in subsequent publications.

Funder

NERC Environmental Bioinformatics Centre

Publisher

Copernicus GmbH

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