PLASIM–GENIE v1.0: a new intermediate complexity AOGCM

We describe the development, tuning and climate of Planet Simulator (PLASIM)–Grid-ENabled Integrated Earth system model (GENIE), a new intermediate complexity Atmosphere–Ocean General Circulation Model (AOGCM), built by coupling the Planet Simulator to the ocean, sea-ice and land-surface components...

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Published in:Geoscientific Model Development
Main Authors: P. B. Holden, N. R. Edwards, K. Fraedrich, E. Kirk, F. Lunkeit, X. Zhu
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2016
Subjects:
Online Access:https://doi.org/10.5194/gmd-9-3347-2016
https://doaj.org/article/50e37d25e60941d5bde837c703029ae2
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spelling ftdoajarticles:oai:doaj.org/article:50e37d25e60941d5bde837c703029ae2 2023-05-15T18:18:36+02:00 PLASIM–GENIE v1.0: a new intermediate complexity AOGCM P. B. Holden N. R. Edwards K. Fraedrich E. Kirk F. Lunkeit X. Zhu 2016-09-01T00:00:00Z https://doi.org/10.5194/gmd-9-3347-2016 https://doaj.org/article/50e37d25e60941d5bde837c703029ae2 EN eng Copernicus Publications http://www.geosci-model-dev.net/9/3347/2016/gmd-9-3347-2016.pdf https://doaj.org/toc/1991-959X https://doaj.org/toc/1991-9603 1991-959X 1991-9603 doi:10.5194/gmd-9-3347-2016 https://doaj.org/article/50e37d25e60941d5bde837c703029ae2 Geoscientific Model Development, Vol 9, Iss 9, Pp 3347-3361 (2016) Geology QE1-996.5 article 2016 ftdoajarticles https://doi.org/10.5194/gmd-9-3347-2016 2022-12-30T21:29:02Z We describe the development, tuning and climate of Planet Simulator (PLASIM)–Grid-ENabled Integrated Earth system model (GENIE), a new intermediate complexity Atmosphere–Ocean General Circulation Model (AOGCM), built by coupling the Planet Simulator to the ocean, sea-ice and land-surface components of the GENIE Earth system model. PLASIM–GENIE supersedes GENIE-2, a coupling of GENIE to the Reading Intermediate General Circulation Model (IGCM). The primitive-equation atmosphere includes chaotic, three-dimensional (3-D) motion and interactive radiation and clouds, and dominates the computational load compared to the relatively simpler frictional-geostrophic ocean, which neglects momentum advection. The model is most appropriate for long-timescale or large ensemble studies where numerical efficiency is prioritised, but lack of data necessitates an internally consistent, coupled calculation of both oceanic and atmospheric fields. A 1000-year simulation with PLASIM–GENIE requires approximately 2 weeks on a single node of a 2.1 GHz AMD 6172 CPU. We demonstrate the tractability of PLASIM–GENIE ensembles by deriving a subjective tuning of the model with a 50-member ensemble of 1000-year simulations. The simulated climate is presented considering (i) global fields of seasonal surface air temperature, precipitation, wind, solar and thermal radiation, with comparisons to reanalysis data; (ii) vegetation carbon, soil moisture and aridity index; and (iii) sea surface temperature, salinity and ocean circulation. Considering its resolution, PLASIM–GENIE reproduces the main features of the climate system well and demonstrates usefulness for a wide range of applications. Article in Journal/Newspaper Sea ice Directory of Open Access Journals: DOAJ Articles Geoscientific Model Development 9 9 3347 3361
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Geology
QE1-996.5
spellingShingle Geology
QE1-996.5
P. B. Holden
N. R. Edwards
K. Fraedrich
E. Kirk
F. Lunkeit
X. Zhu
PLASIM–GENIE v1.0: a new intermediate complexity AOGCM
topic_facet Geology
QE1-996.5
description We describe the development, tuning and climate of Planet Simulator (PLASIM)–Grid-ENabled Integrated Earth system model (GENIE), a new intermediate complexity Atmosphere–Ocean General Circulation Model (AOGCM), built by coupling the Planet Simulator to the ocean, sea-ice and land-surface components of the GENIE Earth system model. PLASIM–GENIE supersedes GENIE-2, a coupling of GENIE to the Reading Intermediate General Circulation Model (IGCM). The primitive-equation atmosphere includes chaotic, three-dimensional (3-D) motion and interactive radiation and clouds, and dominates the computational load compared to the relatively simpler frictional-geostrophic ocean, which neglects momentum advection. The model is most appropriate for long-timescale or large ensemble studies where numerical efficiency is prioritised, but lack of data necessitates an internally consistent, coupled calculation of both oceanic and atmospheric fields. A 1000-year simulation with PLASIM–GENIE requires approximately 2 weeks on a single node of a 2.1 GHz AMD 6172 CPU. We demonstrate the tractability of PLASIM–GENIE ensembles by deriving a subjective tuning of the model with a 50-member ensemble of 1000-year simulations. The simulated climate is presented considering (i) global fields of seasonal surface air temperature, precipitation, wind, solar and thermal radiation, with comparisons to reanalysis data; (ii) vegetation carbon, soil moisture and aridity index; and (iii) sea surface temperature, salinity and ocean circulation. Considering its resolution, PLASIM–GENIE reproduces the main features of the climate system well and demonstrates usefulness for a wide range of applications.
format Article in Journal/Newspaper
author P. B. Holden
N. R. Edwards
K. Fraedrich
E. Kirk
F. Lunkeit
X. Zhu
author_facet P. B. Holden
N. R. Edwards
K. Fraedrich
E. Kirk
F. Lunkeit
X. Zhu
author_sort P. B. Holden
title PLASIM–GENIE v1.0: a new intermediate complexity AOGCM
title_short PLASIM–GENIE v1.0: a new intermediate complexity AOGCM
title_full PLASIM–GENIE v1.0: a new intermediate complexity AOGCM
title_fullStr PLASIM–GENIE v1.0: a new intermediate complexity AOGCM
title_full_unstemmed PLASIM–GENIE v1.0: a new intermediate complexity AOGCM
title_sort plasim–genie v1.0: a new intermediate complexity aogcm
publisher Copernicus Publications
publishDate 2016
url https://doi.org/10.5194/gmd-9-3347-2016
https://doaj.org/article/50e37d25e60941d5bde837c703029ae2
genre Sea ice
genre_facet Sea ice
op_source Geoscientific Model Development, Vol 9, Iss 9, Pp 3347-3361 (2016)
op_relation http://www.geosci-model-dev.net/9/3347/2016/gmd-9-3347-2016.pdf
https://doaj.org/toc/1991-959X
https://doaj.org/toc/1991-9603
1991-959X
1991-9603
doi:10.5194/gmd-9-3347-2016
https://doaj.org/article/50e37d25e60941d5bde837c703029ae2
op_doi https://doi.org/10.5194/gmd-9-3347-2016
container_title Geoscientific Model Development
container_volume 9
container_issue 9
container_start_page 3347
op_container_end_page 3361
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