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Climate of the Past An interactive open-access journal of the European Geosciences Union
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CP | Articles | Volume 16, issue 4
Clim. Past, 16, 1429–1450, 2020
https://doi.org/10.5194/cp-16-1429-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue: Paleoclimate Modelling Intercomparison Project phase 4 (PMIP4)...

Clim. Past, 16, 1429–1450, 2020
https://doi.org/10.5194/cp-16-1429-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 06 Aug 2020

Research article | 06 Aug 2020

CMIP6/PMIP4 simulations of the mid-Holocene and Last Interglacial using HadGEM3: comparison to the pre-industrial era, previous model versions and proxy data

Charles J. R. Williams et al.

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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) (29 May 2020) by Marie-France Loutre
AR by Charles Williams on behalf of the Authors (01 Jun 2020)  Author's response    Manuscript
ED: Publish subject to minor revisions (review by editor) (09 Jun 2020) by Marie-France Loutre
AR by Anna Mirena Feist-Polner on behalf of the Authors (25 Jun 2020)  Author's response    Manuscript
ED: Publish subject to technical corrections (30 Jun 2020) by Marie-France Loutre
AR by Charles Williams on behalf of the Authors (03 Jul 2020)  Author's response    Manuscript
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Short summary
Computer simulations of the geological past are an important tool to improve our understanding of climate change. We present results from two simulations using the latest version of the UK's climate model, the mid-Holocene (6000 years ago) and Last Interglacial (127 000 years ago). The simulations reproduce temperatures consistent with the pattern of incoming radiation. Model–data comparisons indicate that some regions (and some seasons) produce better matches to the data than others.
Computer simulations of the geological past are an important tool to improve our understanding...
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