A Gaussian process emulator for simulating ice sheet–climate interactions on a multi-million-year timescale: CLISEMv1.0

On multi-million-year timescales, fully coupled ice sheet–climate simulations are hampered by computational limitations, even at coarser resolutions and when using asynchronous coupling schemes. In this study, a novel coupling method CLISEMv1.0 (CLimate–Ice Sheet EMulator version 1.0) is presented,...

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Published in:Geoscientific Model Development
Main Authors: Breedam, Jonas, Huybrechts, Philippe, Crucifix, Michel
Format: Text
Language:English
Published: 2021
Subjects:
Online Access:https://doi.org/10.5194/gmd-14-6373-2021
https://gmd.copernicus.org/articles/14/6373/2021/
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spelling ftcopernicus:oai:publications.copernicus.org:gmd94344 2023-05-15T16:39:33+02:00 A Gaussian process emulator for simulating ice sheet–climate interactions on a multi-million-year timescale: CLISEMv1.0 Breedam, Jonas Huybrechts, Philippe Crucifix, Michel 2021-10-25 application/pdf https://doi.org/10.5194/gmd-14-6373-2021 https://gmd.copernicus.org/articles/14/6373/2021/ eng eng doi:10.5194/gmd-14-6373-2021 https://gmd.copernicus.org/articles/14/6373/2021/ eISSN: 1991-9603 Text 2021 ftcopernicus https://doi.org/10.5194/gmd-14-6373-2021 2021-11-01T17:22:29Z On multi-million-year timescales, fully coupled ice sheet–climate simulations are hampered by computational limitations, even at coarser resolutions and when using asynchronous coupling schemes. In this study, a novel coupling method CLISEMv1.0 (CLimate–Ice Sheet EMulator version 1.0) is presented, where a Gaussian process emulator is applied to the climate model HadSM3 and coupled to the ice sheet model AISMPALEO. The temperature and precipitation fields from HadSM3 are emulated to feed the mass balance model in AISMPALEO. The sensitivity of the evolution of the ice sheet over time is tested with respect to the number of predefined ice sheet geometries that the emulator is calibrated on. Additionally, the model performance is evaluated in terms of the formulation of the ice sheet parameter (being ice sheet volume, ice sheet area or both) and the coupling time. Sensitivity experiments are conducted to explore the uncertainty introduced by the emulator. In addition, different lapse rate adjustments are used between the relatively coarse climate model and the much finer ice sheet model topography. It is shown that the ice sheet evolution over a million-year timescale is strongly sensitive to the definition of the ice sheet parameter and to the number of predefined ice sheet geometries. With the new coupling procedure, we provide a computationally efficient framework for simulating ice sheet–climate interactions on a multi-million-year timescale that allows for a large number of sensitivity tests. Text Ice Sheet Copernicus Publications: E-Journals Geoscientific Model Development 14 10 6373 6401
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description On multi-million-year timescales, fully coupled ice sheet–climate simulations are hampered by computational limitations, even at coarser resolutions and when using asynchronous coupling schemes. In this study, a novel coupling method CLISEMv1.0 (CLimate–Ice Sheet EMulator version 1.0) is presented, where a Gaussian process emulator is applied to the climate model HadSM3 and coupled to the ice sheet model AISMPALEO. The temperature and precipitation fields from HadSM3 are emulated to feed the mass balance model in AISMPALEO. The sensitivity of the evolution of the ice sheet over time is tested with respect to the number of predefined ice sheet geometries that the emulator is calibrated on. Additionally, the model performance is evaluated in terms of the formulation of the ice sheet parameter (being ice sheet volume, ice sheet area or both) and the coupling time. Sensitivity experiments are conducted to explore the uncertainty introduced by the emulator. In addition, different lapse rate adjustments are used between the relatively coarse climate model and the much finer ice sheet model topography. It is shown that the ice sheet evolution over a million-year timescale is strongly sensitive to the definition of the ice sheet parameter and to the number of predefined ice sheet geometries. With the new coupling procedure, we provide a computationally efficient framework for simulating ice sheet–climate interactions on a multi-million-year timescale that allows for a large number of sensitivity tests.
format Text
author Breedam, Jonas
Huybrechts, Philippe
Crucifix, Michel
spellingShingle Breedam, Jonas
Huybrechts, Philippe
Crucifix, Michel
A Gaussian process emulator for simulating ice sheet–climate interactions on a multi-million-year timescale: CLISEMv1.0
author_facet Breedam, Jonas
Huybrechts, Philippe
Crucifix, Michel
author_sort Breedam, Jonas
title A Gaussian process emulator for simulating ice sheet–climate interactions on a multi-million-year timescale: CLISEMv1.0
title_short A Gaussian process emulator for simulating ice sheet–climate interactions on a multi-million-year timescale: CLISEMv1.0
title_full A Gaussian process emulator for simulating ice sheet–climate interactions on a multi-million-year timescale: CLISEMv1.0
title_fullStr A Gaussian process emulator for simulating ice sheet–climate interactions on a multi-million-year timescale: CLISEMv1.0
title_full_unstemmed A Gaussian process emulator for simulating ice sheet–climate interactions on a multi-million-year timescale: CLISEMv1.0
title_sort gaussian process emulator for simulating ice sheet–climate interactions on a multi-million-year timescale: clisemv1.0
publishDate 2021
url https://doi.org/10.5194/gmd-14-6373-2021
https://gmd.copernicus.org/articles/14/6373/2021/
genre Ice Sheet
genre_facet Ice Sheet
op_source eISSN: 1991-9603
op_relation doi:10.5194/gmd-14-6373-2021
https://gmd.copernicus.org/articles/14/6373/2021/
op_doi https://doi.org/10.5194/gmd-14-6373-2021
container_title Geoscientific Model Development
container_volume 14
container_issue 10
container_start_page 6373
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