PALEO-PGEM v1.0: a statistical emulator of Pliocene–Pleistocene climate

<p>We describe the development of the “Paleoclimate PLASIM-GENIE (Planet Simulator–Grid-Enabled Integrated Earth system model) emulator” PALEO-PGEM and its application to derive a downscaled high-resolution spatio-temporal description of the climate of the last <span class="inline-form...

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Main Authors: P. B. Holden, N. R. Edwards, T. F. Rangel, E. B. Pereira, G. T. Tran, R. D. Wilkinson
Format: Article
Language:English
Published: Copernicus Publications 2019-12-01
Series:Geoscientific Model Development
Online Access:https://www.geosci-model-dev.net/12/5137/2019/gmd-12-5137-2019.pdf
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author P. B. Holden
N. R. Edwards
T. F. Rangel
E. B. Pereira
G. T. Tran
R. D. Wilkinson
author_facet P. B. Holden
N. R. Edwards
T. F. Rangel
E. B. Pereira
G. T. Tran
R. D. Wilkinson
author_sort P. B. Holden
collection DOAJ
description <p>We describe the development of the “Paleoclimate PLASIM-GENIE (Planet Simulator–Grid-Enabled Integrated Earth system model) emulator” PALEO-PGEM and its application to derive a downscaled high-resolution spatio-temporal description of the climate of the last <span class="inline-formula">5×10<sup>6</sup></span> years. The <span class="inline-formula">5×10<sup>6</sup></span>-year time frame is interesting for a range of paleo-environmental questions, not least because it encompasses the evolution of humans. However, the choice of time frame was primarily pragmatic; tectonic changes can be neglected to first order, so that it is reasonable to consider climate forcing restricted to the Earth's orbital configuration, ice-sheet state, and the concentration of atmosphere <span class="inline-formula">CO<sub>2</sub></span>. The approach uses the Gaussian process emulation of the singular value decomposition of ensembles of the intermediate-complexity atmosphere–ocean GCM (general circulation model) PLASIM-GENIE. Spatial fields of bioclimatic variables of surface air temperature (warmest and coolest seasons) and precipitation (wettest and driest seasons) are emulated at 1000-year intervals, driven by time series of scalar boundary-condition forcing (<span class="inline-formula">CO<sub>2</sub></span>, orbit, and ice volume) and assuming the climate is in quasi-equilibrium. Paleoclimate anomalies at climate model resolution are interpolated onto the observed modern climatology to produce a high-resolution spatio-temporal paleoclimate reconstruction of the Pliocene–Pleistocene.</p>
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spelling doaj.art-bd9ae812f1194b2d9243bd3d5e98a7592022-12-22T01:31:38ZengCopernicus PublicationsGeoscientific Model Development1991-959X1991-96032019-12-01125137515510.5194/gmd-12-5137-2019PALEO-PGEM v1.0: a statistical emulator of Pliocene–Pleistocene climateP. B. Holden0N. R. Edwards1T. F. Rangel2E. B. Pereira3G. T. Tran4R. D. Wilkinson5Environment, Earth and Ecosystem Sciences, The Open University, Walton Hall, Milton Keynes, MK7 6AA, UKEnvironment, Earth and Ecosystem Sciences, The Open University, Walton Hall, Milton Keynes, MK7 6AA, UKDepartmento de Ecologia, Universidade Federal de Goiaìs, CP 131, 74.001-970 Goiânia, Goiaìs, BrazilDepartmento de Ecologia, Universidade Federal de Goiaìs, CP 131, 74.001-970 Goiânia, Goiaìs, BrazilGEOMAR Helmholtz Centre for Ocean Research Kiel, Düsternbrooker Weg 20, 24105 Kiel, GermanySchool of Mathematics and Statistics, University of Sheffield, Sheffield, UK<p>We describe the development of the “Paleoclimate PLASIM-GENIE (Planet Simulator–Grid-Enabled Integrated Earth system model) emulator” PALEO-PGEM and its application to derive a downscaled high-resolution spatio-temporal description of the climate of the last <span class="inline-formula">5×10<sup>6</sup></span> years. The <span class="inline-formula">5×10<sup>6</sup></span>-year time frame is interesting for a range of paleo-environmental questions, not least because it encompasses the evolution of humans. However, the choice of time frame was primarily pragmatic; tectonic changes can be neglected to first order, so that it is reasonable to consider climate forcing restricted to the Earth's orbital configuration, ice-sheet state, and the concentration of atmosphere <span class="inline-formula">CO<sub>2</sub></span>. The approach uses the Gaussian process emulation of the singular value decomposition of ensembles of the intermediate-complexity atmosphere–ocean GCM (general circulation model) PLASIM-GENIE. Spatial fields of bioclimatic variables of surface air temperature (warmest and coolest seasons) and precipitation (wettest and driest seasons) are emulated at 1000-year intervals, driven by time series of scalar boundary-condition forcing (<span class="inline-formula">CO<sub>2</sub></span>, orbit, and ice volume) and assuming the climate is in quasi-equilibrium. Paleoclimate anomalies at climate model resolution are interpolated onto the observed modern climatology to produce a high-resolution spatio-temporal paleoclimate reconstruction of the Pliocene–Pleistocene.</p>https://www.geosci-model-dev.net/12/5137/2019/gmd-12-5137-2019.pdf
spellingShingle P. B. Holden
N. R. Edwards
T. F. Rangel
E. B. Pereira
G. T. Tran
R. D. Wilkinson
PALEO-PGEM v1.0: a statistical emulator of Pliocene–Pleistocene climate
Geoscientific Model Development
title PALEO-PGEM v1.0: a statistical emulator of Pliocene–Pleistocene climate
title_full PALEO-PGEM v1.0: a statistical emulator of Pliocene–Pleistocene climate
title_fullStr PALEO-PGEM v1.0: a statistical emulator of Pliocene–Pleistocene climate
title_full_unstemmed PALEO-PGEM v1.0: a statistical emulator of Pliocene–Pleistocene climate
title_short PALEO-PGEM v1.0: a statistical emulator of Pliocene–Pleistocene climate
title_sort paleo pgem v1 0 a statistical emulator of pliocene pleistocene climate
url https://www.geosci-model-dev.net/12/5137/2019/gmd-12-5137-2019.pdf
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